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RAIDEN RESOURCES LIMITED — Regulatory Filings 2021
May 6, 2021
65675_rns_2021-05-06_03826163-887b-4d55-9447-af5a9b1adf2a.pdf
Regulatory Filings
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FIELD PROGRAMS COMMENCE AT MT SHOLL AND BOODALYERRIE
HIGHLIGHTS
Field programs have commenced at Raiden's Mt Sholl (100% RDN) and Boodalyerrie (100% RDN) properties in the Pilbara region of Western Australia.
Mt Sholl
- Located 10 kilometres northeast of Artemis Resources (ASX:ARV) Radio Hill Ni-Cu mine and associated infrastructure
- Covers part of the Mt Sholl intrusive complex, which hosts widespread Ni-Cu-PGE mineralisation
- Extensive historical exploration for Ni-Cu-(PGE), with drill intercepts including:
- o 20m at 0.88% Ni, 1.05% Cu, 0.78 g/t Pd from 3 metres
- o 17m at 0.91% Ni, 1.11% Cu, 0.62 g/t Pd from 137 metres
- o 13m at 1.18% Ni, 1.02% Cu from 72.2 metres
- Limited historical exploration for Au, which included drilling 700m strike of shallow workings; intercepts include:
- o 10m at 2.21 g/t Au from 11 metres, includes 1m @ 15.9 g/t Au from 16 metres
- o 1m @ 13 g/t Au from 48 metres
Boodalyerrie
- Covers a large area of hydrothermal alteration and a suite of prominent quartz veins in a Paleoarchean granitoid complex
- Historic surface sampling defined extensive anomalies
- Individual historic gold-in-soil anomalies are up to two kilometres long and several hundred metres across
QUICK STATS ASX Code: RDN DAX Code: YM4
BOARD & MANAGEMENT
Non- Executive Chairman Mr Michael Davy
Managing Director Mr Dusko Ljubojevic
Non-Executive Directors Mr Martin Pawlitschek
Company Secretary Ms Kyla Garic
ASSET PORTFOLIO
SERBIA
Cu, Co & Au (~269km2 )
BULGARIA
Cu, Au & Ag (~409km2 )
AUSTRALIA Au, Cu, Ni & PGE (~823km2
)

Mr Dusko Ljubojevic, Managing Director of Raiden commented:
"We have recently consolidated our ownership of the Pilbara portfolio and now have 100% exposure to the discovery upside on this portfolio. These initial programs at both, Boodalyerrie and Mt Sholl will assist in in determining the follow up and more aggressive exploration programs to come. At Mt Sholl, historical data reviews have outlined further gold potential, which the Company was not aware of and presents us with an additional prospect to follow up on. In conjunction, we will also aim to define next steps in advancing the Ni-Cu-PGE targets. This may include drill testing of new targets and defining the extent of the know mineralisation at depth and along strike. Our planned work at Boodalyerrie, aims to understand the relationship of the bonanza grade historical results and the broader gold in soil anomalism. We are also anticipating the results from the aero-magnetic survey which we completed over the northern license of the Arrow project, which will assist the Company in delineating the maiden drill program at Arrow, where we are targeting Hemi style gold mineralisation."
Raiden Resources Limited (ASX: RDN) ("Raiden" or "the Company") is pleased to announce that field work has commenced on the Mt Sholl and Boodalyerrie properties in the Pilbara region of Western Australia.

Figure 1: Pilbara property portfolio and significant deposits in the district
Mt Sholl
Raiden holds 100% of the Mt Sholl property, which incorporates two granted exploration licences covering 10 km2 . Mt Sholl is located 22 kilometres south of Karratha and 10 kilometres northeast of Artemis Resources' (ASX:ARV) Radio Hill nickel-copper-PGE mine and associated processing infrastructure (figure 2). Licences cover part of the Mt Sholl layered mafic-ultramafic intrusive complex, which hosts widespread Ni-Cu-PGE mineralisation as disseminated, matrix, stringer and massive pyrrhotite-pentlandite-chalcopyrite.



Historical exploration has defined two Ni-Cu-PGE prospects on the properties, namely Mt Sholl A1 and Mt Sholl B1 (figure 3). Both are substantial accumulations of sulphide mineralisation in lenses up to 20 metres wide that plunge moderately to the northeast. Figure 4 is a cross section of the Mt Sholl A1 sulphide body, looking west.
A total of 190 percussion and diamond holes targeting Ni-Cu mineralisation have been drilled on the property, for 20,060 metres. Numerous significant intercepts were returned, including:
- 20m at 0.88% Ni, 1.05% Cu, 0.78 g/t Pd from 3 metres in B1RC149
- 17m at 0.91% Ni, 1.11% Cu, 0.62 g/t Pd from 137 metres in A1RC11
- 13m at 1.18% Ni, 1.02% Cu from 72.2 metres in 86SPD343
- 24m at 0.69% Ni, 1.07% Cu, 0.64 g/t Pd from 15 metres in B1MET1
- 27m at 0.50% Ni, 0.82% Cu, 0.86 g/t Pd from 54 metres in B1RC102
- 24m at 0.62% Ni, 0.95% Cu, 0.77 g/t Pd from 3 metres in B1RC121
- 18m at 0.41% Ni, 0.82% Cu, 0.94 g/t Pd from 150 metres in A1RC6
- 15.8m at 0.73% Ni, 0.97% Cu from 115 metres in 86SPD337
- 1m @ 5.7% Ni, 0.73% Cu, 2.3 g/t Pd from 78 metres in B1RC118
True width is not known at this time, therefore the intercepts quoted are downhole intercept widths. A full list of historic drill holes that targeted Ni-Cu mineralisation on the Mt Sholl licences, with intercepts, is provided in Table 1. If no Cu, Ni, Pd or Pt assay is reported then the samples were not assayed for those elements.


Figure 3: Mt Sholl property interpreted geology and historic drillhole collar locations
Historical work also included trial mining at the Mt Sholl B1 prospect. In the 2017 surrender report for their mining licence over the prospect (WAMEX: A111917), Fox Resources (ASX:FXR) reported that Mt Sholl B1 ore was blended with run of mine ore from Radio Hill prior to processing through the Radio Hill mill and precise production and reconciliation figures for Mt Sholl B1 trial mining were not recorded.


Figure 4: Mt Sholl A1 sulphide lens and historic drilling, looking west. Sulphide lens defined above 0.75% Ni+Cu
Despite the fact that the majority of historical exploration work at Mt Sholl targeted Ni-Cu-PGE mineralisation, the project area is also prospective for orogenic style gold mineralisation in association with the Sholl Shear Zone and subsidiary structures. At the Radleys Find (Radleys) Prospect, a series of shallow historic workings were drill tested over a 700 metre strike length by Agip Australia in the 1980s. A total of 45 RC holes were drilled, for 2144 metres. Further historic workings are located 1.3 kilometres along strike east-southeast of Agip's drillholes, where historic grab samples collected from dumps returned up to 48 g/t Au. A further 1.5 kilometres along strike to the east-southeast, a historic soil sample returned a gold value of 0.24 g/t. On the basis of this historic work, the Company infers that the potential strike of the mineralised structure could exceed 3.5 kilometres (Radleys gold trend on figure 3) and warrants additional work.
At Radleys, chlorite-(sericite)-(biotite) altered amygdaloidal basalt is cut by an intermittently developed sinuous quartz reef which is reportedly between 1-3 metres wide. Drilling tested up to 50 metres below surface and returned a best intercept of 10m @ 2.21 g/t Au from 11 metres, including 1m @ 15.9 g/t Au from 16 metres in hole 87RP26. True width is not known, so downhole

intercept widths are quoted. A full list of holes drilled at Radleys, with intercepts, is provided in Table 2. Figure 5 is a schematic cross section of historical drilling results.

Figure 5: Radleys schematic cross section
Field Program - Mt Sholl
Work has commenced at Mt Sholl, with Raiden personnel conducting reconnaissance geological mapping as part of an initial assessment to determine potential for additional Ni-Cu-PGE mineralisation and to evaluate the Radleys gold trend. The company's geologists plan to map the areas of interest and collect selective grab samples.
Boodalyerrie Project
Raiden holds a 100% interest in the Boodalyerrie property, which comprises of one granted exploration licence covering an area of 57 km2 . Boodalyerrie is located 120 kilometres eastsoutheast of Marble Bar and 75 kilometres northeast of Nullagine (figure 6). The licence covers


much of the Boodalyerrie Mining Centre, which has historical recorded production between 1901 and 1910 of 588.4 ounces of gold from 122 tonnes of ore at an average grade of 150 g/t.
Boodalyerrie covers a large area of hydrothermal alteration in the Yilgalong Granitoid associated with a suite of prominent quartz veins. Historical exploration has been limited to surface sampling programs - stream sediment, soil and rock sampling. Rock samples collected by previous explorers returned gold values ranging up to 200 g/t Au and a chip-channel sample across a historic mine face reportedly returned 3 metres at 88.6 g/t Au. Soil sampling in 2013 defined widespread +25 ppb gold anomalies, the largest of which is 2 kilometres long and several hundred metres across (figure 7). Assay data for the soil samples is not available and the methods of collection, analytical techniques and QA/QC for the program are not known.
Raiden's planned field program includes the collection of grid-based soil samples across the largest of the historic soil anomalies, with objectives being to confirm the historical results, define the anomalies in more detail and to attempt to determine the relationship between soil anomalism and the prominent quartz veins.
Field Program - Boodalyerrie
Work at Boodalyerrie will commence on completion of the Mt Sholl field work. Raiden personnel will conduct reconnaissance geological mapping across the historic soil anomalies and visit recorded locations for historic anomalous rock samples. The field crew will collect selective grab samples from prospective outcrops to determine mineralisation relationships.
A program of soil sampling will also be implemented, with samples collected at 50 metre centres along east-west oriented lines spaced 200 metres apart (figure 7). A total of 335 primary samples will be collected.


Figure 6: Boodalyerrie district interpreted geology



Table 1: Mt Sholl historic drillholes targeting Ni-Cu mineralisation
| Hole | Area | E_GDA94 | N_GDA94 | Depth (m) | Azimuth | Dip | Intercept* |
|---|---|---|---|---|---|---|---|
| 06RZDD001 | A1 | 492390 | 7687164 | 147.30 | 180 | -75 | 18.5m @ 0.68% Ni, 0.64% Cu, 0.68 g/t Pd, 0.12 g/t Pt from 114.5m |
| 06RZDD002 | A1 | 492590 | 7687355 | 321.20 | 180 | -75 | 8m @ 0.29% Ni, 0.41% Cu, 0.15 g/t Pd, 0.07g/t Pt from 238m |
| 06RZDD002 | 11.6m @ 0.36% Ni, 0.42% Cu, 0.17 g/t Pd, 0.08 g/t Pt from 251.4m | ||||||
| 06RZDD003 | A1 | 492440 | 7687210 | 174.60 | 180 | -75 | 18.7m @ 0.51% Ni, 0.78% Cu, 0.36 g/t Pd, 0.13 g/t Pt from 147m |
| 06RZDD004 | A1 | 492365 | 7687141 | 132.50 | 180 | -75 | 17m @ 0.55% Ni, 0.90% Cu, 0.66 g/t Pd, 0.13 g/t Pt from 100m |
| 06RZDD005 | A1 | 492415 | 7687187 | 159.20 | 180 | -75 | 5.5m @ 0.59% Ni, 0.93% Cu, 0.43 g/t Pd, 0.12 g/t Pt from 143.5m |
| 07RZDD006 | A1 | 492524 | 7687330 | 260.35 | 180 | -70 | 14m @ 0.28% Ni, 0.34% Cu from 210m |
| 70SD1 | A1 | 492682 | 7687136 | 122 | 180 | -60 | 3.05m @ 0.35% Ni, 0.51% Cu from 67.07m |
| 71SD17 | A1 | 492311 | 7687087 | 96.30 | 180 | -50 | 6.1m @ 0.57% Ni from 80.8m |
| 71SD18 | A1 | 492301 | 7687173 | 123.80 | 0 | -90 | NSI |
| 71SD8 | B1 | 489714 | 7687714 | 65.24 | 0 | -90 | 8.3m @ 0.24% Ni, 0.27% Cu from 50.3m |
| 71SP14 | A1 | 492635 | 7687086 | 44 | 0 | -90 | 1.8m @ 0.32% Ni, 0.2% Cu from 18.3m |
| 71SP14 | 3.7m @ 0.31% Ni, 0.20% Cu from 40.2m | ||||||
| 71SP15 | A1 | 492635 | 7687073 | 29 | 0 | -90 | 1.8m @ 0.22% Ni, 0.28% Cu from 25.6m |
| 72RWP13 | A1 | 491759 | 7687410 | 33 | 0 | -90 | NSI |
| 72RWP14 | A1 | 491781 | 7687455 | 26 | 0 | -90 | NSI |
| 72RWP15 | A1 | 491802 | 7687500 | 33 | 0 | -90 | NSI |
| 72SD10 | A1 | 492309 | 7687120 | 119.20 | 180 | -50 | NSI |
| 72SD17 | B1 | 489897 | 7687956 | 145.70 | 0 | -90 | 47.8m @ 0.33% Ni, 0.30% Cu from 88.4m |
| 72SD18 | B1 | 489913 | 7687979 | 154 | 0 | -90 | 16.8m @ 0.34% Ni, 0.31% Cu from 121.6m |
| 72SD19 | B1 | 489899 | 7688012 | 164.60 | 0 | -90 | 31.5m @ 0.37% Ni, 0.34% Cu from 120m |
| 72SP20 | B1 | 489488 | 7687515 | 22 | 0 | -90 | NSI |
| 72SP21 | B1 | 489458 | 7687516 | 23 | 0 | -90 | NSI |
| 72SP22 | B1 | 489427 | 7687517 | 18 | 0 | -90 | NSI |
| 72SP23 | B1 | 489366 | 7687518 | 22 | 0 | -90 | NSI |
| 72SP24 | B1 | 489304 | 7687520 | 22 | 0 | -90 | NSI |
| 72SP25 | B1 | 489274 | 7687520 | 22 | 0 | -90 | NSI |
| 72SP26 | B1 | 489243 | 7687521 | 26 | 0 | -90 | NSI |
| 72SP27 | B1 | 489212 | 7687522 | 26 | 0 | -90 | NSI |
| 72SP28 | B1 | 489182 | 7687523 | 22 | 0 | -90 | NSI |
| 72SP29 | B1 | 489834 | 7687814 | 15 | 0 | -90 | NSI |
| 72SP30 | B1 | 489834 | 7687829 | 15 | 0 | -90 | NSI |
| 72SP31 | B1 | 489834 | 7687844 | 15 | 0 | -90 | NSI |
| 72SP32 | B1 | 489772 | 7687800 | 37 | 0 | -90 | NSI |
| 72SP33 | B1 | 489772 | 7687815 | 29 | 0 | -90 | NSI |
| 72SP34 | B1 | 489773 | 7687831 | 18 | 0 | -90 | NSI |
| 72SP35 | B1 | 489773 | 7687846 | 22 | 0 | -90 | NSI |
| 72SP36 | B1 | 489765 | 7687508 | 37 | 0 | -90 | NSI |
| 72SP37 | B1 | 489703 | 7687510 | 26 | 0 | -90 | 14.63m @ 0.25% Ni, 0.25% Cu from 1.83m |
| 72SP38 | B1 | 489646 | 7687695 | 18 | 0 | -90 | 5.49m @ 0.28% Ni, 0.23% Cu from surface |
| 72SP39 | B1 | 489593 | 7687697 | 26 | 0 | -90 | 1.83m @ 0.55% Ni, 0.07% Cu from 9.14m |
| 72SP40 | B1 | 489577 | 7687697 | 15 | 0 | -90 | 3.65m @ 0.24% Ni, 0.45% Cu from 5.49m |

| Hole | Area | E_GDA94 | N_GDA94 | Depth (m) | Azimuth | Dip | Intercept* |
|---|---|---|---|---|---|---|---|
| 72SP41 | B1 | 489562 | 7687697 | 11 | 0 | -90 | NSI |
| 73SD1 | B1 | 490008 | 7688060 | 227.40 | 0 | -90 | 15.2m @ 0.22% Ni, 0.25% Cu from 208.8m |
| 73SD4 | A1 | 492467 | 7687124 | 111.60 | 180 | -75 | 12.2m @ 0.41% Ni, 0.39% Cu from 80.8m |
| 73SD5 | B1 | 489974 | 7688129 | 244.80 | 0 | -90 | 21.3m @ 0.35% Ni, 0.41% Cu from 215.2m |
| 85SP332 | B1 | 489769 | 7687925 | 114 | 0 | -90 | 20m @ 0.41% Ni, 0.78% Cu from 86m |
| 85SP333 | A1 | 492369 | 7687139 | 150 | 0 | -90 | 20m @ 0.44% Ni, 0.61% Cu from 116m |
| 85SP334 | A1 | 492435 | 7687214 | 188 | 0 | -90 | 20m @ 0.40% Ni, 0.59% Cu from 166m |
| 85SPD335 | B1 | 489813 | 7688010 | 159.40 | 0 | -90 | 2.5m @ 0.50% Ni, 1.24% Cu from 149m |
| 86SP345 | B1 | 489680 | 7687836 | 54 | 0 | -90 | no assays available |
| 86SPD336 | A1 | 492337 | 7687092 | 112.30 | 0 | -90 | 12m @ 0.38% Ni, 0.69% Cu from 86m |
| 86SPD337 | A1 | 492426 | 7687140 | 130.80 | 0 | -90 | 15.8m @ 0.73% Ni, 0.97% Cu from 115m |
| 86SPD338 | A1 | 492518 | 7687203 | 174.25 | 0 | -90 | 5m @ 0.26% Ni, 0.35% Cu from 164.65m |
| 86SPD339 | A1 | 492558 | 7687266 | 220.65 | 0 | -90 | NSI |
| 86SPD340 | A1 | 492612 | 7687251 | 210.25 | 0 | -90 | 1m @ 0.19% Ni, 0.44% Cu from 188.1m |
| 86SPD343 | B1 | 489761 | 7687877 | 91 | 0 | -90 | 13m @ 1.18% Ni, 1.02% Cu from 72.2m |
| 86SPD344 | B1 | 489856 | 7687930 | 138.05 | 0 | -90 | 13.1m @ 0.41% Ni, 0.47% Cu from 120m |
| 89XDRC1 | B1 | 489233 | 7687307 | 60 | 50 | -60 | no assays available |
| 89XDRC2A | B1 | 489278 | 7687320 | 72 | 235 | -60 | no assays available |
| 89XDRC3 | B1 | 489289 | 7687284 | 78 | 235 | -60 | no assays available |
| A1RC1 | A1 | 492589 | 7687156 | 130 | 180 | -60 | 1m @ 0.32% Ni, 0.25% Cu, 0.62 g/t Pd, 0.07 g/t Pt from 87m |
| A1RC1 | 1m @ 0.35% Ni, 0.24% Cu, 0.19 g/t Pd, 0.03 g/t Pt from 113m | ||||||
| A1RC10 | A1 | 492339 | 7687196 | 180 | 180 | -60 | 5m @ 0.28% Ni, 0.72% Cu, 0.21 g/t Pd, 0.04 g/t Pt from 135m |
| A1RC11 | A1 | 492389 | 7687206 | 180 | 180 | -60 | 17m @ 0.91% Ni, 1.11% Cu, 0.62 g/t Pd, 0.16 g/t Pt from 137m |
| A1RC12 | A1 | 492389 | 7687156 | 150 | 180 | -60 | 15m @ 0.24% Ni, 0.32% Cu, 0.27 g/t Pd, 0.06 g/t Pt from 109m |
| A1RC13 | A1 | 492439 | 7687281 | 216 | 180 | -70 | 6m @ 0.23% Ni, 0.60% Cu, 0.22 g/t Pd, 0.05 g/t Pt from 197m |
| A1RC14 | A1 | 492439 | 7687176 | 150 | 180 | -70 | 19m @ 0.32% Ni, 0.46% Cu, 0.37 g/t Pd, 0.07 g/t Pt from 118m |
| A1RC2 | A1 | 492589 | 7687226 | 150 | 180 | -70 | 1m @ 0.28% Ni, 0.29% Cu, 0.56 g/t Pd, 0.06 g/t Pt from 145m |
| A1RC3 | A1 | 492539 | 7687106 | 87 | 180 | -60 | 3m @ 0.28% Ni, 0.20% Cu, 0.31 g/t Pd, 0.04 g/t Pt from 61m |
| A1RC3 | 1m @ 0.28% Ni, 0.34% Cu, 0.53 g/t Pd, 0.03 g/t Pt from 80m | ||||||
| A1RC4 | A1 | 492489 | 7687156 | 132 | 180 | -70 | 17m @ 0.26% Ni, 0.38% Cu, 0.37 g/t Pd, 0.04 g/t Pt from 90m |
| A1RC5 | A1 | 492439 | 7687106 | 110 | 180 | -70 | 15m @ 0.35% Ni, 0.29% Cu, 0.31 g/t Pd, 0.06 g/t Pt from 70m |
| A1RC6 | A1 | 492439 | 7687231 | 180 | 180 | -70 | 18m @ 0.41% Ni, 0.82% Cu, 0.94 g/t Pd, 0.12 g/t Pt from 150m |
| A1RC7 | A1 | 492389 | 7687106 | 110 | 180 | -60 | NSI |
| A1RC8 | A1 | 492439 | 7687081 | 78 | 180 | -60 | 12m @ 0.28% Ni, 0.43% Cu, 0.29 g/t Pd, 0.04 g/t Pt from 61m |
| A1RC9 | A1 | 492339 | 7687085 | 120 | 180 | -60 | 18m @ 0.40% Ni, 0.52% Cu, 0.47 g/t Pd, 0.13 g/t Pt from 62m |
| B1MET1 | B1 | 489611 | 7687784 | 45.5 | 0 | -90 | 24m @ 0.69% Ni, 1.07% Cu, 0.64 g/t Pd, 0.12 g/t Pt from 15m |
| B1RC101 | B1 | 489724 | 7687830 | 78 | 0 | -90 | 24m @ 0.35% Ni, 0.47% Cu, 0.46 g/t Pd, 0.08 g/t Pt from 52m |
| B1RC102 | B1 | 489707 | 7687842 | 88 | 0 | -90 | 27m @ 0.50% Ni, 0.82% Cu, 0.86 g/t Pd, 0.13 g/t Pt from 54m |
| B1RC103 | B1 | 489657 | 7687753 | 67 | 0 | -90 | 1m @ 0.23% Ni, 0.39% Cu, 0.16 g/t Pd, 0.05 g/t Pt from 41m |
| B1RC104 | B1 | 489641 | 7687764 | 87 | 0 | -90 | NSI |
| B1RC105 | B1 | 489623 | 7687652 | 17 | 0 | -90 | NSI |
| B1RC106 | B1 | 489664 | 7687622 | 22 | 0 | -90 | NSI |
| B1RC107 | B1 | 489747 | 7687563 | 29 | 0 | -90 | 3m @ 0.30% Ni, 0.34% Cu, 0.51 g/t Pd, 0.06 g/t Pt from 12m |
| B1RC108 | B1 | 489788 | 7687534 | 19 | 0 | -90 | NSI |

| Hole | Area | E_GDA94 | N_GDA94 | Depth (m) | Azimuth | Dip | Intercept* |
|---|---|---|---|---|---|---|---|
| B1RC109 | B1 | 489688 | 7687481 | 16 | 0 | -90 | NSI |
| B1RC110 | B1 | 489727 | 7687450 | 9 | 0 | -90 | 5m @ 0.29% Ni, 0.44% Cu from surface |
| B1RC111 | B1 | 489744 | 7687385 | 12 | 0 | -90 | NSI |
| B1RC112 | B1 | 489690 | 7687729 | 54 | 0 | -90 | 36m @ 0.30% Ni, 0.28% Cu, 0.31 g/t Pd, 0.04 g/t Pt from 15m |
| B1RC113 | B1 | 489674 | 7687740 | 55 | 0 | -90 | 32m @ 0.26% Ni, 0.24% Cu, 0.28 g/t Pd, 0.05 g/t Pt from 19m |
| B1RC114 | B1 | 489729 | 7687889 | 96 | 0 | -90 | 13m @ 0.13% Ni, 0.31% Cu from 83m |
| B1RC115 | B1 | 489611 | 7687785 | 45 | 0 | -90 | 27m @ 0.55% Ni, 0.80% Cu, 0.80 g/t Pd, 0.15 g/t Pt from 12m |
| B1RC116 | B1 | 489703 | 7687782 | 69 | 0 | -90 | 8m @ 0.28% Ni, 0.29% Cu, 0.35 g/t Pd, 0.05 g/t Pt from 44m |
| B1RC117 | B1 | 489770 | 7687859 | 87 | 0 | -90 | 20m @ 0.32% Ni, 0.27% Cu, 0.34 g/t Pd, 0.05 g/t Pt from 59m |
| B1RC118 | B1 | 489800 | 7687901 | 117 | 0 | -90 | 41m @ 0.37% Ni, 0.28% Cu, 0.41 g/t Pd, 0.07 g/t Pt from 63m |
| B1RC118 | incl. 1m @ 5.7% Ni, 0.73% Cu, 2.3 g/t Pd, 0.14 g/t Pt from 78m | ||||||
| B1RC119 | B1 | 489720 | 7687771 | 80 | 0 | -90 | 42m @ 0.26% Ni, 0.33% Cu, 0.29 g/t Pd, 0.04 g/t Pt from 22m |
| B1RC121 | B1 | 489582 | 7687764 | 50 | 0 | -90 | 24m @ 0.62% Ni, 0.95% Cu, 0.77 g/t Pd, 0.14 g/t Pt from 3m |
| B1RC122 | B1 | 489607 | 7687794 | 60 | 0 | -90 | 21m @ 0.50% Ni, 0.90% Cu, 0.63 g/t Pd, 0.12 g/t Pt from 20m |
| B1RC123 | B1 | 489630 | 7687835 | 80 | 0 | -90 | 4m @ 0.59% Ni, 0.68% Cu, 0.55 g/t Pd, 0.10 g/t Pt from 54m |
| B1RC123 | 4m @ 0.24% Ni, 0.55% Cu, 0.35 g/t Pd, 0.06 g/t Pt from 68m | ||||||
| B1RC124 | B1 | 489653 | 7687810 | 80 | 0 | -90 | 14m @ 0.28% Ni, 0.40% Cu, 0.35 g/t Pd, 0.06 g/t Pt from 54m |
| B1RC125 | B1 | 489657 | 7687875 | 100 | 0 | -90 | 15m @ 0.42% Ni, 0.81% Cu, 0.52 g/t Pd, 0.10 g/t Pt from 73m |
| B1RC126 | B1 | 489679 | 7687862 | 100 | 0 | -90 | 8m @ 0.28% Ni, 0.45% Cu, 0.27 g/t Pd, 0.05 g/t Pt from 76m |
| B1RC127 | B1 | 489740 | 7687820 | 100 | 0 | -90 | 42m @ 0.34% Ni, 0.29% Cu, 0.21 g/t Pd, 0.04 g/t Pt from 28m |
| B1RC128 | B1 | 489764 | 7687802 | 100 | 0 | -90 | 21m @ 0.22% Ni, 0.27% Cu, 0.22 g/t Pd, 0.03 g/t Pt from 38m |
| B1RC129 | B1 | 489681 | 7687931 | 130 | 0 | -90 | NSI |
| B1RC130 | B1 | 489788 | 7687843 | 110 | 0 | -90 | 44m @ 0.23% Ni, 0.30% Cu, 0.23 g/t Pd, 0.03 g/t Pt from 36m |
| B1RC131 | B1 | 489741 | 7687938 | 130 | 0 | -90 | NSI |
| B1RC132 | B1 | 489816 | 7687884 | 130 | 0 | -90 | 37m @ 0.27% Ni, 0.29% Cu, 0.27 g/t Pd, 0.05 g/t Pt from 57m |
| B1RC133 | B1 | 489777 | 7687976 | 150 | 0 | -90 | 7m @ 0.30% Ni, 0.73% Cu, 0.42 g/t Pd, 0.05% g/t Pt from 130m |
| B1RC134 | B1 | 489872 | 7687965 | 150 | 0 | -90 | 38m @ 0.21% Ni, 0.21% Cu, 0.22 g/t Pd, 0.05 g/t Pt from 104m |
| B1RC135 | B1 | 489797 | 7687773 | 100 | 0 | -90 | 25m @ 0.23% Ni, 0.28% Cu, 0.22 g/t Pd, 0.04 g/t Pt from 41m |
| B1RC136 | B1 | 489614 | 7687795 | 50 | 0 | -90 | 26m @ 0.44% Ni, 0.92% Cu, 0.68 g/t Pd, 0.14 g/t Pt from 16m |
| B1RC137 | B1 | 489622 | 7687790 | 50 | 0 | -90 | 20m @ 0.48% Ni, 0.77% Cu, 0.54 g/t Pd, 0.11 g/t Pt from 21m |
| B1RC138 | B1 | 489630 | 7687785 | 50 | 0 | -90 | 22m @ 0.27% Ni, 0.48% Cu, 0.30 g/t Pd, 0.07 g/t Pt from 20m |
| B1RC139 | B1 | 489625 | 7687777 | 50 | 0 | -90 | 24m @ 0.30% Ni, 0.53% Ni, 0.33 g/t Pd, 0.07 g/t Pt from 16m |
| B1RC140 | B1 | 489603 | 7687779 | 45 | 0 | -90 | 23m @ 0.53% Ni, 0.83% Cu, 0.69 g/t Pd, 0.14 g/t Pt from 8m |
| B1RC141 | B1 | 489611 | 7687774 | 45 | 0 | -90 | 34m @ 0.35% Ni, 0.54% Cu, 0.35 g/t Pd, 0.07 g/t Pt from surface |
| B1RC142 | B1 | 489619 | 7687769 | 45 | 0 | -90 | 27m @ 0.18% Ni, 0.27% Cu, 0.21 g/t Pd, 0.04 g/t Pt from 4m |
| B1RC143 | B1 | 489590 | 7687776 | 40 | 0 | -90 | 18m @ 0.41% Ni, 0.89% Cu, 0.55 g/t Pd, 0.11 g/t Pt from 12m |
| B1RC144 | B1 | 489598 | 7687771 | 40 | 0 | -90 | 24m @ 0.57% Ni, 0.86% Cu, 0.70 g/t Pd, 0.14 g/t Pt from 4m |
| B1RC145 | B1 | 489606 | 7687766 | 40 | 0 | -90 | 23m @ 0.33% Ni, 0.51% Cu, 0.46 g/t Pd, 0.24 g/t Pt from 4m |
| B1RC146 | B1 | 489593 | 7687763 | 40 | 0 | -90 | 23m @ 0.43% Ni, 0.65% Cu, 0.51 g/t Pd, 0.10 g/t Pt from 4m |
| B1RC147 | B1 | 489601 | 7687758 | 40 | 0 | -90 | 21m @ 0.37% Ni, 0.34% Cu, 0.33 g/t Pd, 0.07 g/t Pt from 4m |
| B1RC148 | B1 | 489572 | 7687766 | 30 | 0 | -90 | 10m @ 0.29% Ni, 0.61% Cu, 0.64 g/t Pd, 0.10 g/t Pt from 9m |
| B1RC149 | B1 | 489580 | 7687760 | 30 | 0 | -90 | 20m @ 0.88% Ni, 1.05% Cu, 0.78 g/t Pd, 0.16 g/t Pt from 3m |
| B1RC150 | B1 | 489588 | 7687755 | 30 | 0 | -90 | 23m @ 0.31% Ni, 0.50% Cu, 0.37 g/t Pd, 0.12 g/t Pt from 2m |
| B1RC151 | B1 | 489567 | 7687758 | 30 | 0 | -90 | 12m @ 0.43% Ni, 0.77% Cu, 0.43 g/t Pd, 0.12 g/t Pt from surface |

| Hole | Area | E_GDA94 | N_GDA94 | Depth (m) | Azimuth | Dip | Intercept* |
|---|---|---|---|---|---|---|---|
| B1RC152 | B1 | 489575 | 7687752 | 30 | 0 | -90 | 14m @ 0.55% Ni, 0.69% Cu, 0.61 g/t Pd, 0.15 g/t Pt from surface |
| B1RC153 | B1 | 489583 | 7687747 | 30 | 0 | -90 | 22m @ 0.25% Ni, 0.40% Cu, 0.34 g/t Pd, 0.08 g/t Pt from surface |
| B1RC154 | B1 | 489591 | 7687742 | 30 | 0 | -90 | 9m @ 0.27% Ni, 0.37% Cu, 0.24 g/t Pd, 0.06 g/t Pt from 2m |
| B1RC155 | B1 | 489599 | 7687737 | 30 | 0 | -90 | 10m @ 0.20% Ni, 0.28% Cu, 0.21 g/t Pd, 3.8 g/t Pt from 5m |
| B1RC156 | B1 | 489609 | 7687753 | 40 | 0 | -90 | 19m @ 0.26% Ni, 0.40% Cu, 0.29 g/t Pd, 0.05 g/t Pt from 4m |
| B1RC157 | B1 | 489566 | 7687792 | 40 | 0 | -90 | NSI |
| B1RC158 | B1 | 489582 | 7687781 | 40 | 0 | -90 | 16m @ 0.54% Ni, 1.08% Cu, 0.69 g/t Pd, 0.09 g/t Pt from 16m |
| B1RC159 | B1 | 489593 | 7687797 | 50 | 0 | -90 | 16m @ 0.22% Ni, 0.82% Cu, 0.44 g/t Pd, 0.10 g/t Pt from 23m |
| B1RC160 | B1 | 489598 | 7687805 | 52 | 0 | -90 | 21m @ 0.21% Ni, 0.79% Cu, 0.37 g/t Pd, 0.08 g/t Pt from 24m |
| B1RC161 | B1 | 489639 | 7687815 | 80 | 180 | -60 | 14m @ 0.42% Ni, 0.85% Cu, 0.78 g/t Pd, 0.13 g/t Pt from 49m |
| B1RC162 | B1 | 489672 | 7687792 | 80 | 180 | -60 | 16m @ 0.31% Ni, 0.48% Cu, 0.41 g/t Pd, 0.15 g/t Pt from 50m |
| B1RC163 | B1 | 489783 | 7687913 | 140 | 180 | -60 | 26m @ 0.46% Ni, 0.63% Cu, 0.51 g/t Pd, 0.09 g/t Pt from 88m |
| B1RC164 | B1 | 489871 | 7687913 | 150 | 180 | -60 | 53m @ 0.29% Ni, 0.36% Cu, 0.27 g/t Pd, 0.05 g/t Pt from 76m |
| B1RC165 | B1 | 489796 | 7687966 | 140 | 180 | -60 | 7m @ 0.18% Ni, 0.43% Cu, 0.34 g/t Pd, 0.07 g/t Pt from 124m |
| B1RC166 | B1 | 489659 | 7688105 | 150 | 180 | -60 | no assays available |
| B1RCD120 | B1 | 489818 | 7687926 | 129 | 0 | -90 | 32m @ 0.31% Ni, 0.37% Cu, 0.50 g/t Pd, 0.09 g/t Pt from 82m |
| RBRC001 | B1 | 490339 | 7687556 | 170 | 0 | -90 | NSI |
| RBRC002 | B1 | 490289 | 7687556 | 170 | 0 | -90 | NSI |
| RBRC003 | B1 | 490239 | 7687556 | 170 | 0 | -90 | NSI |
| RBRC004 | B1 | 490539 | 7687456 | 170 | 0 | -90 | NSI |
| RBRC005 | B1 | 490489 | 7687456 | 170 | 0 | -90 | NSI |
| RBRC006 | B1 | 490439 | 7687456 | 170 | 0 | -90 | NSI |
| RBRC007 | B1 | 490539 | 7687356 | 170 | 0 | -90 | NSI |
| RBRC008 | B1 | 490489 | 7687356 | 170 | 0 | -90 | NSI |
| RBRC009 | B1 | 490439 | 7687356 | 170 | 0 | -90 | NSI |
| RBRC010 | B1 | 490389 | 7687356 | 170 | 0 | -90 | NSI |
| RBRC011 | B1 | 490489 | 7687256 | 170 | 0 | -90 | no assays available |
| RBRC012 | B1 | 490439 | 7687256 | 170 | 0 | -90 | no assays available |
| RBRC013 | B1 | 490389 | 7687256 | 170 | 0 | -90 | no assays available |
| SRRC10 | B1 | 490139 | 7688106 | 150 | 180 | -60 | NSI |
| SRRC11 | B1 | 490139 | 7688156 | 162 | 180 | -60 | NSI |
| SRRC12 | B1 | 490339 | 7687806 | 174 | 180 | -60 | NSI |
| SRRC13 | B1 | 490339 | 7687856 | 172 | 180 | -60 | NSI |
| SRRC14 | B1 | 490339 | 7687906 | 180 | 180 | -60 | NSI |
| SRRC15 | B1 | 490339 | 7687956 | 150 | 180 | -60 | NSI |
| SRRC16 | B1 | 490339 | 7688006 | 150 | 180 | -60 | NSI |
| SRRC17 | B1 | 490339 | 7688056 | 150 | 180 | -60 | NSI |
| SRRC18 | B1 | 490539 | 7687796 | 150 | 180 | -60 | NSI |
| SRRC19 | B1 | 490539 | 7687846 | 150 | 180 | -60 | NSI |
| SRRC20 | B1 | 490539 | 7687896 | 150 | 180 | -60 | NSI |
| SRRC21 | B1 | 490539 | 7687956 | 150 | 180 | -60 | NSI |
| SRRC22 | B1 | 490739 | 7687756 | 150 | 180 | -60 | NSI |
| SRRC23 | B1 | 490739 | 7687806 | 160 | 180 | -60 | NSI |
| SRRC24 | B1 | 490739 | 7687656 | 150 | 180 | -60 | NSI |

| Hole | Area | E_GDA94 | N_GDA94 | Depth (m) | Azimuth | Dip | Intercept* |
|---|---|---|---|---|---|---|---|
| SRRC25 | B1 | 490739 | 7687856 | 150 | 180 | -60 | NSI |
| SRRC26 | B1 | 490739 | 7687906 | 150 | 180 | -60 | NSI |
| SRRC27 | B1 | 490939 | 7687506 | 150 | 180 | -60 | NSI |
| SRRC28 | B1 | 490939 | 7687556 | 150 | 180 | -60 | NSI |
| SRRC29 | B1 | 490939 | 7687606 | 150 | 180 | -60 | NSI |
| SRRC30 | B1 | 491139 | 7687456 | 150 | 180 | -60 | NSI |
| SRRC31 | B1 | 491139 | 7687506 | 180 | 180 | -60 | NSI |
| SRRC32 | B1 | 491139 | 7687406 | 126 | 180 | -60 | NSI |
| SRRC33 | B1 | 491289 | 7687256 | 172 | 180 | -60 | NSI |
| SRRC34 | B1 | 491289 | 7687306 | 168 | 180 | -60 | NSI |
| SRRC35 | B1 | 491289 | 7687356 | 168 | 180 | -60 | NSI |
| SRRC36 | B1 | 491289 | 7687406 | 150 | 180 | -60 | NSI |
| SRRC37 | B1 | 491289 | 7687456 | 172 | 180 | -60 | NSI |
| SRRC38 | B1 | 491289 | 7687506 | 160 | 180 | -60 | NSI |
| SRRC39 | B1 | 491289 | 7687556 | 160 | 180 | -60 | NSI |
| SRRC47 | B1 | 490149 | 7687931 | 180 | 0 | -90 | NSI |
| SRRC48 | B1 | 490139 | 7687856 | 200 | 180 | -60 | 4m @ 0.18% Ni, 0.42% Cu, 0.37 g/t Pd, 0.38 g/t Pt from 100m |
| SRRC48 | 4m @ 0.22% Ni, 0.61% Cu, 0.69 g/t Pd, 0.06 g/t Pt from 132m | ||||||
| SRRC48 | 4m @ 0.33% Ni, 0.40% Cu, 0.32 g/t Pd, 0.46 g/t Pt from 180m | ||||||
| SRRC6 | B1 | 490139 | 7687906 | 150 | 180 | -60 | 19m @ 0.23% Ni, 0.19% Cu, 0.18 g/t Pd, 0.03 g/t Pt from 123m |
| SRRC7 | B1 | 490139 | 7687956 | 150 | 180 | -60 | 2m @ 0.25% Ni, 0.36% Cu, 0.21 g/t Pd, 0.03 g/t Pt from 148m to EOH |
| SRRC8 | B1 | 490139 | 7688006 | 150 | 180 | -60 | NSI |
| SRRC9 | B1 | 490139 | 7688056 | 150 | 180 | -60 | NSI |
| SRRCD62 | B1 | 490940 | 7687360 | 295.10 | 0 | -90 | no assays available |
* quoted as downhole lengths; holes were oriented roughly perpendicular to the lode but the true width is not known
* intercepts are calculated as weighted averages > 0.5% Cu+Ni with no internal intervals < 0.1% Cu+Ni
Table 2: Mt Sholl Radleys historic drillholes
| Hole | Year | E_GDA94 | N_GDA94 | Depth (m) | Azimuth | Dip | Intercept* |
|---|---|---|---|---|---|---|---|
| 86RP3 | 1986 | 488964 | 7688689 | 36 | 200 | -60 | NSI |
| 86RP4 | 1986 | 488970 | 7688705 | 36 | 200 | -60 | NSI |
| 86RP5 | 1986 | 488976 | 7688720 | 36 | 200 | -60 | NSI |
| 86RP6 | 1986 | 488982 | 7688736 | 36 | 200 | -60 | NSI |
| 86RP7 | 1986 | 488989 | 7688752 | 36 | 200 | -60 | NSI |
| 86RP8 | 1986 | 489077 | 7688701 | 42 | 200 | -60 | NSI |
| 86RP9 | 1986 | 489163 | 7688645 | 12.5 | 200 | -60 | NSI |
| 86RP10 | 1986 | 489167 | 7688657 | 48 | 200 | -60 | NSI |
| 86RP11 | 1986 | 489246 | 7688582 | 48 | 200 | -60 | NSI |
| 86RP12 | 1986 | 489251 | 7688595 | 48 | 200 | -60 | NSI |
| 86RP13 | 1986 | 489256 | 7688608 | 60 | 200 | -60 | 2m @ 0.25 g/t Au from 30m |
| 86RP14 | 1986 | 489453 | 7688558 | 36 | 200 | -60 | 2m @ 1.52 g/t Au from 8m |
| 86RP15 | 1986 | 489456 | 7688565 | 48 | 200 | -60 | 3m @ 2.76 g/t Au from 15m |
| 86RP16 | 1986 | 489545 | 7688519 | 48 | 200 | -60 | NSI |

| Hole | Year | E_GDA94 | N_GDA94 | Depth (m) | Azimuth | Dip | Intercept* |
|---|---|---|---|---|---|---|---|
| 86RP17 | 1986 | 489554 | 7688542 | 48 | 200 | -60 | NSI |
| 86RP18 | 1986 | 489564 | 7688566 | 48 | 200 | -60 | 2m @ 0.36 g/t Au from 19m |
| 86RP19 | 1986 | 489567 | 7688574 | 48 | 200 | -60 | NSI |
| 86RP20 | 1986 | 489154 | 7688624 | 30 | 20 | -60 | NSI |
| 87RP21 | 1987 | 489117 | 7688667 | 36 | 200 | -60 | 2m @ 3.09 g/t Au from 14m |
| 87RP22 | 1987 | 489122 | 7688679 | 32 | 200 | -60 | 2m @ 0.47g/t Au from 26m |
| 87RP23 | 1987 | 489171 | 7688666 | 66 | 200 | -60 | 2m @ 0.33 g/t Au from 41m |
| 87RP24 | 1987 | 489398 | 7688558 | 36 | 200 | -60 | 1m @ 0.5 g/t Au from 15m |
| 87RP25 | 1987 | 489404 | 7688571 | 42 | 200 | -60 | 2m @ 0.48 g/t Au from 19m |
| 87RP26 | 1987 | 489509 | 7688555 | 36 | 200 | -60 | 10m @ 2.21 g/t Au from 11m |
| 87RP26 | incl. 1m @ 15.9 g/t Au from 16m | ||||||
| 87RP27 | 1987 | 489512 | 7688565 | 48 | 200 | -60 | 5m @ 0.51 g/t Au from 21m |
| 87RP28 | 1987 | 489460 | 7688576 | 54 | 200 | -60 | 3m @ 0.77 g/t Au from 25m |
| 87RP29 | 1987 | 489463 | 7688585 | 48 | 200 | -60 | 3m @ 1.03 g/t Au from 34m |
| 87RP30 | 1987 | 489478 | 7688622 | 66 | 200 | -60 | 3m @ 4.15 g/t Au from 60m |
| 87RP30 | Incl. 1m @ 12 g/t Au from 61m | ||||||
| 87RP31 | 1987 | 489614 | 7688556 | 36 | 200 | -60 | 1m @ 0.12 g/t Au from 10m |
| 87RP32 | 1987 | 489618 | 7688565 | 42 | 200 | -60 | NSI |
| 87RP33 | 1987 | 489622 | 7688575 | 48 | 200 | -60 | NSI |
| 87RP34 | 1987 | 489663 | 7688542 | 36 | 200 | -60 | 1m @ 0.59 g/t Au from 23m |
| 87RP35 | 1987 | 489666 | 7688551 | 36 | 200 | -60 | 4m @ 0.82 g/t Au from 29m |
| 89RP52 | 1989 | 489503 | 7688548 | 30 | 200 | -60 | 1m @ 3.4 g/t Au from 2m |
| 89RP52 | 2m @ 1.05 g/t Au from 26m | ||||||
| 89RP53 | 1989 | 489526 | 7688607 | 66 | 200 | -60 | 1m @ 0.18 g/t Au from 59m |
| 89RP54 | 1989 | 489471 | 7688604 | 54 | 200 | -60 | 3m @ 4.49 g/t Au from 48m |
| 89RP54 | incl. 1m @ 13 g/t Au from 48m | ||||||
| 89RP55 | 1989 | 489413 | 7688593 | 60 | 200 | -60 | 5m @ 0.72 g/t Au from 37m |
| 90RP56 | 1990 | 489308 | 7688603 | 48 | 200 | -60 | 1m @ 0.15 g/t Au from 36m |
| 90RP57 | 1990 | 489359 | 7688593 | 80 | 200 | -60 | 1m @ 0.79 g/t Au from 50m |
| 90RP58 | 1990 | 489420 | 7688612 | 80 | 200 | -60 | 3m @ 0.93 g/t Au from 72m |
| 90RP59 | 1990 | 489480 | 7688626 | 98 | 200 | -60 | 1m @ 0.72 g/t Au from 91m |
| 90RP60 | 1990 | 489666 | 7688551 | 60 | 200 | -60 | 1m @ 0.1 g/t Au from 14m |
| 90RP61 | 1990 | 489299 | 7688580 | 54 | 200 | -60 | 1m @ 1.8 g/t Au from 24m |
| 90RP62 | 1990 | 489351 | 7688575 | 48 | 200 | -60 | 2m @ 0.62 g/t Au from 23m |
| 90RP63 | 1990 | 489512 | 7688570 | 60 | 200 | -60 | 1m @ 4 g/t Au from 39m |
* quoted as downhole lengths; holes were oriented roughly perpendicular to the lode but the true width is not known * intercepts are calculated as weighted averages > 0.1 g/t Au with no internal waste

Table 3: JORC Code, 2012 Edition. Section 1.
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Samplingtechniques | •Nature and quality of sampling (eg cutchannels, random chips, or specificspecialised industry standardmeasurement tools appropriate to theminerals under investigation, such asdown hole gamma sondes, or handheldXRF instruments, etc). These examplesshould not be taken as limiting the broadmeaning of sampling.•Include reference to measures taken toensure sample representivity and theappropriate calibration of anymeasurement tools or systems used.•Aspects of the determination ofmineralisation that are Material to thePublic Report.•In cases where 'industry standard' workhas been done this would be relativelysimple (eg 'reverse circulation drilling wasused to obtain 1 m samples from which 3kg was pulverised to produce a 30 gcharge for fire assay'). In other cases moreexplanation may be required, such aswhere there is coarse gold that hasinherent sampling problems. Unusualcommodities or mineralisation types (egsubmarine nodules) may warrantdisclosure of detailed information. | •The nature and quality of historical soilsampling at Boodalyerrie is not known tothe CP. This is one of the reasons Raidenis implementing a program of verificationsampling.•At Mt Sholl, reverse circulation anddiamond drill rigs were employed byprevious explorers to obtain samples of drillchips or core using practices that wereconsidered to be industry standard at thetime.•Sample collection and preparationprocedures for drill samples are not known. |
| Drillingtechniques | •Drill type (eg core, reverse circulation,open-hole hammer, rotary air blast, auger,Bangka, sonic, etc) and details (eg corediameter, triple or standard tube, depth ofdiamond tails, face-sampling bit or othertype, whether core is oriented and if so, bywhat method, etc). | •Reverse circulation percussion anddiamond - both HQ and NQ sized core.•It is not known if a face sampling hammerwas used. |
| Drill samplerecovery | •Method of recording and assessing coreand chip sample recoveries and resultsassessed.•Measures taken to maximise samplerecovery and ensure representative natureof the samples.•Whether a relationship exists betweensample recovery and grade and whethersample bias may have occurred due topreferential loss/gain of fine/coarsematerial. | •It is not known how or whether samplerecovery was monitored. |
| Logging | •Whether core and chip samples have beengeologically and geotechnically logged to alevel of detail to support appropriateMineral Resource estimation, miningstudies and metallurgical studies.•Whether logging is qualitative orquantitative in nature. Core (or costean, | •Core and chip samples were geologicallylogged. It is not known if core wasgeotechnically logged.•The data is not being used for MineralResource estimation. |

| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| channel, etc) photography.•The total length and percentage of therelevant intersections logged. | ||
| Sub-samplingtechniquesand samplepreparation | •If core, whether cut or sawn and whetherquarter, half or all core taken.•If non-core, whether riffled, tube sampled,rotary split, etc and whether sampled wetor dry.•For all sample types, the nature, qualityand appropriateness of the samplepreparation technique.•Quality control procedures adopted for allsub-sampling stages to maximiserepresentivity of samples.•Measures taken to ensure that thesampling is representative of the in situmaterial collected, including for instanceresults for field duplicate/second-halfsampling.•Whether sample sizes are appropriate tothe grain size of the material beingsampled. | •Methods for splitting the drill samples andrelevant quality control procedures areunknown to the CP. It is not known ifduplicate splits were collected or analysed.•Commercial laboratories followed standardprocedures for sample preparation toproduce sub-samples for analysis. |
| Quality ofassay dataandlaboratorytests | •The nature, quality and appropriateness ofthe assaying and laboratory proceduresused and whether the technique isconsidered partial or total.•For geophysical tools, spectrometers,handheld XRF instruments, etc, theparameters used in determining theanalysis including instrument make andmodel, reading times, calibrations factorsapplied and their derivation, etc.•Nature of quality control proceduresadopted (eg standards, blanks, duplicates,external laboratory checks) and whetheracceptable levels of accuracy (ie lack ofbias) and precision have been established. | •Laboratory procedures and assaying areconsidered appropriate by the CP for thetype of sample.•Laboratory quality control procedures arenot available for the samples. |
| Verification ofsampling andassaying | •The verification of significant intersectionsby either independent or alternativecompany personnel.•The use of twinned holes.•Documentation of primary data, data entryprocedures, data verification, data storage(physical and electronic) protocols.•Discuss any adjustment to assay data. | •Significant intercepts have not beenverified by Raiden or independentpersonnel, as the core is not available.•No drillholes have been twinned.•Because the data are historical, themethods of data documentation,verification and storage are unknown.•As far as the CP is aware, no adjustmentshave been made to assay data. |
| Location ofdata points | •Accuracy and quality of surveys used tolocate drill holes (collar and down-holesurveys), trenches, mine workings andother locations used in Mineral Resourceestimation.•Specification of the grid system used.•Quality and adequacy of topographiccontrol. | •Drillhole locations were either digitised fromhistoric maps or imported direct from digitaldata obtained using the DMIRS' WAMEXsystem. No field verifications of drill collarshave been conducted to date.•Downhole surveys were not recorded forRC holes and generally not recorded forvertical diamond drillholes. |

| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| •Co-ordinates are provided in theGeocentric Datum of Australia (GDA94). | ||
| Data spacinganddistribution | •Data spacing for reporting of ExplorationResults.•Whether the data spacing and distributionis sufficient to establish the degree ofgeological and grade continuityappropriate for the Mineral Resource andOre Reserve estimation procedure(s) andclassifications applied.•Whether sample compositing has beenapplied. | •Drillhole spacing is variable. Drill sampleswere collected at varying intervals up to 4m .•Current reporting is for progressiveexploration results and not for MineralResource or Ore Reserve estimation.•Sample compositing has not been applied. |
| Orientation ofdata inrelation togeologicalstructure | •Whether the orientation of samplingachieves unbiased sampling of possiblestructures and the extent to which this isknown, considering the deposit type.•If the relationship between the drillingorientation and the orientation of keymineralised structures is considered tohave introduced a sampling bias, thisshould be assessed and reported ifmaterial. | •Drillholes were oriented to result inapproximately perpendicular penetration ofthe projected lodes.•No known sampling bias was introducedbecause of the drill orientation. |
| Samplesecurity | •The measures taken to ensure samplesecurity. | •Sample security measures are not known. |
| Audits orreviews | •The results of any audits or reviews ofsampling techniques and data. | •No reviews or audits have beenundertaken. |
Table 4: JORC Code, 2012 Edition. Section 2.
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Mineraltenement andland tenurestatus | •Type, reference name/number, locationand ownership including agreements ormaterial issues with third parties such asjoint ventures, partnerships, overridingroyalties, native title interests, historicalsites, wilderness or national park andenvironmental settings.•The security of the tenure held at the timeof reporting along with any knownimpediments to obtaining a licence tooperate in the area. | •Mt Sholl exploration licences E47/3468 andE47/4309 are located in the City of Karrathaand Boodalyerrie licence E45/3586 islocated in the Shire of East Pilbara, allwithin the Pilbara region of WesternAustralia.•E47/3468 and E47/4309 are owned byPeter Romeo Gianni and Mining EquitiesPty Ltd, respectively; E45/3586 is owned byPacton Pilbara Pty Ltd. Raiden Resourceshas acquired 100% interest in all threetenements and is in the process oftransferring these licences to Pilbara GoldCorporation Pty Ltd (a wholly ownedsubsidiary of Raiden Resources Ltd).•E47/3468 and E47/4309 are on the MtWelcome pastoral lease.•E45/3586 is on unallocated Crown Land. |
| Exploration | •Acknowledgment and appraisal of | •A full search and compilation of historic |

| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| done by otherparties | exploration by other parties. | exploration has been completed.•Work on E47/3468 and E47/4309 includedstream sediment, soil and rock sampling,geological mapping, geophysical surveysand drilling. Work on E45/3586 consisted ofstream sediment, soil and rock sampling. |
| Geology | •Deposit type, geological setting and styleof mineralisation. | •Magmatic Ni-Cu-PGE and orogenic goldmineralisation at Mt Sholl.•Paleoarchean greenstone rocks intruded byMesoarchean mafic-ultramafic intrusivecomplex associated with widespreaddisseminated to matrix and stringerpyrrhotite-pentlandite-chalcopyritemineralisation. Mesoarchean mylonite inthe Sholl Shear Zone north of the property,with lode gold mineralisation in adjacentsubsidiary structures.•Orogenic gold mineralisation atBoodalyerrie.•Paleoarchean granitoid complex;hydrothermally altered adjacent togreenstone contact and cut by a suite ofprominent planar quartz veins. |
| Drill holeInformation | •A summary of all information material tothe understanding of the explorationresults including a tabulation of thefollowing information for all Material drillholes:oeasting and northing of the drill holecollaroelevation or RL (Reduced Level –elevation above sea level in metres) ofthe drill hole collarodip and azimuth of the holeodown hole length and interceptiondepthohole length.•If the exclusion of this information isjustified on the basis that the information isnot Material and this exclusion does notdetract from the understanding of thereport, the Competent Person shouldclearly explain why this is the case. | •Drillhole data are tabulated in the body ofthe announcement.•RL is not provided as it is not consideredmaterial. |
| Dataaggregationmethods | •In reporting Exploration Results, weightingaveraging techniques, maximum and/orminimum grade truncations (eg cutting ofhigh grades) and cut-off grades are usuallyMaterial and should be stated.•Where aggregate intercepts incorporateshort lengths of high grade results andlonger lengths of low grade results, theprocedure used for such aggregationshould be stated and some typicalexamples of such aggregations should be | •High grades have not been cut.•Cut off grades and treatment of internalwaste for drill intercepts are listed in thebody of the report.•Metal equivalent values are not reported. |

| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| shown in detail.•The assumptions used for any reporting ofmetal equivalent values should be clearlystated. | ||
| Relationshipbetweenmineralisationwidths andinterceptlengths | •These relationships are particularlyimportant in the reporting of ExplorationResults.•If the geometry of the mineralisation withrespect to the drill hole angle is known, itsnature should be reported.•If it is not known and only the down holelengths are reported, there should be aclear statement to this effect (eg 'downhole length, true width not known'). | •Intercepts are quoted as downhole lengths;holes were oriented roughly perpendicularto mineralisation but the true width is notknown. |
| Diagrams | •Appropriate maps and sections (withscales) and tabulations of interceptsshould be included for any significantdiscovery being reported These shouldinclude, but not be limited to a plan view ofdrill hole collar locations and appropriatesectional views. | •Maps and cross sections are included in thebody of the announcement. |
| Balancedreporting | •Where comprehensive reporting of allExploration Results is not practicable,representative reporting of both low andhigh grades and/or widths should bepracticed to avoid misleading reporting ofExploration Results. | •All results are reported. |
| Othersubstantiveexplorationdata | •Other exploration data, if meaningful andmaterial, should be reported including (butnot limited to): geological observations;geophysical survey results; geochemicalsurvey results; bulk samples – size andmethod of treatment; metallurgical testresults; bulk density, groundwater,geotechnical and rock characteristics;potential deleterious or contaminatingsubstances. | •All relevant data are reported in thisrelease. |
| Further work | •The nature and scale of planned furtherwork (eg tests for lateral extensions ordepth extensions or large-scale step-outdrilling).•Diagrams clearly highlighting the areas of | •Field work, including mapping andsampling, to better evaluate mineralisedareas is underway. |
| possible extensions, including the maingeological interpretations and futuredrilling areas, provided this information isnot commercially sensitive. |

This ASX announcement has been authorised for release by the Board of Raiden Resources Limited.
FOR FURTHER INFORMATION PLEASE CONTACT
DUSKO LJUBOJEVIC Managing Director RAIDEN RESOURCES LIMITED [email protected] www.raidenresources.com.au

Competent Person's Statement
The information in this announcement that relates to exploration results is based on and fairly represents information and supporting documentation prepared by Mr Martin Pawlitschek, a competent person who is a member of the Australian Institute of Geoscientists (AIG). Mr Martin Pawlitschek employed by Raiden Resources Limited. Mr Martin Pawlitschek has sufficient experience that is relevant to the style of mineralisation and type of deposits under consideration and to the activity being undertaken to qualify as a Competent Person as defined in the 2012 edition of the JORC Code. Mr Martin Pawlitschek has provided his prior written consent as to the form and context in which the exploration results and the supporting information are presented in this announcement.
Disclaimer:
Forward-looking statements are statements that are not historical facts. Words such as "expect(s)", "feel(s)", "believe(s)", "will", "may", "anticipate(s)", "potential(s)"and similar expressions are intended to identify forward-looking statements. These statements include, but are not limited to statements regarding future production, resources or reserves and exploration results. All of such statements are subject to certain risks and uncertainties, many of which are difficult to predict and generally beyond the control of the Company, that could cause actual results to differ materially from those expressed in, or implied or projected by, the forward-looking information and statements. These risks and uncertainties include, but are not limited to: (i) those relating to the interpretation of drill results, the geology, grade and continuity of mineral deposits and conclusions of economic evaluations, (ii) risks relating to possible variations in reserves, grade, planned mining dilution and ore loss, or recovery rates and changes in project parameters as plans continue to be refined, (iii) the potential for delays in exploration or development activities or the completion of feasibility studies, (iv) risks related to commodity price and foreign exchange rate fluctuations, (v) risks related to failure to obtain adequate financing on a timely basis and on acceptable terms or delays in obtaining governmental approvals or in the completion of development or construction activities, and (vi) other risks and uncertainties related to the Company's prospects, properties and business strategy. Investors are cautioned not to place undue reliance on these forwardlooking statements that speak only as of the date hereof, and the Company does not undertake any obligation to revise and disseminate forward-looking statements to reflect events or circumstances after the date hereof, or to reflect the occurrence of or non-occurrence of any events.
About Raiden Resources
Raiden Resources Limited . (ASX:RDN / DAX:YM4) is a dual listed base metal—gold focused exploration Company focused on the emerging prolific Tethyan metallogenic belt in Eastern Europe and has established a significant exploration footprint in Serbia and Bulgaria. More recently Raiden executed a transaction to purchase a highly prospective portfolio of gold, copper, nickel and PGE projects in the Pilbara region of Western Australia.
Over the last 3 years, the Company has secured one of the largest project portfolios, considered prospective for porphyry and epithermal mineralisation in Eastern Europe. The Company has defined over 20 porphyry, epithermal and polymetallic prospects over the course of 2019, a number of which the Company plans to drill test. Furthermore, initial work programs in the Pilbara are demonstrating the potential of the recently acquired portfolio and will lead to near term drilling.
The Directors believe that the Company is well positioned to unlock value from this exploration portfolio and deliver a significant mineral discovery.