ESTRELLA RESOURCES LIMITED — Capital/Financing Update 2021

Jul 4, 2021

5 July 2021

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ASX ANNOUNCEMENT

First Phase 3 Assays Received for T5 Drilling at Carr Boyd

HIGHLIGHTS

• CBDD054 returned 13.4m[(1) ] @ 1.3% Ni & 0.4% Cu.

• Including 6.26m[(1) ] @ 2.08% Ni & 0.63% Cu, 2.78 g/t Ag, 0.67 g/t Pt + Pd.

• CBDD054B returned 25.32m[(1) ] @ 0.8% Ni & 0.6% Cu.

• Including 4.96m[(1) ] @ 1.15% Ni & 0.71% Cu, 2.45 g/t Ag, 1.13 g/t Pt + Pd.

• And a further 7.78m[(1) ] @ 1.14% Ni & 0.93% Cu, 3.14 g/t Ag, 0.72 g/t Pt + Pd.

• Other significant massive sulphide results include:

• CBDD049A: 1.87m[(1) ] @ 1.74% Ni & 0.54% Cu, 2.60 g/t Ag, 0.90 g/t Pt + Pd.

• CBDD053: 1.89m[(1) ] @ 1.40% Ni & 0.34% Cu, 1.49 g/t Ag, 0.59 g/t Pt + Pd.

• CBDD053A: 2.0m[(1) ] @ 0.46% Ni & 1.43% Cu, 6.50 g/t Ag, 0.52 g/t Pt + Pd.

• Four recently completed holes have assays pending with the laboratory.

• Massive sulphide plunge direction confirmed for the Upper T5 Conductor (Figure 1).

• The Company is understanding the cause of the limited Downhole Electromagnetic (DHEM) response at T5 which should enable further “blind” massive sulphides to be found.

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Figure 1: High-grade longsection depicting grade and width of Massive and Breccia Ni-Cu Sulphides on T5 Basal Contact in relation to the DHEM responses received to date.

(1): Downhole lengths are reported, true widths are approximately one half of downhole length. Refer to Table 1.

Estrella Resources Limited (ASX: ESR) (Estrella or the Company) is pleased to announce receipt of significant assays for the first eight Phase 3 diamond drill holes at the T5 Prospect at its 100%-owned Carr Boyd Project.

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Office Address London House, Level 11, 216 St Georges Terrace, PERTH WA 6000 Postal Address GPO Box 2517, PERTH WA 6831 Phone +61 8 9481 0389 Fax +61 8 9463 6103 Email info@estrellaresources.com.au

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The assays received have confirmed the Company’s interpretation of the geology, flow direction and grade distribution within the Upper T5 Conductor Zone along the basal contact. A full list of significant results can be seen in Table 1 below.

Of note are the intersections received for CBDD054 and CBDD054B which are some of the best results intersected at the T5 Prospect to date.

Assays are pending from four holes which have recently been completed, CBDD049B, CBDD050, CBDD054A and CBDD055, the latter two penetrating the same core zone as did CBDD030 which intersected 3.2m @ 3.19% Ni (refer to ASX Announcement 4 November 2020)

Table 1:	**Phase 3 Significant Intersections using **	**Phase 3 Significant Intersections using **	**Phase 3 Significant Intersections using **	**0.5% Nickel cutoff for lower-grade disseminated **	**0.5% Nickel cutoff for lower-grade disseminated **	**0.5% Nickel cutoff for lower-grade disseminated **	**0.5% Nickel cutoff for lower-grade disseminated **	**mineralisation **
				True				2PGE
Hole	m From	m To	Interval	Width	Ni%	Cu%	Co%	**	**Ag g/t **
CBDD048	381.5	388.4	6.9	3.3	0.54	0.26	0.03	0.41	1.10
including	382.5	383.14	0.64	0.3	1.52	0.21	0.08	0.95	1.35
and	385.85	386.2	0.35	0.2	1.32	0.36	0.06	0.61	2.10
CBDD049A	386.67	393.58	6.91	3.3	0.75	0.54	0.04	0.48	2.39
including	388.49	390.36	1.87	0.9	1.74	0.54	0.08	0.90	2.60
CBDD049B	Awaiting Results
CBDD049C	372.67	375.96	3.29	1.6	0.75	0.53	0.04	0.58	2.35
including	372.67	373.27	0.6	0.3	1.19	1.07	0.06	0.72	5.23
CBDD050	Awaiting Results
CBDD050A	Currentlydrillingat T5
CBDD051	Planned	Regional Hole
CBDD053	247.7	248	0.3		0.10	1.50	0.01	0.01	10.67
CBDD053	438.06	446.29	8.23	4.0	0.69	0.32	0.03	0.45	1.34
including	441.11	443	1.89	0.9	1.40	0.34	0.07	0.59	1.49
CBDD053A	426	428	2	1.0	0.46	1.43	0.02	0.52	6.50
CBDD053B	421.81	426.64	4.83	2.3	0.63	0.50	0.03	0.47	2.58
including	422.63	423.05	0.42	0.2	1.14	0.62	0.05	0.92	4.30
and	425.79	426.64	0.85	0.4	1.14	0.47	0.05	0.72	2.52
CBDD054	392.3	405.71	13.41	6.4	1.31	0.44	0.06	0.46	1.93
including	394.85	401.11	6.26	3.0	2.08	0.63	0.09	0.67	2.78
with	397.87	398.98	1.11	0.5	3.92	0.16	0.17	0.59	0.80
CBDD054A	Awaiting Results
CBDD054B	357	382.32	25.32	12.2	0.79	0.58	0.04	0.58	1.92
including	358.6	363.56	4.96	2.4	1.15	0.71	0.06	1.13	2.45
and	368.33	376.11	7.78	3.7	1.14	0.93	0.05	0.72	3.14
with	368.33	368.63	0.3	0.1	3.49	0.08	0.15	0.89	<0.5
CBDD055	Awaiting Results
CBDD055A	Currentlydrillingat T5

** 2PGE refers to Pt + Pd in g/t

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Estrella Managing Director Chris Daws commented:

“To have received some of the best results yet from our highly prospective Carr Boyd nickel-copper project is very encouraging.

“The results are particularly pleasing as it not only confirms our geological modelling of the Carr Boyd intrusive complex but it also demonstrates that the contact zone has the potential to bear high-grade results.

“We have a large volume of additional assay results to come and will update shareholders as soon as they are available. ”

Geological Interpretation of Assay Data

The assays confirm the Company’s geological interpretation of the settling, remobilisation and re-settling of massive sulphides along the T5 Pyroxenite Feeder basal contact. The intersections from diamond drillholes CBDD048, CBDD049A and CBDD049C show higher-grade massive and breccia sulphides on the basal contact with only a thin zone of lower-grade material stratigraphically above. The lower-grade material consists of disseminated sulphides that grade into globular sulphides just above the massive sulphide zones. This represents the active erosion of massive sulphides in this location at the time of solidification of the melt.

These sulphides are carried “down-stream” and are piled up above the massive sulphides intersected in CBDD054, CBDD054A (assays pending) and CBDD054B. In CBDD054B there are two massive sulphide zones, a lower basal contact breccia zone, and an upper semi-massive zone where remobilised globular sulphides from the eroded area mentioned above are beginning to coagulate and descend through the melt. Above this is a much broader zone of disseminated to blebby sulphides which remain suspended by flow turbulence.

Further down-stream, around holes CBDD053, CBDD053A and CBDD053B, a broad zone of globular, blebby and disseminated sulphides was intersected and is interpreted to be an area where higher turbulence prevented massive sulphide formation and in areas may even have scoured the contact of massive sulphides.

This is expected to be a cyclic repetition of scouring and redeposition along the flow direction, as evidenced by the intersection of massive sulphides further down the contact in holes CBDD035, CBDD036 and CBDD042A (Figure 1 and Figure 3).

Phase 3 will continue to step-out along the T5 Conductor to gain important vectoring information to further areas of suggested massive sulphide deposition beyond the current T5 Electromagnetic Conductor.

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Figure 2: Sulphide remobilisation in the flow direction and subsequent settling "down stream".

Observed Geology from Phase 3 and Implications for DHEM Response

The evidence being gathered by the Phase 3 program is aimed at understanding the flow dynamics that have existed over the T5 basal contact and the subsequent formation of massive and breccia sulphides. The Company aims to target these massive sulphides through a combination of drilling and downhole geophysics, particularly electromagnetics (DHEM).

However, the Company has noted that significant massive sulphides have been discovered by drillholes CBDD042A and CBDD035 in areas proximal or outside of the modelled DHEM responses. The Company has also noted that later intruding dolerite dykes and faulting has also off-set and dislocated nickel-copper sulphides such as in holes CBDD053A and CBDD053B. In addition, globular sulphides do contain significant nickel and copper, however they tend not to give a strong DHEM response.

Further possibility of late stage off-sets such as seen in holes CBDD034 and CBDD035 which drilled into an un-foreseen fault blank is creating more complexity. The combined result is a poorer DHEM response which can lead to semi-massive sulphide bodies being “blind” to downhole geophysical techniques.

Broader Implications of the Geological Interpretation for Phase 4 and Phase 5 Exploration

These globular and semi-massive sulphide bodies can still be of significant size and grade and their presence cannot be dismissed. The Company will principally use geological vectors to target drilling to give the DHEM the best chance of succeeding.

Phase 3 has also led to the understanding that the entire T5 Basal Contact orientation is prospective . The flow dynamics are such that massive sulphide plunge directions will have a local orientation. However,

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mineralisation continuity on the larger scale will have an oblique, possibly perpendicular orientation due to the effects of flow scouring and sulphide re-deposition.

Phase 4 Exploration Opportunity

Recognition of the flow dynamics, flow direction and modelling of the basal contact through seismic and other historical geophysics has placed a significant exploration opportunity before the Company at T5.

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Figure 3: The T5 Basal Contact as modelled represents a very significant exploration opportunity when compared to the current T5 discovery and drill area.

Figure 3 shows the scale of this opportunity with respect to the massive and semi-massive sulphides already discovered in the T5 Conductor Zone. This is marked within the small blue box “Drill Area”. As can be seen, Phase 4 has a very large scope and the Company aims to test this opportunity over the next few months through a combination of RC, RC pre-collar and diamond drilling whilst maintaining momentum following up the newly understood T5 massive sulphide plunge direction.

The discovery of massive sulphides at the Carr Boyd Mine in 1968 and the T5 massive sulphide discovery in 2020 show that this area within the T5 Igneous Complex is highly prospective. Exploration spend has been greatly de-risked and as such the T5 basal contact will receive the highest priority in exploration ranking.

Phase 5 Exploration Opportunity

The T5 pyroxenite is just one of several basal-contact locations within the broader Carr Boyd Igneous Complex. To date, around 30km of basal contact has been mapped (Figure 4).

The aim of Phase 5 drilling, which is likely to overlap timing-wise with the tail end of Phase 4 drilling, is to incorporate all available historical and newly generated data (such as the upcoming CSIRO collaboration) so that project areas within the Carr Boyd Complex can be risk-ranked according to probable success versus exploration spend required.

The learnings from Phase 3 and Phase 4 at T5 will be invaluable when ascertaining mineralisation controls on other parts of the complex where disseminated nickel-copper sulphides have already been discovered. Whilst disseminated sulphides will not likely lead to significant grades, they do show the high fertility of the Carr Boyd system and also can act as geological vectors towards additional high grade massive nickelcopper-iron sulphides elsewhere within the complex.

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Figure 4: The T5 Pyroxenite os only one of several mineralised pyroxenite bodies discovered within the Carr Boyd Igneous Complex. Phase 5 will set about ranking thesee opportunities and discovering currently unknown opportunities that will exist within such a large and fertile system.

The Board has authorised for this announcement to be released to the ASX.

FURTHER INFORMATION CONTACT

Christopher J. Daws Managing Director Estrella Resources Limited +61 8 9481 0389 info@estrellaresources.com.au

Media: David Tasker Managing Director Chapter One Advisors E: dtasker@chapteroneadvisors.com.au T: +61 433 112 936

Competent Person Statement

The information in this announcement relating to Exploration Results is based on information compiled by Steve Warriner, who is the Exploration Manager of Estrella Resources, and a member of The Australasian Institute of Geoscientists. Mr. Warriner has sufficient experience relevant to the style of mineralisation and type of deposit under consideration, and to the activity he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resource and Ore Reserves”. Mr. Warriner consents to the inclusion in the report of the matters based on his information in the form and context in which it appears.

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Table 2: Drill hole collar details

Hole ID	Final Depth	Easting	Northing	RL	Dip	Azimuth	Status
CBDD048	420.4	367423	6673626	429.2	-61	261	Completed
CBDD049	240.2	367422.5	6673626	429.2	-60	265	Completed
CBDD049A	414.6	367422.5	6673626	429.2	-60	265	Completed
CBDD049B	390.5	367422.5	6673626	429.2	-60	265	Completed
CBDD049C	415	367422.5	6673626	429.2	-60	265	Completed
CBDD050	411.4	367422	6673626	429.2	-59	267	Completed
CBDD053	514	367393.5	6673656	429.7	-70	270	Completed
CBDD053A	484	367393.5	6673656	429.7	-70	270	Completed
CBDD053B	460.2	367393.5	6673656	429.7	-70	270	Completed
CBDD054	461.4	367393	6673656.5	429.7	-69	267	Completed
CBDD054A	415	367393	6673656.5	429.7	-69	267	Completed
CBDD054B	411.6	367393	6673656.5	429.7	-69	267	Completed
CBDD055	421	367392	6673656	429.7	-68	266	Completed

Table 3: Assay Results informing Significant Intersection Calculations

Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co **ppm **	Ag **g/t **	MgO%	**Aug/t **	**Ptg/t **	**Pdg/t **	As **ppm **	S%	SG
CBDD048	ECB11044	372	373	1	0.06	0.01	67	<0.5	20.15	0.01	0.01	0.01	<5	0.07	2.97
CBDD048	ECB11045	373	374	1	0.07	0.01	72	<0.5	20.48	0.01	0.01	0.01	5.00	0.10	2.98
CBDD048	ECB11046	374	375	1	0.06	0.01	71	<0.5	19.57	0.01	0.01	0.01	<5	0.11	2.98
CBDD048	ECB11047	375	376	1	0.06	0.01	66	<0.5	18.82	0.01	0.01	0.01	<5	0.09	2.96
CBDD048	ECB11048	376	377	1	0.06	0.01	65	<0.5	18.99	0.01	0.01	0.01	<5	0.12	2.98
CBDD048	ECB11049	377	378	1	0.13	0.05	91	0.60	19.32	0.04	0.03	0.05	<5	0.49	3.00
CBDD048	ECB11050	378	379	1	0.09	0.03	85	<0.5	19.40	0.02	0.02	0.02	<5	0.41	2.87
CBDD048	ECB11051	379	380	1	0.06	0.02	73	<0.5	20.39	0.01	0.01	0.01	<5	0.14	3.00
CBDD048	ECB11052	380	380.5	0.5	0.08	0.02	76	<0.5	19.98	0.01	0.02	0.03	<5	0.20	2.99
CBDD048	ECB11053	380.5	381.5	1	0.12	0.04	85	<0.5	19.98	0.02	0.06	0.04	5.00	0.55	3.02
CBDD048	ECB11054	381.5	382.08	0.58	0.37	0.20	202	0.80	17.16	0.03	0.12	0.13	<5	2.95	3.07
CBDD048	ECB11055	382.08	382.5	0.42	0.48	0.25	243	1.00	17.41	0.02	0.30	0.19	<5	4.01	3.14
CBDD048	ECB11056	382.5	382.82	0.32	1.68	0.26	844	1.50	12.27	0.02	0.79	0.55	<5	15.55	3.54
CBDD048	ECB11057	382.82	383.14	0.32	1.36	0.16	683	1.20	12.82	0.01	0.10	0.44	<5	12.75	3.44
CBDD048	ECB11058	383.14	383.55	0.41	0.21	0.07	117	<0.5	17.82	0.01	0.05	0.05	6.00	1.57	3.03
CBDD048	ECB11059	383.55	383.91	0.36	0.28	0.12	156	0.70	18.16	0.03	0.08	0.10	<5	2.16	3.07
CBDD048	ECB11060	383.91	384.4	0.49	0.75	0.75	403	3.40	15.11	0.03	0.21	0.18	5.00	7.17	3.26
CBDD048	ECB11061	384.4	384.7	0.3	0.35	0.55	189	2.10	17.58	0.05	0.08	0.09	<5	3.44	3.14
CBDD048	ECB11062	384.7	385	0.3	0.68	0.61	351	2.00	14.61	0.18	1.03	0.24	<5	6.07	3.22
CBDD048	ECB11063	385	385.45	0.45	0.20	0.11	118	<0.5	17.66	0.02	0.09	0.06	<5	1.49	3.03
CBDD048	ECB11064	385.45	385.85	0.4	0.35	0.16	185	0.80	17.74	0.02	0.12	0.19	<5	2.79	3.08
CBDD048	ECB11065	385.85	386.2	0.35	1.32	0.36	647	2.10	10.45	0.03	0.16	0.45	<5	12.40	3.37
CBDD048	ECB11066	386.2	386.6	0.4	0.32	0.08	172	<0.5	16.91	0.01	0.04	0.12	<5	2.54	3.07
CBDD048	ECB11067	386.6	387.02	0.42	0.20	0.07	109	<0.5	18.90	0.01	0.04	0.05	<5	1.37	3.09
CBDD048	ECB11068	387.02	387.4	0.38	0.32	0.28	169	1.00	17.66	0.10	0.19	0.13	<5	2.72	3.11

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Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co **ppm **	Ag **g/t **	MgO%	**Aug/t **	**Ptg/t **	**Pdg/t **	As **ppm **	S%	SG
CBDD048	ECB11069	387.4	387.74	0.34	0.40	0.11	200	0.50	15.70	0.01	0.13	0.20	<5	3.29	3.13
CBDD048	ECB11070	387.74	388	0.26	0.19	0.11	116	0.70	10.10	0.02	0.08	0.05	<5	1.69	3.00
CBDD048	ECB11071	388	388.4	0.4	0.43	0.47	211	1.90	8.27	0.08	0.57	0.15	<5	3.43	3.05
CBDD048	ECB11072	388.4	389.25	0.85	0.03	0.03	61	<0.5	8.39	0.02	0.02	0.02	<5	0.26	2.98
CBDD048	ECB11073	389.25	390	0.75	0.02	0.01	56	<0.5	7.89	0.01	0.02	0.02	<5	0.15	3.01
CBDD048	ECB11074	390	390.3	0.3	0.23	0.23	146	1.10	7.00	0.01	0.19	0.10	5.00	1.42	3.04
CBDD048	ECB11075	390.3	391.1	0.8	0.02	0.01	55	<0.5	7.81	0.00	0.01	0.02	<5	0.11	3.01
CBDD048	ECB11076	391.1	391.9	0.8	0.07	0.05	72	0.50	8.11	0.02	0.08	0.04	<5	0.60	3.05
CBDD048	ECB11077	391.9	392.7	0.8	0.11	0.05	90	0.50	8.89	0.01	0.09	0.05	<5	0.94	3.07
CBDD048	ECB11078	392.7	393.57	0.87	0.11	0.16	78	0.60	6.83	0.06	0.11	0.09	<5	0.95	3.08
CBDD048	ECB11079	393.57	395	1.43	0.01	0.01	52	<0.5	7.48	0.01	0.02	0.02	<5	0.05	3.01
CBDD048	ECB11080	395	397	2	0.01	0.02	59	0.50	7.74	0.01	0.02	0.03	<5	0.13	3.00
CBDD048	ECB11081	397	399	2	0.01	0.01	59	<0.5	7.43	0.01	0.02	0.02	<5	0.08	3.02
CBDD048	ECB11082	399	401	2	0.01	0.01	58	<0.5	7.78	0.01	0.02	0.02	<5	0.07	3.04
CBDD048	ECB11083	401	403	2	0.01	0.01	53	<0.5	7.10	0.01	0.02	0.02	<5	0.05	3.04
CBDD049A	ECB11150	370.1	372.1	2	0.06	0.02	70	<0.5	19.48	0.01	0.01	0.01	<5	0.13	2.99
CBDD049A	ECB11151	372.1	374.1	2	0.06	0.01	65	<0.5	18.82	0.01	0.01	0.01	<5	0.09	3.00
CBDD049A	ECB11152	374.1	376.1	2	0.06	0.01	68	<0.5	19.15	0.01	0.01	0.01	<5	0.12	2.99
CBDD049A	ECB11153	376.1	378.1	2	0.05	0.01	66	<0.5	18.82	0.01	0.01	0.01	<5	0.08	3.02
CBDD049A	ECB11154	378.1	380.1	2	0.06	0.01	66	<0.5	18.90	0.01	0.01	0.01	<5	0.10	3.01
CBDD049A	ECB11155	380.1	382.1	2	0.06	0.01	66	<0.5	18.99	0.01	0.01	0.01	<5	0.09	3.00
CBDD049A	ECB11156	382.1	384.1	2	0.07	0.02	69	<0.5	18.90	0.02	0.03	0.02	<5	0.13	3.00
CBDD049A	ECB11157	384.1	385.91	1.81	0.10	0.02	78	<0.5	19.32	0.02	0.02	0.03	<5	0.19	3.01
CBDD049A	ECB11158	385.91	386.67	0.76	0.09	0.04	71	<0.5	16.75	0.02	0.03	0.03	<5	0.28	2.98
CBDD049A	ECB11159	386.67	388.49	1.82	0.40	0.37	206	1.50	17.66	0.02	0.32	0.15	<5	3.15	3.14
CBDD049A	ECB11160	388.49	390.36	1.87	1.74	0.54	844	2.60	10.55	0.03	0.20	0.69	<5	15.25	3.53
CBDD049A	ECB11161	390.36	390.96	0.6	0.22	0.50	124	2.10	15.37	0.04	0.14	0.07	<5	2.10	3.07
CBDD049A	ECB11162	390.96	391.36	0.4	0.70	0.86	362	4.80	11.01	0.07	0.09	0.27	<5	6.46	3.18
CBDD049A	ECB11163	391.36	391.96	0.6	0.29	1.40	154	5.70	12.30	0.15	0.24	0.08	<5	3.14	3.05
CBDD049A	ECB11164	391.96	393.58	1.62	0.23	0.34	137	1.40	8.51	0.03	0.04	0.10	<5	1.94	3.05
CBDD049A	ECB11165	393.58	395.58	2	0.04	0.04	62	<0.5	7.59	0.01	0.02	0.03	<5	0.37	3.03
CBDD049A	ECB11166	395.58	397.55	1.97	0.04	0.05	63	0.50	8.54	0.01	0.02	0.03	<5	0.34	3.05
CBDD049A	ECB11167	397.55	397.89	0.34	0.31	0.27	159	1.30	6.90	0.06	0.78	0.10	<5	2.48	3.10
CBDD049A	ECB11168	397.89	399.89	2	0.02	0.02	55	<0.5	8.12	0.01	0.02	0.02	<5	0.12	3.04
CBDD049A	ECB11169	399.89	401.89	2	0.02	0.05	60	<0.5	7.98	0.01	0.02	0.02	<5	0.21	3.03
CBDD049A	ECB11170	401.89	403.89	2	0.01	0.02	54	<0.5	7.73	0.01	0.02	0.02	<5	0.09	3.03
CBDD049A	ECB11171	403.89	405.89	2	0.04	0.07	59	0.60	7.68	0.04	0.05	0.04	<5	0.48	3.06
CBDD049A	ECB11172	405.89	407.89	2	0.01	0.03	59	<0.5	7.99	0.02	0.02	0.02	<5	0.19	1.00
CBDD049A	ECB11173	407.89	408.7	0.81	0.02	0.03	60	<0.5	7.86	0.02	0.03	0.03	<5	0.22	3.06

==> picture [145 x 60] intentionally omitted <==

Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co **ppm **	Ag **g/t **	MgO%	**Aug/t **	**Ptg/t **	**Pdg/t **	As **ppm **	S%	SG
CBDD049C	ECB11271	360.8	361.17	0.37	0.00	0.01	7	<0.5	1.34	0.00	<0.005	<0.001	<5	0.02	2.64
CBDD049C	ECB11272	361.17	362.54	1.37	0.10	0.03	93	<0.5	24.54	0.04	0.02	0.01	<5	0.05	2.95
CBDD049C	ECB11273	362.54	363.88	1.34	0.20	0.09	111	0.70	20.39	0.11	0.01	0.01	<5	0.27	2.95
CBDD049C	ECB11274	363.88	365.22	1.34	0.07	0.00	72	<0.5	18.74	<0.001	0.02	0.01	<5	<0.01	2.93
CBDD049C	ECB11275	365.22	366.04	0.82	0.12	0.06	92	<0.5	21.80	0.02	0.03	0.03	<5	0.57	2.94
CBDD049C	ECB11276	366.04	366.58	0.54	0.08	0.03	71	<0.5	15.69	0.01	0.02	0.02	<5	0.34	2.94
CBDD049C	ECB11277	366.58	367.47	0.89	0.05	0.01	62	<0.5	17.33	0.00	<0.005	<0.001	<5	0.08	2.94
CBDD049C	ECB11278	367.47	369.09	1.62	0.04	0.01	57	<0.5	15.62	0.01	<0.005	<0.001	<5	0.09	2.94
CBDD049C	ECB11279	369.09	370.7	1.61	0.04	0.01	62	<0.5	16.75	0.01	<0.005	<0.001	<5	0.07	2.96
CBDD049C	ECB11280	370.7	372.29	1.59	0.05	0.02	58	<0.5	13.02	0.00	0.01	0.01	<5	0.29	2.95
CBDD049C	ECB11281	372.29	372.67	0.38	0.37	0.09	197	<0.5	13.18	0.01	0.07	0.17	<5	2.99	3.08
CBDD049C	ECB11282	372.67	372.97	0.3	1.34	0.53	639	3.00	10.10	0.06	0.68	0.29	<5	13.00	3.40
CBDD049C	ECB11283	372.97	373.27	0.3	1.38	0.53	694	2.80	9.25	0.35	0.34	0.24	<5	13.05	3.35
CBDD049C	ECB11284	373.27	373.57	0.3	0.85	2.17	446	10.00	11.81	0.34	0.21	0.39	<5	8.97	3.30
CBDD049C	ECB11285	373.57	374.18	0.61	0.27	0.14	160	0.50	17.24	0.01	0.65	0.08	<5	2.17	3.12
CBDD049C	ECB11286	374.18	374.76	0.58	0.77	0.39	412	1.60	14.11	0.04	0.31	0.30	<5	5.91	3.26
CBDD049C	ECB11287	374.76	375.14	0.38	0.61	0.50	322	2.20	10.28	0.03	0.15	0.22	<5	4.94	3.12
CBDD049C	ECB11288	375.14	375.53	0.39	0.75	0.48	389	2.00	11.36	0.03	0.16	0.29	<5	5.89	3.20
CBDD049C	ECB11289	375.53	375.96	0.43	0.50	0.18	264	<0.5	13.30	0.01	0.11	0.21	<5	3.94	3.14
CBDD049C	ECB11290	375.96	376.98	1.02	0.08	0.04	68	<0.5	8.66	0.02	0.01	0.03	<5	0.60	2.97
CBDD049C	ECB11291	376.98	377.99	1.01	0.14	0.11	100	0.60	9.20	0.02	0.02	0.07	<5	1.01	3.01
CBDD049C	ECB11292	377.99	378.3	0.31	0.22	0.07	134	<0.5	7.94	0.01	0.05	0.10	<5	1.80	3.00
CBDD049C	ECB11293	378.3	379.32	1.02	0.09	0.04	80	<0.5	8.97	0.01	0.02	0.04	<5	0.64	3.01
CBDD049C	ECB11294	379.32	380.4	1.08	0.16	0.06	111	<0.5	8.04	0.02	0.02	0.07	<5	1.15	3.05
CBDD049C	ECB11295	380.4	382	1.6	0.02	0.02	60	<0.5	6.52	0.01	0.02	0.02	<5	0.13	2.97
CBDD049C	ECB11296	382	384	2	0.02	0.03	60	0.60	6.86	0.02	0.02	0.02	<5	0.15	3.00
CBDD049C	ECB11297	384	386	2	0.03	0.05	67	0.60	6.17	0.02	0.12	0.03	<5	0.27	2.97
CBDD053	ECB10830	247.7	248	0.3	0.10	1.50	123	10.67	3.85	2.30	0.01	0.00	X	1.72	3.03
CBDD053	ECB10831	363	363.5	0.5	0.03	0.00	29	X	4.63	0.01	0.02	0.02	12.00	0.05	2.98
CBDD053	ECB10832	367.4	367.9	0.5	0.05	0.01	37	0.13	4.29	0.01	0.03	0.03	1.00	0.10	3.00
CBDD053	ECB10833	370	372	2	0.05	0.01	38	0.07	3.96	0.00	0.02	0.02	1.00	0.13	3.05
CBDD053	ECB10834	372	374	2	0.05	0.02	42	0.16	4.15	0.01	0.03	0.02	1.00	0.14	2.97
CBDD053	ECB10835	374	376	2	0.11	0.02	70	0.15	8.99	0.01	0.02	0.02	X	0.22	3.19
CBDD053	ECB10836	376	377.7	1.7	0.17	0.05	90	0.21	9.17	0.02	0.05	0.05	1.00	0.53	3.25
CBDD053	ECB10837	377.7	379.7	2	0.04	0.01	32	0.09	4.18	0.01	0.03	0.02	2.00	0.09	2.81
CBDD053	ECB10838	379.7	381	1.3	0.09	0.02	69	0.10	5.92	0.01	0.03	0.03	2.00	0.32	3.04
CBDD053	ECB10839	381	383	2	0.11	0.03	73	0.09	5.67	0.01	0.03	0.03	3.00	0.36	3.00
CBDD053	ECB10840	383	385	2	0.09	0.03	59	0.19	4.69	0.01	0.03	0.03	1.00	0.31	2.98
CBDD053	ECB10841	385	387	2	0.15	0.07	95	0.47	3.63	0.03	0.26	0.07	1.00	0.81	3.01
CBDD053	ECB10842	387	389	2	0.13	0.10	102	0.64	5.24	0.03	0.09	0.07	1.00	1.14	2.95
CBDD053	ECB10843	389	391	2	0.10	0.09	85	0.65	4.68	0.04	0.14	0.06	X	0.87	2.97
CBDD053	ECB10844	391	393	2	0.02	0.01	18	0.08	3.47	0.01	0.01	0.01	X	X	2.98
CBDD053	ECB10845	393	395	2	0.01	0.01	14	0.09	2.64	0.01	0.01	0.01	X	X	3.21
CBDD053	ECB10846	395	397	2	0.11	0.07	58	0.52	3.17	0.03	0.13	0.08	X	0.52	2.95
CBDD053	ECB10847	397	397.8	0.8	0.42	0.20	200	1.39	3.02	0.07	0.30	0.25	X	2.42	3.06

==> picture [145 x 60] intentionally omitted <==

Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co ppm	Ag g/t	MgO%	Aug/t	Ptg/t	Pdg/t	As ppm	S%	SG
CBDD053	ECB10848	397.8	399.1	1.3	0.35	0.23	171	1.83	2.82	0.16	0.14	0.21	X	2.24	3.05
CBDD053	ECB10849	399.1	400.4	1.3	0.27	0.25	135	2.20	2.47	0.10	0.22	0.17	X	1.78	2.88
CBDD053	ECB10850	400.4	402.04	1.64	0.09	0.10	45	0.87	3.23	0.08	0.09	0.07	X	0.36	2.78
CBDD053	ECB10851	402.04	403.8	1.76	0.12	0.05	72	0.21	4.94	0.01	0.02	0.03	X	0.71	3.01
CBDD053	ECB10852	403.8	404.13	0.33	0.21	0.06	117	0.23	5.16	0.01	0.15	0.08	1.00	0.95	2.94
CBDD053	ECB10853	404.13	405.07	0.94	0.16	0.05	106	0.17	6.86	0.01	0.10	0.05	2.00	0.76	2.98
CBDD053	ECB10854	405.07	405.98	0.91	0.11	0.03	77	0.11	5.69	0.00	0.03	0.03	1.00	0.52	3.04
CBDD053	ECB10855	405.98	407	1.02	0.01	0.00	5	X	0.46	0.00	0.00	0.00	1.00	X	2.59
CBDD053	ECB10856	407	408.11	1.11	0.12	0.07	72	0.50	4.76	0.06	0.17	0.07	X	0.45	3.07
CBDD053	ECB10857	408.11	409.23	1.12	0.21	0.15	105	1.00	4.33	0.13	0.23	0.13	X	1.20	3.04
CBDD053	ECB10858	409.23	409.53	0.3	0.23	0.12	117	1.05	4.76	0.07	0.26	0.16	X	1.34	3.07
CBDD053	ECB10859	409.53	409.89	0.36	0.29	0.35	153	2.51	5.55	0.21	0.10	0.19	X	1.96	3.00
CBDD053	ECB10860	409.89	411.12	1.23	0.09	0.07	56	0.56	4.66	0.05	0.07	0.05	X	0.39	3.09
CBDD053	ECB10861	411.12	411.97	0.85	0.18	0.09	100	0.64	4.44	0.03	0.08	0.10	X	1.12	3.05
CBDD053	ECB10862	411.97	412.78	0.81	0.20	0.14	113	1.00	4.96	0.06	0.11	0.11	1.00	1.27	2.97
CBDD053	ECB10863	412.78	413.88	1.1	0.12	0.06	83	0.40	5.19	0.02	0.05	0.06	1.00	0.80	3.00
CBDD053	ECB10864	413.88	415.03	1.15	0.09	0.04	57	0.35	4.64	0.02	0.05	0.04	1.00	0.38	2.96
CBDD053	ECB10865	415.03	417	1.97	0.03	0.01	24	X	4.01	0.01	0.03	0.02	X	0.05	2.91
CBDD053	ECB10866	417	419	2	0.02	0.00	18	X	3.47	0.00	0.01	0.01	X	X	2.96
CBDD053	ECB10867	419	421	2	0.02	0.00	18	X	3.43	0.00	0.01	0.01	X	X	3.01
CBDD053	ECB10868	421	423	2	0.01	0.00	15	0.07	2.98	0.00	0.01	0.01	X	X	2.99
CBDD053	ECB10869	423	425	2	0.02	0.01	17	0.09	3.27	0.01	0.01	0.01	X	X	2.99
CBDD053	ECB10870	425	427	2	0.02	0.00	17	0.06	3.23	0.00	0.01	0.01	X	X	2.95
CBDD053	ECB10871	427	429	2	0.02	0.01	16	0.06	3.08	0.01	0.01	0.01	X	X	2.97
CBDD053	ECB10872	429	431	2	0.01	0.01	15	0.07	2.85	0.00	0.01	0.01	X	X	2.97
CBDD053	ECB10874	431	432.25	1.25	0.03	0.01	26	0.14	3.02	0.01	0.02	0.02	X	0.11	3.05
CBDD053	ECB10875	432.25	434	1.75	0.10	0.05	45	0.38	2.98	0.03	0.03	0.03	X	0.41	3.00
CBDD053	ECB10876	434	435.75	1.75	0.12	0.08	61	0.49	2.93	0.03	0.03	0.04	X	0.64	3.11
CBDD053	ECB10877	435.75	436.52	0.77	0.41	0.23	206	1.06	3.10	0.01	0.02	0.16	X	3.12	3.04
CBDD053	ECB10878	436.52	437.6	1.08	0.10	0.06	60	0.23	2.54	0.01	0.04	0.05	X	0.70	3.00
CBDD053	ECB10879	437.6	438.06	0.46	0.31	0.15	147	0.98	2.35	0.01	0.18	0.15	X	2.55	3.07
CBDD053	ECB10880	438.06	438.31	0.25	0.53	1.50	250	5.01	2.54	0.18	0.06	0.27	3.00	5.90	3.31
CBDD053	ECB10881	438.31	438.84	0.53	0.50	0.69	233	2.70	2.42	0.02	0.14	0.20	X	4.21	3.07
CBDD053	ECB10882	438.84	439.29	0.45	0.48	0.31	215	1.12	2.45	0.01	0.09	0.19	X	3.67	3.07
CBDD053	ECB10883	439.29	439.72	0.43	0.32	0.19	150	0.65	2.84	0.02	0.27	0.14	X	2.41	3.13
CBDD053	ECB10884	439.72	440.25	0.53	0.08	0.06	50	0.29	2.64	0.03	0.02	0.02	X	0.64	3.13
CBDD053	ECB10885	440.25	440.64	0.39	0.59	0.67	277	3.20	2.47	0.07	0.15	0.28	X	5.62	3.20
CBDD053	ECB10886	440.64	441.11	0.47	0.72	0.41	334	1.89	2.60	0.02	0.10	0.30	X	6.46	3.14
CBDD053	ECB10887	441.11	441.57	0.46	1.36	0.43	644	1.95	2.17	0.02	0.20	0.44	1.00	11.93	3.27
CBDD053	ECB10888	441.57	442	0.43	0.97	0.31	448	1.34	2.98	0.02	0.28	0.28	1.00	8.12	3.14
CBDD053	ECB10889	442	442.49	0.49	1.48	0.50	686	2.08	2.44	0.01	0.23	0.36	1.00	12.09	3.36
CBDD053	ECB10890	442.49	443	0.51	1.70	0.14	794	0.65	2.90	0.01	0.18	0.38	2.00	13.34	3.45
CBDD053	ECB10891	443	443.53	0.53	0.57	0.07	269	0.31	3.47	0.01	0.23	0.25	X	4.36	3.13
CBDD053	ECB10892	443.53	444	0.47	0.20	0.21	100	1.36	1.54	0.09	0.09	0.10	X	1.78	3.02
CBDD053	ECB10893	444	444.62	0.62	0.57	0.18	269	0.92	3.56	0.01	0.10	0.47	X	4.40	3.15

==> picture [145 x 60] intentionally omitted <==

Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co ppm	Ag g/t	MgO%	Aug/t	Ptg/t	Pdg/t	As ppm	S%	SG
CBDD053	ECB10894	444.62	445.44	0.82	0.27	0.14	131	0.55	1.97	0.03	0.29	0.15	X	1.97	2.92
CBDD053	ECB10895	445.44	446.29	0.85	0.69	0.16	336	0.62	3.88	0.02	0.40	0.24	X	4.93	3.10
CBDD053	ECB10896	446.29	447.31	1.02	0.28	0.26	139	1.11	3.37	0.03	0.17	0.14	X	2.19	3.09
CBDD053	ECB10897	447.31	448.34	1.03	0.24	0.16	118	1.13	2.65	0.14	0.35	0.11	1.00	0.93	3.03
CBDD053	ECB10898	452.14	452.65	0.51	0.10	0.03	70	0.13	5.27	0.00	0.04	0.04	1.00	0.62	2.76
CBDD053	ECB10899	455.82	456.39	0.57	0.02	0.00	23	0.08	4.16	0.00	0.01	0.02	X	X	2.94
CBDD053	ECB10900	462.28	462.71	0.43	0.08	0.65	96	12.26	3.28	0.12	0.03	0.04	X	0.99	2.92
CBDD053	ECB10901	464.69	465.21	0.52	0.01	0.00	17	0.06	3.40	0.00	0.02	0.03	X	X	2.98
CBDD053	ECB10902	470.14	470.66	0.52	0.02	0.00	20	X	4.05	0.00	0.02	0.01	X	X	2.92
CBDD053	ECB10903	473	474.42	1.42	0.12	0.06	47	0.66	2.72	0.05	0.04	0.05	X	0.45	2.91
CBDD053	ECB10905	474.42	476	1.58	0.15	0.07	77	0.54	4.56	0.02	0.03	0.05	X	0.56	2.97
CBDD053	ECB10906	476	478	2	0.04	0.02	25	0.35	2.80	0.01	0.00	0.00	X	0.08	2.87
CBDD053	ECB10907	478	480	2	0.04	0.02	31	0.34	3.81	0.01	0.00	0.00	X	0.06	2.98
CBDD053	ECB10908	480	480.56	0.56	0.06	0.01	41	0.24	5.50	0.01	0.00	0.00	X	0.06	2.85
CBDD053	ECB10909	489	491	2	0.06	0.02	46	0.11	4.08	0.00	0.00	0.00	X	0.20	3.02
CBDD053	ECB10910	491	493	2	0.04	0.02	40	0.14	5.39	0.01	0.01	0.01	X	0.18	3.32
CBDD053	ECB10911	493	493.73	0.73	0.05	0.05	39	0.39	3.58	0.03	0.01	0.01	X	0.32	3.18
CBDD053	ECB10912	493.73	495	1.27	0.13	0.26	79	1.04	0.78	0.03	0.06	0.03	X	1.51	2.91
CBDD053	ECB10913	495	497	2	0.01	0.03	13	0.35	0.91	0.01	0.00	0.00	X	0.14	2.81
CBDD053	ECB10914	497	498	1	0.01	0.02	10	0.31	0.96	0.02	0.00	0.00	X	0.07	2.75
CBDD053	ECB10915	498	498.3	0.3	0.12	0.18	69	0.72	0.85	0.02	0.02	0.02	X	1.20	2.74
CBDD053	ECB10916	498.3	499.84	1.54	0.03	0.02	23	0.15	0.78	0.01	0.01	0.01	X	0.34	2.95
CBDD053	ECB10917	499.84	501.2	1.36	0.09	0.09	58	0.43	0.60	0.02	0.02	0.03	X	0.98	2.94
CBDD053	ECB10918	501.2	503	1.8	0.01	0.04	17	0.38	0.75	0.02	0.02	0.02	X	0.22	3.09
CBDD053	ECB10919	503	505	2	0.00	0.02	9	0.20	0.70	0.01	0.01	0.02	X	0.07	3.02
CBDD053	ECB10920	505	507	2	0.00	0.01	9	0.15	0.63	0.01	0.02	0.01	X	0.08	2.99
CBDD053	ECB10921	507	509	2	0.00	0.01	8	0.12	0.55	0.01	0.01	0.01	X	0.06	2.96
CBDD053	ECB10922	509	511	2	0.00	0.01	8	0.20	0.60	0.01	0.01	0.01	X	0.06	2.97
CBDD053	ECB10923	511	513	2	0.00	0.01	9	0.11	0.83	0.00	0.01	0.01	X	0.05	3.01
CBDD053A	ECB10926	390	391.16	1.16	0.09	0.04	74	X	16.76	0.01	0.03	0.04	X	0.43	2.99
CBDD053A	ECB10927	391.16	391.82	0.66	0.26	0.41	162	2.00	4.38	0.04	0.01	0.16	X	3.36	2.98
CBDD053A	ECB10928	391.82	393	1.18	0.13	0.08	78	X	17.79	0.02	0.06	0.06	X	0.63	3.11
CBDD053A	ECB10929	393	394	1	0.19	0.06	113	X	20.51	0.01	0.06	0.06	X	0.79	3.04
CBDD053A	ECB10930	394	395	1	0.17	0.08	127	X	21.68	0.01	0.05	0.05	X	1.10	3.02
CBDD053A	ECB10931	395	397	2	0.21	0.08	134	X	19.68	0.03	0.25	0.12	X	1.11	3.04
CBDD053A	ECB10932	397	399	2	0.11	0.05	87	X	20.05	0.04	0.07	0.05	X	0.42	3.03
CBDD053A	ECB10933	399	400	1	0.18	0.10	115	X	20.82	0.02	0.13	0.09	X	1.37	3.05
CBDD053A	ECB10934	400	401	1	0.33	0.18	182	0.80	20.92	0.07	0.16	0.19	X	2.52	3.11
CBDD053A	ECB10935	401	403	2	0.09	0.04	69	X	18.95	0.05	0.04	0.03	X	0.18	3.02
CBDD053A	ECB10936	403	405	2	0.07	0.01	61	X	18.14	0.01	0.02	0.02	X	0.08	2.98
CBDD053A	ECB10937	410	411.4	1.4	0.06	0.01	59	X	16.92	0.01	0.01	0.01	X	0.08	2.98
CBDD053A	ECB10938	411.4	412	0.6	0.52	0.26	285	1.10	15.01	0.03	0.14	0.18	X	4.67	3.11
CBDD053A	ECB10940	412	414	2	0.26	0.14	150	0.60	16.86	0.04	0.14	0.12	X	2.13	2.94
CBDD053A	ECB10941	414	415	1	0.11	0.06	73	X	16.78	0.09	0.17	0.06	X	0.52	3.01
CBDD053A	ECB10942	415	416	1	0.25	0.15	135	1.70	16.48	0.09	0.27	0.13	X	1.96	3.05

==> picture [145 x 60] intentionally omitted <==

Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co ppm	Ag g/t	MgO%	Aug/t	Ptg/t	Pdg/t	As ppm	S%	SG
CBDD053A	ECB10943	416	417	1	0.14	0.14	82	1.20	14.58	0.16	0.15	0.09	X	1.04	3.02
CBDD053A	ECB10944	417	418	1	0.19	0.10	109	X	16.87	0.04	0.20	0.12	X	1.52	3.01
CBDD053A	ECB10945	418	419	1	0.11	0.06	75	X	16.11	0.04	0.04	0.04	X	0.63	2.96
CBDD053A	ECB10946	419	420	1	0.27	0.12	151	X	12.28	0.02	0.04	0.10	X	2.16	3.05
CBDD053A	ECB10947	420	422	2	0.07	0.02	58	X	14.66	0.01	0.02	0.03	X	0.21	3.01
CBDD053A	ECB10948	422	424.45	2.45	0.06	0.03	59	X	11.75	0.01	0.03	0.04	X	0.25	2.94
CBDD053A	ECB10949	424.45	425	0.55	0.12	0.06	94	X	14.53	0.01	0.10	0.05	X	0.91	3.06
CBDD053A	ECB10950	425	426	1	0.21	0.11	130	X	15.12	0.01	0.08	0.12	X	1.66	3.14
CBDD053A	ECB10951	426	427	1	0.41	0.73	213	3.10	15.38	0.08	0.09	0.29	X	4.03	3.27
CBDD053A	ECB10952	427	428	1	0.52	2.12	284	9.90	12.67	0.23	0.25	0.41	X	6.62	3.27
CBDD053A	ECB10953	428	429	1	0.09	0.08	75	X	13.12	0.08	0.11	0.06	X	0.61	2.99
CBDD053A	ECB10954	429	430	1	0.25	0.15	136	X	10.67	0.02	0.06	0.11	X	2.10	3.02
CBDD053A	ECB10955	430	430.6	0.6	0.40	0.26	203	1.00	13.07	0.03	0.13	0.25	X	3.46	3.08
CBDD053A	ECB10956	430.6	432	1.4	0.16	0.11	109	X	12.40	0.03	0.04	0.07	X	1.31	3.00
CBDD053A	ECB10957	432	433	1	0.19	0.16	124	X	13.38	0.29	0.34	0.07	X	1.56	3.09
CBDD053A	ECB10958	433	434	1	0.73	0.31	375	0.90	14.19	0.01	0.02	0.26	X	6.12	3.28
CBDD053A	ECB10959	434	435	1	0.08	0.01	83	X	15.99	0.00	0.02	0.02	X	0.18	3.07
CBDD053A	ECB10960	435	436	1	0.17	0.11	127	0.70	16.89	0.09	0.02	0.03	X	1.09	3.08
CBDD053A	ECB10962	436	438	2	0.13	0.07	108	X	17.05	0.04	0.01	0.03	X	0.74	3.05
CBDD053A	ECB10963	438	439.6	1.6	0.29	0.15	179	X	16.81	0.01	0.02	0.12	X	2.57	3.14
CBDD053A	ECB10964	439.6	440	0.4	0.46	0.33	264	1.20	7.32	0.07	0.02	0.17	X	4.51	3.16
CBDD053A	ECB10965	440	442	2	0.02	0.02	61	X	8.14	0.01	0.02	0.02	X	0.18	3.03
CBDD053A	ECB10966	442	444	2	0.01	0.02	58	X	7.75	0.01	0.02	0.02	X	0.05	3.03
CBDD053A	ECB10967	444	446	2	0.01	0.01	57	X	6.62	0.01	0.02	0.02	X	0.07	3.02
CBDD053B	ECB10968	386	387.5	1.5	0.07	0.01	73	<0.5	21.64	0.01	0.01	0.01	<5	0.09	2.87
CBDD053B	ECB10969	387.5	388	0.5	0.07	0.01	71	<0.5	21.39	0.01	0.01	0.01	<5	0.07	2.99
CBDD053B	ECB10970	388	389	1	0.23	0.09	129	0.50	20.15	0.02	0.14	0.11	<5	1.31	3.02
CBDD053B	ECB10971	389	390	1	0.53	0.25	244	1.30	19.57	0.07	0.13	0.26	<5	3.64	3.10
CBDD053B	ECB10972	390	391	1	0.33	0.13	168	0.70	19.81	0.03	0.22	0.16	<5	2.13	3.06
CBDD053B	ECB10973	391	391.77	0.77	0.39	0.93	244	4.00	20.56	0.02	0.04	0.14	<5	3.09	3.09
CBDD053B	ECB10974	391.77	392.5	0.73	0.20	0.07	105	<0.5	19.90	0.01	0.12	0.08	5.00	0.88	3.05
CBDD053B	ECB10975	392.5	393.5	1	0.16	0.08	104	<0.5	21.89	0.02	0.20	0.06	<5	0.71	3.05
CBDD053B	ECB10976	393.5	394.5	1	0.24	0.14	145	0.90	20.23	0.08	0.23	0.12	<5	1.37	3.10
CBDD053B	ECB10977	394.5	395.5	1	0.12	0.03	89	<0.5	21.72	0.02	0.06	0.04	<5	0.32	3.04
CBDD053B	ECB10978	395.5	396.5	1	0.13	0.05	80	<0.5	20.15	0.04	0.12	0.05	<5	0.35	3.03
CBDD053B	ECB10979	396.5	397.5	1	0.22	0.14	124	1.30	20.39	0.15	0.24	0.08	<5	0.95	3.08
CBDD053B	ECB10980	397.5	398.5	1	0.33	0.21	173	1.40	20.64	0.12	0.18	0.17	<5	2.32	3.11
CBDD053B	ECB10981	398.5	399.16	0.66	0.35	0.20	177	1.40	21.47	0.06	0.22	0.17	<5	2.50	3.07
CBDD053B	ECB10982	399.16	399.85	0.69	0.14	0.08	88	0.60	21.14	0.07	0.06	0.05	<5	0.44	3.03
CBDD053B	ECB10983	399.85	401.85	2	0.08	0.01	60	<0.5	19.40	0.02	0.02	0.02	<5	0.05	2.99
CBDD053B	ECB10984	401.85	403.85	2	0.07	0.01	61	<0.5	19.40	0.01	0.01	0.01	<5	0.04	2.98
CBDD053B	ECB10985	403.85	405.85	2	0.07	0.01	58	<0.5	19.15	0.00	0.01	0.01	<5	0.07	3.00
CBDD053B	ECB10986	405.85	406.52	0.67	0.54	0.20	250	1.00	17.58	0.02	0.22	0.12	<5	4.08	3.11
CBDD053B	ECB10987	406.52	407.12	0.6	0.67	0.65	314	2.40	17.00	0.42	0.38	0.13	<5	5.42	3.17
CBDD053B	ECB10988	407.12	408.03	0.91	0.11	0.05	75	<0.5	18.99	0.01	0.07	0.05	<5	0.59	3.01

==> picture [145 x 60] intentionally omitted <==

Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co ppm	Ag g/t	MgO%	Aug/t	Ptg/t	Pdg/t	As ppm	S%	SG
CBDD053B	ECB10989	408.03	408.9	0.87	0.31	0.14	155	0.50	17.91	0.02	0.21	0.12	<5	2.33	3.06
CBDD053B	ECB10990	408.9	409.78	0.88	0.41	0.17	203	0.80	18.74	0.03	0.35	0.17	<5	2.97	3.11
CBDD053B	ECB10991	409.78	410.52	0.74	0.05	0.02	28	<0.5	1.36	0.01	0.01	0.02	5.00	0.36	2.73
CBDD053B	ECB10992	410.52	410.82	0.3	0.46	0.05	221	0.50	12.30	0.01	0.11	0.19	<5	3.55	3.07
CBDD053B	ECB10993	410.82	411.37	0.55	0.08	0.06	51	0.60	10.11	0.01	0.02	0.02	7.00	0.51	2.89
CBDD053B	ECB10994	411.37	412.55	1.18	0.10	0.01	93	<0.5	20.06	0.00	0.01	0.00	<5	0.18	3.08
CBDD053B	ECB10995	412.55	413.7	1.15	0.08	0.01	78	<0.5	18.49	<0.001	0.01	0.01	<5	0.19	3.02
CBDD053B	ECB10996	413.7	414.49	0.79	0.42	0.21	189	1.10	14.92	0.02	0.24	0.17	<5	3.00	3.07
CBDD053B	ECB10997	414.49	415.28	0.79	0.66	1.17	285	5.70	15.06	0.04	0.11	0.40	8.00	5.90	3.20
CBDD053B	ECB10998	415.28	416.04	0.76	0.39	0.28	180	1.30	15.97	0.15	0.04	0.21	8.00	2.80	3.08
CBDD053B	ECB10999	416.04	416.78	0.74	0.12	0.07	72	0.50	12.30	0.04	0.05	0.06	<5	0.72	2.96
CBDD053B	ECB11000	416.78	417.5	0.72	0.23	0.15	121	1.50	15.80	0.12	0.08	0.09	<5	1.54	3.05
CBDD053B	ECB11001	417.5	418.55	1.05	0.07	0.03	71	<0.5	17.41	0.03	0.02	0.03	<5	0.22	3.03
CBDD053B	ECB11002	418.55	419.39	0.84	0.07	0.03	63	<0.5	12.85	0.01	0.03	0.04	<5	0.32	2.98
CBDD053B	ECB11003	419.39	420.35	0.96	0.07	0.03	58	<0.5	10.31	0.03	0.03	0.04	<5	0.37	2.94
CBDD053B	ECB11004	420.35	420.84	0.49	0.09	0.08	72	0.60	13.60	0.02	0.07	0.09	5.00	0.57	3.01
CBDD053B	ECB11005	420.84	421.33	0.49	0.26	0.87	134	4.10	14.34	0.05	0.09	0.17	5.00	2.71	3.12
CBDD053B	ECB11006	421.33	421.81	0.48	0.36	0.61	185	2.60	14.71	0.05	0.34	0.18	<5	3.24	3.16
CBDD053B	ECB11007	421.81	422.23	0.42	0.66	0.71	308	3.90	11.23	1.86	0.41	0.34	7.00	5.53	3.19
CBDD053B	ECB11008	422.23	422.63	0.4	0.80	0.29	384	2.20	8.06	0.02	0.21	0.43	6.00	6.14	3.18
CBDD053B	ECB11009	422.63	423.05	0.42	1.14	0.62	516	4.30	10.11	0.09	0.20	0.72	<5	8.98	3.34
CBDD053B	ECB11010	423.05	423.73	0.68	0.27	0.23	135	1.20	12.90	0.06	0.03	0.17	<5	2.01	3.07
CBDD053B	ECB11011	423.73	424.2	0.47	0.61	1.74	274	7.40	11.72	0.11	0.06	0.42	<5	5.82	3.19
CBDD053B	ECB11012	424.2	424.79	0.59	0.05	0.02	72	<0.5	15.34	0.00	0.00	0.01	6.00	0.20	3.06
CBDD053B	ECB11013	424.79	425.3	0.51	0.37	0.51	181	2.00	14.82	0.07	0.04	0.18	7.00	2.97	3.13
CBDD053B	ECB11014	425.3	425.79	0.49	0.49	0.20	226	1.10	12.80	0.02	0.27	0.14	6.00	3.46	3.12
CBDD053B	ECB11015	425.79	426.28	0.49	0.77	0.40	335	2.30	13.55	0.04	0.26	0.20	<5	6.01	3.25
CBDD053B	ECB11016	426.28	426.64	0.36	1.62	0.55	666	2.80	9.50	0.04	0.38	0.67	<5	13.35	3.46
CBDD053B	ECB11017	426.64	427.36	0.72	0.21	0.04	130	<0.5	13.02	0.01	0.02	0.07	7.00	1.34	3.05
CBDD053B	ECB11018	427.36	428.07	0.71	0.12	0.08	84	<0.5	13.33	0.00	0.01	0.03	6.00	0.79	3.03
CBDD053B	ECB11019	428.07	428.4	0.33	0.18	0.31	109	1.40	12.98	0.01	0.01	0.06	<5	1.42	3.08
CBDD053B	ECB11020	428.4	428.82	0.42	0.10	0.03	84	<0.5	14.19	0.01	0.01	0.01	5.00	0.46	3.07
CBDD053B	ECB11021	428.82	429.17	0.35	0.52	0.17	233	0.70	14.28	0.03	0.13	0.13	<5	3.81	3.17
CBDD053B	ECB11022	429.17	429.51	0.34	0.50	0.37	233	1.80	16.22	0.04	0.08	0.13	6.00	3.66	3.20
CBDD053B	ECB11023	429.51	430.57	1.06	0.08	0.01	83	<0.5	17.16	0.00	0.01	0.01	<5	0.14	3.05
CBDD053B	ECB11024	430.57	431.66	1.09	0.06	0.00	80	<0.5	17.00	0.00	0.00	0.00	<5	0.06	3.05
CBDD053B	ECB11025	431.66	432.33	0.67	0.12	0.13	96	1.10	18.16	0.03	0.01	0.03	<5	0.54	3.07
CBDD053B	ECB11026	432.33	433.04	0.71	0.09	0.02	91	<0.5	18.49	0.01	0.01	0.01	7.00	0.13	3.05
CBDD053B	ECB11027	433.04	433.74	0.7	0.07	0.01	84	<0.5	17.33	0.01	0.00	0.00	<5	0.09	3.05
CBDD053B	ECB11028	433.74	434.04	0.3	0.29	0.28	156	1.70	14.46	0.04	0.02	0.08	<5	1.64	3.10
CBDD053B	ECB11029	434.04	434.67	0.63	0.39	0.16	198	1.00	16.43	0.02	0.01	0.10	<5	2.59	3.16
CBDD053B	ECB11030	434.67	435.33	0.66	0.22	0.10	127	0.70	16.51	0.03	0.03	0.06	<5	1.38	3.07
CBDD053B	ECB11031	435.33	435.63	0.3	0.55	0.34	270	2.30	13.88	0.03	0.58	0.25	<5	3.96	3.19
CBDD053B	ECB11032	435.63	436.19	0.56	0.41	0.48	207	2.70	18.16	0.05	0.02	0.13	<5	3.09	3.18
CBDD053B	ECB11033	436.19	436.79	0.6	0.61	0.19	295	1.20	17.82	0.03	0.08	0.15	5.00	4.25	3.22

==> picture [145 x 60] intentionally omitted <==

Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co ppm	Ag g/t	MgO%	Aug/t	Ptg/t	Pdg/t	As ppm	S%	SG
CBDD053B	ECB11034	436.79	437.29	0.5	0.14	0.21	100	1.00	18.49	0.01	0.02	0.02	<5	0.83	3.11
CBDD053B	ECB11035	437.29	437.7	0.41	0.39	0.12	206	0.80	17.00	0.02	0.57	0.13	<5	2.97	3.19
CBDD053B	ECB11036	437.7	438.01	0.31	0.24	1.30	144	4.90	5.85	0.10	0.08	0.27	11.00	2.83	2.97
CBDD053B	ECB11037	438.01	439.12	1.11	0.03	0.06	61	0.70	8.34	0.02	0.02	0.03	5.00	0.47	3.05
CBDD053B	ECB11038	439.12	440.15	1.03	0.02	0.05	58	0.60	8.27	0.05	0.02	0.03	5.00	0.28	3.05
CBDD053B	ECB11039	440.15	442	1.85	0.01	0.01	62	<0.5	8.26	0.01	0.02	0.02	<5	0.07	3.03
CBDD053B	ECB11040	442	444	2	0.01	0.01	56	<0.5	8.29	0.01	0.02	0.01	<5	0.04	3.03
CBDD053B	ECB11041	444	446	2	0.01	0.01	57	<0.5	8.07	0.01	0.02	0.01	<5	0.03	3.02
CBDD053B	ECB11042	446	448	2	0.01	0.03	58	<0.5	7.48	0.02	0.01	0.02	<5	0.07	3.04
CBDD053B	ECB11043	459.13	460.2	1.07	0.04	0.02	24	<0.5	1.77	0.00	<0.005	0.02	<5	0.19	2.69
CBDD054	ECB11105	380.06	381.42	1.36	0.24	0.13	124	0.90	20.15	0.07	0.15	0.12	<5	1.24	3.07
CBDD054	ECB11106	381.42	382.78	1.36	0.53	0.34	249	1.90	22.14	0.10	0.20	0.28	<5	3.85	3.10
CBDD054	ECB11107	382.78	384.13	1.35	0.26	0.14	134	0.90	21.97	0.05	0.17	0.12	<5	1.71	3.07
CBDD054	ECB11108	384.13	385.36	1.23	0.32	0.18	159	1.00	21.72	0.06	0.08	0.16	<5	2.23	3.05
CBDD054	ECB11109	385.36	387.16	1.8	0.26	0.18	143	1.20	20.48	0.09	0.15	0.11	<5	1.44	3.09
CBDD054	ECB11110	387.16	388.82	1.66	0.13	0.08	83	<0.5	20.48	0.01	0.04	0.04	<5	0.59	3.06
CBDD054	ECB11111	388.82	389.21	0.39	0.72	0.25	356	1.90	16.91	0.01	0.04	0.15	<5	5.24	3.21
CBDD054	ECB11112	389.21	390.76	1.55	0.11	0.03	77	<0.5	19.15	0.02	0.02	0.03	<5	0.40	3.00
CBDD054	ECB11113	390.76	392.3	1.54	0.08	0.02	65	<0.5	17.74	0.01	0.02	0.01	<5	0.20	3.02
CBDD054	ECB11114	392.3	392.67	0.37	1.73	0.21	730	1.60	11.71	0.00	0.02	0.02	<5	14.85	3.49
CBDD054	ECB11115	392.67	394.36	1.69	0.11	0.02	89	<0.5	19.65	0.01	0.04	0.02	<5	0.41	3.05
CBDD054	ECB11116	394.36	394.85	0.49	0.80	1.47	363	5.70	11.86	0.05	0.48	0.19	<5	7.32	3.24
CBDD054	ECB11117	394.85	395.78	0.93	1.86	1.31	811	5.40	7.38	0.19	0.29	0.36	<5	16.35	3.49
CBDD054	ECB11118	395.78	396.52	0.74	1.06	1.94	500	7.60	12.97	0.31	0.26	0.19	<5	9.17	3.31
CBDD054	ECB11119	396.52	397.05	0.53	2.20	0.44	974	1.80	9.57	0.02	0.54	0.29	<5	18.45	3.67
CBDD054	ECB11120	397.05	397.57	0.52	3.23	0.12	1375	1.90	4.34	0.02	0.02	0.41	7.00	28.70	4.06
CBDD054	ECB11121	397.57	397.87	0.3	0.48	0.54	228	1.80	8.59	0.02	0.02	0.05	<5	3.03	3.04
CBDD054	ECB11122	397.87	398.98	1.11	3.92	0.16	1710	0.80	2.09	0.03	0.02	0.58	<5	32.30	4.20
CBDD054	ECB11123	398.98	400.75	1.77	0.84	0.44	389	1.80	14.72	0.04	0.27	0.21	<5	5.82	3.24
CBDD054	ECB11124	400.75	401.11	0.36	2.59	0.24	1150	2.00	6.60	0.05	2.20	0.75	5.00	22.90	3.24
CBDD054	ECB11125	401.11	402.3	1.19	0.58	0.25	277	1.20	15.04	0.02	0.26	0.25	<5	4.60	3.21
CBDD054	ECB11126	402.3	402.87	0.57	0.16	0.02	106	<0.5	9.75	0.00	0.00	0.02	<5	1.14	2.95
CBDD054	ECB11127	402.87	404.15	1.28	0.22	0.16	123	0.80	10.98	0.03	0.08	0.10	<5	1.76	3.04
CBDD054	ECB11128	404.15	404.66	0.51	0.53	0.39	255	1.80	15.06	0.05	0.17	0.18	<5	4.18	3.22
CBDD054	ECB11129	404.66	405.41	0.75	0.90	0.18	417	0.80	15.67	0.01	0.08	0.24	<5	6.84	3.26
CBDD054	ECB11130	405.41	405.71	0.3	1.74	0.11	766	1.10	9.43	0.01	0.03	0.23	<5	13.25	3.54
CBDD054	ECB11131	405.71	407.38	1.67	0.17	0.05	112	<0.5	8.79	0.01	0.40	0.03	<5	1.28	3.07
CBDD054	ECB11132	407.38	409.05	1.67	0.08	0.12	75	0.80	9.15	0.03	0.03	0.04	<5	0.66	3.12
CBDD054	ECB11133	409.05	409.35	0.3	0.20	0.79	128	3.80	7.58	0.10	0.02	0.07	<5	2.31	3.11
CBDD054	ECB11134	409.35	410.7	1.35	0.02	0.03	54	<0.5	8.84	0.01	0.02	0.02	<5	0.17	3.07
CBDD054	ECB11135	410.7	412.05	1.35	0.06	0.11	66	1.10	7.68	0.04	0.03	0.03	<5	0.39	3.05
CBDD054	ECB11136	412.05	414.05	2	0.01	0.01	48	<0.5	7.53	0.01	0.02	0.01	<5	0.06	3.01
CBDD054	ECB11137	414.05	416.05	2	0.01	0.03	52	<0.5	8.09	0.01	0.02	0.02	<5	0.09	3.05
CBDD054	ECB11138	416.05	416.92	0.87	0.08	0.06	58	<0.5	6.10	0.03	0.03	0.06	<5	0.65	2.96
CBDD054	ECB11139	416.92	417.35	0.43	0.65	0.24	320	1.40	5.97	0.01	0.03	0.24	<5	4.87	3.26

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Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co ppm	Ag g/t	MgO%	Aug/t	Ptg/t	Pdg/t	As ppm	S%	SG
CBDD054	ECB11140	417.35	419.35	2	0.04	0.12	56	1.30	7.15	0.08	0.05	0.05	<5	0.30	3.06
CBDD054	ECB11141	419.35	421.35	2	0.05	0.38	53	2.00	6.32	0.07	0.03	0.04	<5	0.53	3.05
CBDD054	ECB11142	421.35	423.27	1.92	0.01	0.07	54	0.70	7.76	0.02	0.03	0.02	<5	0.15	3.06
CBDD054	ECB11143	423.27	423.63	0.36	0.08	0.68	66	9.70	5.85	0.77	0.07	0.06	<5	1.23	3.08
CBDD054	ECB11144	423.63	425.63	2	0.01	0.02	51	<0.5	8.42	0.01	0.02	0.01	<5	0.03	3.05
CBDD054	ECB11145	425.63	427.63	2	0.01	0.02	50	<0.5	8.32	0.01	0.01	0.01	<5	0.04	3.04
CBDD054	ECB11146	427.63	429.63	2	0.01	0.06	55	0.60	7.30	0.04	0.02	0.02	<5	0.13	3.04
CBDD054	ECB11147	429.63	430.2	0.57	0.04	0.17	55	1.90	7.05	0.09	0.02	0.08	<5	0.89	3.13
CBDD054	ECB11148	430.2	432.04	1.84	0.03	0.07	53	<0.5	7.61	0.01	0.02	0.04	<5	0.93	2.99
CBDD054	ECB11149	432.04	434.04	2	0.01	0.01	55	<0.5	6.86	0.01	0.02	0.02	<5	0.09	2.99
CBDD054B	ECB11222	237.18	237.89	0.71	0.16	0.03	124	<0.5	28.93	0.02	0.02	0.01	<5	0.13	3.16
CBDD054B	ECB11223	237.89	238.56	0.67	0.20	0.03	156	<0.5	33.08	0.02	0.02	0.02	<5	0.16	3.25
CBDD054B	ECB11224	238.56	239.47	0.91	0.13	0.02	112	<0.5	27.86	0.01	0.01	0.01	<5	0.09	3.06
CBDD054B	ECB11225	239.47	240.1	0.63	0.11	0.03	96	<0.5	26.86	0.02	0.01	<0.001	<5	0.12	3.00
CBDD054B	ECB11226	300.98	302.4	1.42	0.00	0.01	13	<0.5	1.31	0.00	<0.005	<0.001	<5	0.31	2.69
CBDD054B	ECB11227	302.4	303.82	1.42	0.00	0.00	10	<0.5	1.34	0.00	<0.005	0.00	<5	0.02	2.69
CBDD054B	ECB11228	303.82	305.18	1.36	0.01	0.01	30	<0.5	4.61	0.00	<0.005	0.00	<5	0.05	2.82
CBDD054B	ECB11229	349.85	351.85	2	0.12	0.01	87	<0.5	21.31	0.00	0.02	0.02	<5	0.15	3.02
CBDD054B	ECB11230	351.85	353.85	2	0.15	0.04	98	<0.5	22.38	0.01	0.04	0.03	<5	0.43	3.03
CBDD054B	ECB11231	353.85	354.4	0.55	0.20	0.06	123	<0.5	21.22	0.01	0.10	0.04	<5	0.79	3.05
CBDD054B	ECB11232	354.4	355.7	1.3	0.36	0.22	192	0.80	19.48	0.02	0.32	0.12	<5	2.46	3.14
CBDD054B	ECB11233	355.7	357	1.3	0.25	0.11	141	<0.5	18.74	0.02	0.21	0.10	<5	1.44	3.13
CBDD054B	ECB11234	357	357.52	0.52	1.18	1.07	587	4.00	13.03	0.02	0.81	0.65	<5	7.81	3.39
CBDD054B	ECB11235	357.52	357.95	0.43	0.32	0.14	173	<0.5	17.24	0.01	0.07	0.21	<5	2.27	3.14
CBDD054B	ECB11236	357.95	358.3	0.35	0.07	0.03	57	<0.5	11.57	0.00	0.02	0.03	<5	0.41	2.98
CBDD054B	ECB11237	358.3	358.6	0.3	0.19	0.31	110	0.50	16.75	0.05	0.05	0.10	<5	1.40	3.09
CBDD054B	ECB11238	358.6	359.43	0.83	1.17	0.91	603	3.40	13.45	0.02	0.14	0.68	<5	8.05	3.36
CBDD054B	ECB11239	359.43	359.87	0.44	0.65	0.80	329	2.50	17.74	0.02	0.42	0.32	<5	5.14	3.22
CBDD054B	ECB11240	359.87	360.17	0.3	2.14	0.49	1010	3.30	7.05	0.02	1.23	0.85	<5	19.90	3.71
CBDD054B	ECB11241	360.17	361.3	1.13	0.85	0.33	411	0.90	12.82	0.05	1.46	0.30	<5	5.64	3.25
CBDD054B	ECB11242	361.3	362.25	0.95	1.13	0.76	516	2.40	12.44	0.09	0.52	0.42	<5	6.53	3.37
CBDD054B	ECB11243	362.25	362.55	0.3	0.20	0.19	122	0.50	14.41	0.30	0.03	0.06	<5	1.46	3.11
CBDD054B	ECB11244	362.55	363.56	1.01	1.61	1.07	744	3.60	11.19	0.03	0.53	0.50	<5	13.90	3.50
CBDD054B	ECB11245	363.56	364.8	1.24	0.38	0.93	208	3.10	8.99	0.03	0.21	0.11	<5	3.14	3.09
CBDD054B	ECB11246	364.8	365.93	1.13	0.55	0.72	273	3.00	14.59	0.45	0.16	0.17	<5	4.33	3.22
CBDD054B	ECB11247	365.93	367.88	1.95	0.07	0.01	71	<0.5	16.30	0.00	0.00	0.00	<5	0.07	3.03
CBDD054B	ECB11248	367.88	368.33	0.45	0.54	0.17	267	<0.5	11.94	0.01	0.04	0.15	<5	3.79	3.14
CBDD054B	ECB11249	368.33	368.63	0.3	3.49	0.08	1535	<0.5	2.74	0.01	0.02	0.87	<5	29.80	4.16
CBDD054B	ECB11250	368.63	369.67	1.04	1.22	0.47	542	1.30	11.95	0.02	0.13	0.37	<5	7.91	3.37
CBDD054B	ECB11251	369.67	371.67	2	1.39	1.38	622	4.40	11.28	0.09	0.72	0.41	<5	9.85	3.43
CBDD054B	ECB11252	371.67	373.15	1.48	1.34	2.05	634	7.90	10.36	0.09	0.44	0.47	<5	13.95	3.47
CBDD054B	ECB11253	373.15	374.12	0.97	0.48	0.31	249	1.00	15.14	0.02	0.13	0.20	<5	3.63	3.17
CBDD054B	ECB11254	374.12	375.68	1.56	0.37	0.27	186	0.70	14.97	0.02	0.13	0.16	<5	2.67	3.08
CBDD054B	ECB11255	375.68	376.11	0.43	1.06	0.12	470	<0.5	10.84	0.01	0.20	0.54	<5	7.29	3.26
CBDD054B	ECB11256	376.11	377.2	1.09	0.06	0.04	52	<0.5	7.61	0.01	0.02	0.03	<5	0.45	2.95

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Hole_ID	SampleID	mFrom	mTo	Interval	Ni%	Cu%	Co ppm	Ag g/t	MgO%	Aug/t	Ptg/t	Pdg/t	As ppm	S%	SG
CBDD054B	ECB11257	377.2	378.19	0.99	0.61	0.38	281	0.80	10.18	0.03	0.24	0.25	<5	3.55	3.14
CBDD054B	ECB11258	378.19	379.93	1.74	0.06	0.10	57	<0.5	8.72	0.01	0.01	0.03	<5	0.46	2.97
CBDD054B	ECB11259	379.93	380.23	0.3	0.01	0.02	22	<0.5	3.61	0.02	0.00	0.01	<5	0.11	2.76
CBDD054B	ECB11260	380.23	380.64	0.41	0.22	0.04	115	<0.5	5.01	0.01	0.05	0.09	<5	1.70	2.88
CBDD054B	ECB11261	380.64	381.22	0.58	0.10	0.07	76	<0.5	12.78	0.02	0.12	0.02	<5	0.55	3.09
CBDD054B	ECB11262	381.22	381.95	0.73	1.74	0.23	783	<0.5	11.74	0.02	0.23	0.43	<5	14.40	3.50
CBDD054B	ECB11263	381.95	382.32	0.37	0.55	0.24	257	1.20	13.76	0.03	0.06	0.14	<5	3.94	3.05
CBDD054B	ECB11264	382.32	384.2	1.88	0.04	0.04	63	<0.5	8.04	0.01	0.02	0.02	<5	0.28	3.03
CBDD054B	ECB11265	384.2	386.06	1.86	0.02	0.02	53	<0.5	7.94	0.01	0.02	0.02	<5	0.13	3.05
CBDD054B	ECB11266	386.06	388.06	2	0.03	0.02	45	<0.5	5.72	0.01	0.01	0.01	<5	0.19	2.89
CBDD054B	ECB11267	388.06	390.06	2	0.02	0.03	57	<0.5	7.10	0.02	0.02	0.02	<5	0.15	3.04
CBDD054B	ECB11268	395.2	395.75	0.55	0.03	0.25	61	2.80	5.01	0.35	0.04	0.16	<5	0.47	2.94
CBDD054B	ECB11269	409.05	410.28	1.23	0.01	0.02	58	<0.5	7.44	0.01	0.02	0.01	<5	0.08	3.02
CBDD054B	ECB11270	410.28	411.68	1.4	0.01	0.02	53	<0.5	7.91	0.01	0.01	0.02	<5	0.13	3.02

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APPENDIX 1 JORC TABLE 1 - JORC CODE, 2012 EDITION – TABLE 1 Section 1 Sampling Techniques and Data

(Criteria in this section apply to all succeeding sections.)

Criteria	JORC Code explanation	Commentary
Sampling	Nature and quality of sampling (e.g. cut	DD core samples have been half cut with an automatic
techniques	channels, random chips, or specific	core saw.
	specialised industry standard	0.25m-1.1m samples are collected from the core trays as
	measurement tools appropriate to the	marked out by the supervising geologist.
	minerals under investigation, such as	A handheld XRF tool was used to verify the mineralisation
	down hole gamma sondes or handheld	with samples reporting >0.3% Ni in disseminated zones
	XRF instruments, etc.). These	and >1% Ni in the matrix sulphide zones.
	examples should not be taken as	XRF results have not been reported and are used as a
	limiting the broad meaning of sampling.	logging/sampling verification tool only.
	Include reference to measures taken to	Core is cut and sampled to ensure the sample is
	ensure sample representivity and the	representative and no bias is introduced. Cutting of
	appropriate calibration of any	specific, banded or stringer sulphide zoned core is done
	measurement tools or systems used.	orthogonal to the banding to ensure there is no bias.
	Aspects of the determination of	Determination of mineralisation has been based on
	mineralisation that are material to the	geological logging, visual sulphide estimates and
	Public Report.	confirmation using a pXRF machine. Samples were
		dispatched to an accredited laboratory for multi-element
		analysis.
		.
	In cases where ‘industry standard’ work	Diamond core drilling was used to obtain 3m length
	has been done this would be relatively	samples from the core barrel which are then marked in
	simple (e.g. ‘reverse circulation drilling	one meter intervals, based on core block measurements.
	was used to obtain 1 m samples from	Samples are selected based on geological logging
	which 3 kg was pulverised to produce a	boundaries or on nominal meter marks.
	30g charge for fire assay’). In other	Collected samples weigh a nominal 2-3 kg (depending on
	cases more explanation may be	sample length).
	required, such as where there is coarse	Samples have been dispatched to an accredited
	gold that has inherent sampling	commercial laboratory in Perth for analysis.
	problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information	Samples are being analysed using a 4-acid digest, ME- ICP for 33 elements and ore zone samples are also being tested for Au & PGE elements using ICP analysis.
Drilling	Drill type (e.g. core, reverse circulation,	Drilling was undertaken using NQ2 sized drill core.
techniques	open-hole hammer, rotary air blast,	Holes have been collared with mud rotary from surface,
	auger, Bangka, sonic, etc) and details	HQ rough cored to top of fresh rock then NQ2 cored to
	(e.g. core diameter, triple or standard	EOH.
	tube, depth of diamond tails, face-
	sampling bit or other type, whether core
	is oriented and if so, by what method,
	etc).
Drill sample	Method of recording and assessing	Core recovery was recorded by the field crew and verified
recovery	core and chip sample recoveries and	by the geologist.
	results assessed.	RQD measurements were digitally recorded to ensure
	Measures taken to maximise sample	recovery details were captured.
	recovery and ensure representative	Sample recovery in all mineralised zones is high with
	nature of the samples.	negligible core loss observed.
	Whether a relationship exists between	Diamond core drilling is the highest standard and no
	sample recovery and grade and	relationship has been established between sample
	whether sample bias may have	recovery and reported grade as the core is in very good
	occurred due to preferential loss/gain of	condition.
	fine/coarse material.

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Criteria	JORC Code explanation Commentary
Logging	Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. The total length and percentage of the relevantintersectionslogged. Detailed industry standard of collecting core in core trays, marking meter intervals & drawing core orientation lines was undertaken. Core trays were photographed wet and dry prior to sampling. Drill hole logs are recorded in Excel spread sheets and validated in Micromine Software as the drilling progresses. The entire length of all holes is logged.
Sub- sampling techniques and sample preparation	If core, whether cut or sawn and whether quarter, half or all core taken. If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. For all sample types, the nature, quality and appropriateness of the sample preparation technique. Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples. Measures taken to ensure that the sampling is representative of the in-situ material collected, including for instance results for field duplicate/second-half sampling. Whether sample sizes are appropriate to the grain size of the material being sampled. Core is half cut using an automatic core saw to achieve a half-core sample for laboratory submission. The sample preparation technique is considered industry best standard practice. No field duplicates have been collected in this program. Field duplicates will be collected once initial results are returned and resampling of the mineralised zones is warranted. Sample sizes are appropriate to the grain size of the mineralisation.
Quality of assay data and laboratory tests	For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc. Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established. No handheld XRF results are reported however the tool was used to verify the mineralisation with reporting >0.3% Ni in disseminated zones and >1% Ni in the matrix sulphide zones. DHTEM parameters are as follows;  Tx Loop size: 500 x 800 m  Transmitter: GAP HPTX-70  Receiver: EMIT SMARTem24  Sensor: EMIT DigiAtlantis  Station spacing: 2m to 10m  Tx Freq: 0.5 Hz  Duty cycle: 50%  Current: ~130 Amp  Stacks: 32-64  Readings: 2-3 repeatable readings per station
Verification of sampling and assaying	The verification of significant intersections by either independent or alternative company personnel. Results verified internally by Company personnel
	The use of twinned holes. Hole CBDD0028 is twinning hole CBP042. No other twinningiswarranted at this stage.
	Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. The data was collected and logged using Excel spreadsheets and validated using Micromine Software. The data will be loaded into an externally hosted and managed database.
	Discuss any adjustment to assay data. No adjustments have been made to the assay data other than length weighted averaging.

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Criteria	JORC Code explanation Commentary
Location of data points	Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation. The holes were pegged using a hand-held GPS+3m The rig was setup over the nominated hole position and final GPS pickup occurred at the completion of the hole. Holes are progressively surveyed by DGPS on a batch basis.
	 Specificationofthe grid systemused. MGA94_51
	Quality and adequacy of topographic control. Topography is relatively flat and control is more than adequate given the early stage of the project. A 3D drone ortho-photographic survey had been used to create a DTMofthe project area.
Data spacing and distribution	Data spacing for reporting of Exploration Results. Refer to Cross Sections and Plans included
	Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. Not applicable, no Mineral Resource is being stated.
	Whether sample compositing has been applied No compositing has been applied. Intercepts are quoted aslength weightedintervals.
Orientation of data in relation to geological structure	Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material. The drill hole orientation does not introduce a sample bias.
Sample security	The measures taken to ensure sample security. Samples are in the possession of Estrella’s personnel from field collectiontolaboratory submission.
Audits or reviews	The results of any audits or reviews of sampling techniques and data. No audits or reviews have been conducted for this release giventhe early stage ofthe project.

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Section 2 Reporting of Exploration Results

(Criteria listed in the preceding section also apply to this section.)

Criteria	JORC Code explanation	Commentary
Mineral	Type, reference name/number,	Carr Boyd Nickel Pty Ltd (a wholly owned subsidiary of
tenement and	location and ownership including	ESR) holds a 100% interest in the nickel and base metal
land tenure	agreements or material issues with	rights to the project.
status	third parties such as joint ventures,	There are no known impediments to operate in the area.
	partnerships, overriding royalties,
	native title interests, historical sites,
	wilderness or national park and
	environmental settings.
	The security of the tenure held at the
	time of reporting along with any
	known impediments to obtaining a
	licence to operateinthe area.
Exploration	Acknowledgment and appraisal of	The Carr Boyd Rocks deposit was discovered by Great
done by other	exploration by other parties.	Boulder Mines, in a joint venture with North Kalgurli Ltd
parties		in 1968. The deposit was mined between 1972 and
		1975, during which time they explored for additional
		breccia pipe occurrences near the mine.
		WMC acquired Great Boulder Mines Ltd in 1975, briefly
		reopening the mine in 1977 before closing it permanently
		shortly thereafter due to a collapse in the nickel price.
		The mine had produced 210,000t at 1.44% Ni and 0.46%
		Cu before its closure.
		From 1968 Pacminex Pty Ltd held most of the ground
		over the CBLC outside of the immediate mine area.
		Between 1968 and 1971 they conducted extensive
		exploration programs searching for large basal contact
		and/or stratabound Ni-Cu deposits. It was during this
		time that most of the disseminated and cloud sulphide
		occurrences such as those at Tregurtha, West Tregurtha
		and Gossan Hill were discovered.
		Defiance Mining acquired the regional tenements from
		Pacminex in 1987 and focused on exploration for PGE
		deposits between 1987 and 1990. In 1990 Defiance
		purchased the Carr Boyd Rocks mine from WMC and
		switched focus to the mine area between 1990 and 2001,
		leaving many PGE targets untested.
		From 1990 Defiance dewatered the mine to conduct
		testwork and feasibility studies on the remnant
		mineralisation. Metallurgical testwork, Mineral Resource
		estimations, and scoping studies were completed.
		Around 1996 the focus shifted again to regional
		exploration for large tonnage basal contact deposits.
		In 2001 Titan Resources Ltd (Titan) acquired the project
		and recommenced economic evaluations of the remnant
		material at Carr Boyd Rocks before embarking on
		another regional exploration program focusing on the
		basal contact. An aeromagnetic survey, airborne EM
		reprocessing, and several programs of RAB and RC
		drilling were completed.
		From 2005 Yilgarn Mining entered a JV with Titan and
		continued with some regional exploration, but focused
		most attention in and around the Carr Boyd Rocks mine.
		In 2007 Titan was acquired by Consolidated Minerals Ltd
		(Consmin). Consmin conducted IP surveys and detailed
		gravity surveys, but did not drill any targets before selling
		the project to Salt Lake Mining (SLM) in 2013. SLM
		completed limited drilling to meet expenditure

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Criteria	JORC	Code explanation	Code explanation	Code explanation				Commentary
								commitments, before selling the project to Apollo
								Phoenix Resources in 2016.
								Apollo sold the project to ESR in 2018.
Geology	Deposit type,		geological setting				and	The Carr Boyd project lies within the Achaean Yilgarn
	style of mineralisation.							Craton in a 700km belt of elongate deformed and folded
								mafic, ultramafic rocks and volcanic sediments intruded
								by granitoids which is referred to as the Norseman-
								Wiluna Belt. The belt has been divided into several
								geological distinct terranes, with the project area lying at
								the northern end of the Gindalbie terrane (Swager, 1996).
								The geology of the Carr Boyd area is dominated by the
								Carr Boyd mafic-ultramafic intrusive complex (CBIC).
								Several distinctive styles of Ni and Ni-Cu mineralisation
								have been identified within the CBIC. At the Carr Boyd
								Rocks Nickel Mine Ni-Cu mineralisation is hosted within
								several 20 - 60m diameter brecciated pipe-like bodies
								that appear to be discordant to the magmatic
								stratigraphy. Mineralisation is hosted by a matrix of
								sulphides (pyrrhotite, pentlandite, pyrite and
								chalcopyrite) within brecciated Bronzite and altered
								country rock clasts.
								Stratiform Ni-Cu-PGE mineralisation has been identified
								at several different locations within the layered magmatic
								complex.
								Estrella is in the process of re-mapping and reclassifying
								the Carr Boyd Igneous Complex. Previous “Layered
								Intrusive” models are misleading as the complex is made
								up of many overprinted and juxtaposed, smaller layered
								and non-layered intrusives that have progressed from
								Ultramafic to Mafic over time. The complex is better
								described as a magma feeder zone, where the earliest
								melts passing through the Morelands Formation have
								assimilated graphitic sulphidic shales, reached sulphur
								saturation and deposited nickel sulphides along basal
								contacts.
								These basal contacts are not restricted to the base of the
								complex, but can form within the complex, wherever
								access was gained by these earlier flows.
								The complex has then been intruded and inflated over
								time by progressively more mafic, barren magmas to
								produce what we see today.
Drill hole	A	summary	of	all	information			All relevant drillhole information can be found in the
Information	material to the understanding of						the	Tables and sections within the announcement.
	exploration		results		including		a
	tabulation		of	the		following
	information for all Material						drill
	holes:
	o	easting and northing of					the
		drill hole collar
	o	elevation or RL (Reduced
		Level	– elevation above				sea
		level	in metres) of the				drill
		hole collar
	o	dip and azimuth of				the hole
	o	down	hole		length		and
		interception		depth
	o	hole length.

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Criteria	JORC Code explanation Commentary
	If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case. No information is excluded.
Data aggregation methods	In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g. cutting of high grades) and cut-off grades are usually Material and should be stated. Where aggregate intercepts incorporate short lengths of high- grade results and longer lengths of low-grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown indetail. Intersections are reported on a 0.5% Ni cut-off with SG and length weighted intervals. All intercepts are reported using SG and length weighted intervals.
	The assumptions used for any reporting of metal equivalent values should be clearly stated. No metal equivalents have been stated
Relationship between mineralisation widths and intercept lengths	These relationships are particularly important in the reporting of Exploration Results. If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g. ‘down hole length, true width not known’). True widths have not been stated. The variable orientation of mineralisation within magma feeders combined with a structural overprint and steep drill angles make true width calculations highly misleading.
Diagrams	Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views. Maps and sections with drill hole locations are included in the announcement.
Balanced reporting	Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results. All new drillhole information within this announcement is reported
Other substantive exploration data	Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk Everything meaningful and material is disclosed in the body of the report. Geological observations are included in the report. No bulk samples, metallurgical, bulk density, groundwater, geotechnical and/or rock characteristics test were carried out.

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Criteria	JORC Code explanation	Commentary	Commentary
	samples – size and method of		There are no known potential deleterious or contaminating
	treatment; metallurgical test results;		substances.
	bulk density, groundwater,
	geotechnical and rock
	characteristics; potential deleterious
	orcontaminating substances.
Further work	The nature and scale of planned		Diamond drilling and DHTEM geophysical testing is
	further work (e.g. tests for lateral		continuing.
	extensions or depth extensions or
	large-scale step-out drilling).
	Diagrams clearly highlighting the
	areas of possible extensions,
	including the main geological
	interpretations and future drilling
	areas, provided this information is
	not commercially sensitive.