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METEORIC RESOURCES NL — Capital/Financing Update 2014
Oct 27, 2014
65311_rns_2014-10-27_f2956625-6cc6-42ae-9692-bcec65cc6f35.pdf
Capital/Financing Update
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ASX ANNOUNCEMENT & MEDIA RELEASE
2 8 October 2 014
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HIG H GRADE COPP ER AND GO LD I NTERS ECTIONS C ONTI NUE AT BLU EBIR D
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Figure 1 – Ph a se II RC drillin g operations, Bluebird Prospect, Tennant Cre e k
HIGHLIGHTS
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Phase II RC drilling has returned more very high grade Tennant Creek style gold-bismuth-copper mineralisation
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New drill results include:
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BBRC0012: 31m at 2.48% Cu, 0.21g/t Au and 0.03% Bi from 116m Includi n g 12m at 4.41% Cu, 0 .23g/t Au a nd 0.02% B i from 125 m And 1 m at 11.50 % Cu, 1.44g / t Au and 0 . 04% Bi fro m 142m
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BBRC0010: 11m at 0.98g/t Au, 0.68% Cu and 0.03% Bi from 77m Including 2m at 3 .54g/t Au, 0.25% C u and 0.06 % Bi from 77m
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Diamond drilling of five holes underway to penetrate through to the high grade gold target position
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New footwall zone of mineralisation identified, increasing prospectivity
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Mineralisation still remains open along strike and down dip
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Width and grades continue to increase
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First signs of significant primary copper sulphide mineralisation observed in diamond core
Blaze International Limited ( A BN 15 074 7 2 8 019) 1st Floo r , 8 Parliamen t Place, West P erth, WA 600 5 • PO Box 1618, West Perth, WA 6872 t: +61 8 9481 7833 • f: +61 8 9481 7835 • www.blazelimited.com.a u
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P H A S E I I D R I L L I N G R E S U L T S
The RC component of the phase II drilling program at Bluebird is complete and final assay results have been received. Four holes were completed and a further five holes were partially completed with the RC rig. The most significant intersections for phase II so far are:
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BBRC0012: 31m at 2.48% Cu 0.21g/t, Au and 0.03% Bi from 116m including 12 m at 4.41% Cu, 0.23g/t Au and 0.02% Bi from 125m); and
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BBRC0010: 11m at 0.98g/t Au, 0.68% Cu and 0.03% Bi from 77m including 2m at 3.54g/t Au, 0.25% Cu and 0.06% Bi from 77m
These very impressive results were achieved from four mostly lower priority holes of the program. Five of the highest priority holes for phase II have not yet been completed and are yet to penetrate the high grade gold target position, which is located further downhole from the copper-gold zone. Only four of the nine phase II holes, mostly located around the margins of the mineralised system, penetrated through the high grade gold target position and reached final planned depth. The other five unfinished holes will be completed by diamond drilling from the RC pre-collars. The Company looks forward to reporting the remainder of the results as soon as possible after diamond drilling is completed. Diamond drilling is completed for BBDD0006 and BBDD0004, but logging and assay results are awaited. A summary of all intersections in this phase II program, irrespective of grade, is included in Appendix 2 of this report.
During the program, the diamond drill rig experienced a number of mechanical issues which has led to a delay in the completion of the program. These issues resulting in poor performance of the diamond rig have now been largely resolved. A change of crew and a double shift have been implemented, resulting in much improved production levels. Drilling conditions continue to be challenging due to broken ground, but the team are working hard to overcome this issue.
Figure 2 shows the status of the drilling so far at the Bluebird Prospect. The successfully completed phase II holes are BBDD0003, BBDD0004, BBDD0006, BBRC0009, BBRC0010, and BBRC0011 (results awaited for BBDD0004 and BBDD0006). The remaining holes will be diamond tailed to penetrate through the lower contact, which is the anticipated high grade gold position. Diamond drilling is in progress.
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Figure 2 – Long se c tion of Bluebir d , looking north, showing recent and historic d r illing. Note BB D D0004 is completed, but marked a s in progress a s sampling and logging are yet to be complete d
M E T A L Z O N A T I O N A N D P R O S P E C T I V I T Y
The new results indicate th a t the metal z onation between copper and gold a t Bluebird i s more sig n ificant and complex th a n previously interprete d . The high grade cop p er intersected in BB R C0012 is l o cated at a s imilar dept h and close t o the very h igh grade g old intersec t ion in BB D D-2. Howe v er it shoul d be noted t hat BBRC0012 is one of the hole s yet to pe n etrate through the lo w er ironston e contact w h ere the hi g h grade g o ld is expec t ed to be l o cated (Figure 3).
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Figure 3 – Cros s section at 448 3 80mE, looking west. Note that RC drilling of B BRC0012 sto p ped in mineral i sed
ironstone
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BB D D0003 was originally planned as a RC pre-coll a r with a di a mond tail, b ut was re-e n tered and completed b y the RC ri g due to the breakdown and delay w ith the dia m ond rig. Th e hole was extended w ell beyond d esigned de p th as it int e rsected several zones o f elevated c opper and iron in the footwall hematite shale s equence. T his significa n tly enhanc e s prospecti v ity by de m onstrating t he potential for additi o nal zones of footwall mineralisati o n not pre v iously targ e ted or inte r sected by drilling at Blu e bird (Figur e 4). The remaining ph a se II holes w ill be pus h ed deeper t o test for thi s potential f o otwall mine r alisation.
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Fi g ure 4 – Cross s ection at 4484 0 0mE, looking w est. Note the h ematite shales and chlorite h e matite breccia i n the footwall w h ich are anomalous in copper
I R O N S T O N E G E O M E T R Y A N D A L T E R A T I O N
The new result s indicate that the irons t one host g e ometry and the chlorit e -hematite breccia alte r ation patte r ns are m o re comple x than pre v iously inter p reted. Dril l ing is identifying sig n ificant chan g es in the ironstone c o mposition f r om magnetite dominan t , to jasper- q uartz do m inant, to hematite-chl o rite domin a nt as new areas are drilled at B luebird. T hese obs e rvations and their relati o nships wit h metal zon a tion and str u ctural archi t ecture are g reatly enh a ncing the Company’s understanding of the g eometry a n d controls o n minerali s ation. Pro s pectivity is significantly improved as areas of favourable alterati o n and str u ctural co m plexity are i d entified by d rilling.
An i mportant a s pect of the ongoing changes in g e ological int e rpretation i s demonstrated in Fig u re 5. BBR C 0013 was designed t o test the w e stern edge of and pos s ibly close o ff the min e ralised sys t em (also re f er to Figure 2). The hole returned a much broa d er zone of s trong cop p er minerali s ation and thicker irons t one than a n ticipated. It was event u ally termin a ted in stro n gly mineralised ironst o ne at leas t 20m beyond the exp e cted footw a ll contact o f the iron s tone, wher e the high grade gold zo n e is expect e d. This re s ult may rep r esent a bla n ket of sup e rgene enri c hed mineral i sation. BB R C0013 will b e diamond tailed in the c oming day s . The sup e rgene targ e t will be furt h er explored as part of t h e next drilli n g program.
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Fi g ure 5 – Cross section at 448 3 60mE, looking west, showing r ecent drilling r e sults. Note B B RC0013 stopp e d in
mineralised ironstone
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Another observ a tion from the recent dril l ing results is the spatial and geoch e mical relati o nship bet w een miner a lisation, alteration and a hematit e rich shal e unit (Hematite Shale). The He m atite Shale appears to b e more co m mon as deeper drilling t e sts the syst e m. It is ge n erally loc a ted below t h e footwall c ontact of the ironstone body, but i s sometimes intermingle d with the ironstone a n d the chlor i te-hematite breccia. T h e Hematite Shale can b e highly c h loritehe m atite altere d , and mine r alised, ass a ying up to 2 5% Fe an d over 1% C u as obser v ed in BB D D0003. F u ture drill pr o grams will a im to pene t rate throug h the hemat i te shale an d fully exp l ore its pote n tial to host s ignificant m i neralisation .
An e arly interpr e tation was t h at the ironstone body w as flattening in dip with d epth has b e en pro v en not to b e the case b y further drilling on all cross sections o ther than 4 4 8420E. This app a rent chang e in dip is still evident on the 448420 E cross section, but it is p ossibly related to thru s t fault offsets rather tha t changes in dip (Figure 6 ).
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Figure 6 – Cross s ection at 4484 2 0mE, looking w est. Note the a pparent change in dip, and B B RC0008 stop p ing in mineralised ironstone
D I S C O V E R Y O F P R I M A R Y S U L P H I D E S
Alth o ugh sulphi d e minerals have been o bserved in much of the drilling at Bluebird, the y have onl y been in mi n or concentr a tions. The mineralisati o n has generally been s t rongly weat h ered, with malachite b eing the do m inant visible copper mineral. Figur e 7 shows a HQ3 core s a mple fro m approxim a tely 150m d ownhole o f BBDD000 4 . This is the first sig n ificant amount of pri m ary sulphid e mineralisa t ion intersec t ed at Bluebird. Based o n these ob s ervations t h ere is goo d potential f o r significant primary sul p hide miner a lisation at d e pth.
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Figure 7 – Str o ng primary sulphide minerali s ation intersected by BBDD000 4
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D I S C U S S I O N A N D F O L L O W - U P P L A N S
Phase II diamo n d drilling is in progress and sched u led for com p letion by l a te October. Final ass a y results can be expect e d by the thi r d week of N ovember.
3D m odels will b e re-interpr e ted and up d ated following the recei p t of the fin a l results. T h e aim of t h is work will be to gene r ate an initi a l resource m odel, determine if a J O RC 2012 m ineral res o urce estima t e can be p u blished, an d to initiate a high level s c oping stud y for the proj e ct.
The diamond ri g will remain in the Tenn a nt Creek r e gion to drill for other cli e nts. If the r esults of P hase II are supportive, there are p r ovisions fo r at least tw o deeper h o les in the c urrent Bar k ly Mine M a nagement P lan. These holes ha v e been pe g ged and p r epared rea d y for drilling. The dia m ond rig wil l be able to r eturn to drill these extra holes at ver y short notic e .
H I G H G R A D E C H E C K S
Du e to the ver y high grade s and coar s e grained n a ture of the mineralisati o n, the lab o ratory con t inues to ex p erience ch a llenges wit h the repeatability of th e assay res u lts. Extra Q AQC and checks ha v e been req u ired to ens u re that the results are c orrect and repeatable b efore the y can be rel e ased. This h as been a r e ason for th e delay in reporting of a s say results, but is nec e ssary give n the excepti o nally high g rades identi f ied in the program so fa r .
B A R K L Y C O P P E R - G O L D P R O J E C T
Bla z e Internati o nal Limited is in a F arm-In Joi n t Venture Agr e ement wit h Meteoric Resources NL over t he highly pro s pective Barkly Copper-Gold project . Blaze has the right to e arn up to a n 80% inte r est in the p roject. The project is loc a ted around 3 0 km east o f the town of Tennant C r eek in the Nor t hern Territo r y (Figure 8).
The Bluebird c opper-gold prospect a t the Barkly Project co m prises a 1. 6 km-long gr a vity ridge o p en to the e ast where sha l low geoche m ical drillin g by Meteori c Resource s identified a 6 00m-long c opper an o maly, also open to the east. Pre v iously rep o rted follo w -up drillin g confirmed Tennant Cre e k-style c o pper-gold mineralisati o n associ a ted with iron s tone. The ironstone s and min e ralisation are often discordant to th e host sedi m ents and a re consider e d to be a hig h -grade var i ant of the iron oxid e -copper-gold (IOCG) dep o sits found i n Proterozoi c terranes in Australia.
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Figure 8 – L ocation of the Barkly Cu-Au proje ct
As p art of the e a rn-in to the Barkly Project, Blaze ha s recently c o mpleted tw o RC and di a mond drilling program s targeting copper-gold m ineralisation at the Blu e bird prospe c t. The Co m pany has also compl e ted a re int e rpretation o f the geophysics and g e nerated a s eries of magnetic and gravity targ e ts within th e Barkly JV a rea (Figure 9)
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D R I L L R E S U L T S S U M M A R Y T A B L E
Table 1 below contains summary intersections using nominal 0.2% Cu and 0.2g/t Au cut-off grade. These cut-off grades were selected as they best represent the overall mineralised envelope at the Bluebird Prospect. The full set of results contained in Appendix 2 of this report.
| Hole ID | Length | **Collar Location GDA94 ** | **Collar Location GDA94 ** | **Collar Location GDA94 ** | **Dip ** | Azimuth | From m |
To m |
Cu Grade % |
Au Grade g/t |
Bi Grade % |
Width m |
Intersection Description |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| East |
North |
RL |
|||||||||||
| BBDD‐1 | 129.2 | **448400 ** | 7827075 | 328 | ‐60 | 0 | 89 | 92.8 | 1.26 | 0.08 | 0.01 | 3.8 | 3.8m @ 1.26% Cu, 0.08g/t Au, 0.01% Bi |
| 107.2 | 114 | 0.45 | 0.08 | 0.01 | 6.8 | 6.8m @ 0.45% Cu, 0.08g/t Au, 0.01% Bi | |||||||
| BBDD‐2 | 198 | **448400 ** | 7827025 | 324 | ‐60 | 0 | 135.5 | 140 | 1.35 | 0.22 | 0.03 | 4.5 | 4.5m @ 1.35% Cu, 0.22g/t Au, 0.03% Bi |
| 157 | 177 | 0.61 | 8.17 | 0.22 | 20 | 20m @ 8.17g/t Au, 0.61%Cu, 0.22% Bi | |||||||
| includes | 169 | 173 | 0.66 | 37.90 | 0.80 | 4 | 4m@ 37.90g/t Au, 0.66% Cu, 0.80% Bi | ||||||
| and | 171 | 172 | 0.94 | 62.30 | 1.11 | 1 | 1m @ 62.30g/t Au, 0.94% Cu, 1.11% Bi | ||||||
| BBDD0003 | 251 | **448400 ** | 7826997 | 328 | ‐60 | 0 | 163 | 179 | 0.44 | 0.06 | 0.00 | 16 | 16m @ 0.44% Cu, 0.06g/t Au |
| 188 | 195 | 0.64 | 0.07 | 0.02 | 7 | 7m@ 0.64% Cu, 0.07g/t Au, 0.02% Bi | |||||||
| 228 | 235 | 0.34 | 0.02 | 0.00 | 7 | 7m@ 0.34% Cu, 0.02g/t Au | |||||||
| **BBDD0004 ** | 240.7 | **448420 ** | 7827013 | 329 | ‐60 | 0 | In Progress | ||||||
| BBDD0005 | 50* | **448420 ** | 7827085 | 329 | ‐60 | 0 | In Progress | ||||||
| **BBDD0006 ** | 113.2 | **448380 ** | 7827104 | 330 | ‐60 | 0 | In Progress | ||||||
| BBRC‐1 | 100 | **448329 ** | 7827204 | 326 | ‐60 | 90 | Meteroric Resources Hole NSI | ||||||
| BBRC‐2 | 137 | **448400 ** | 7827050 | 323 | ‐60 | 0 | 115 | 119 | 4.69 | 4 | Meteroric Resources Hole 4m @ 4.69% Cu, 0.38g/t Au, 170g/t Bi | ||
| BBRC‐3 | 155 | **448519 ** | 7827033 | 323 | ‐60 | 0 | Meteroric Resources Hole NSI | ||||||
| BBRC‐4 | 77 | **448400 ** | 7827120 | 331 | ‐60 | 0 | Anomalous Zone 37‐55m @ 213ppm Cu | ||||||
| BBRC‐5 | 113 | **448400 ** | 7827097 | 328 | ‐60 | 0 | 62 | 87 | 1.89 | 0.27 | 0.03 | 25 | 25m @ 1.89% Cu, 0.27g/t Au, 0.03% Bi |
| includes | 66 | 68 | 2.98 | 0.42 | 0.12 | 2 | 2m @ 2.98% Cu, 0.42g/t, 0.12% Bi | ||||||
| and | 74 | 78 | 8.93 | 1.05 | 0.01 | 4 | 4m @ 8.93% Cu, 1.05g/t Au, 0.01% Bi | ||||||
| includes | 75 | 77 | 16.50 | 0.15 | 0.01 | 2 | 2m @ 16.50% Cu, 0.15g/t Au, 0.01% Bi | ||||||
| and | 75 | 76 | 24.20 | 0.21 | 0.01 | 1 | 1m@ 24.2% Cu, 0.21g/t Au, 0.01% Bi | ||||||
| and | 76 | 77 | 1.20 | 3.81 | 0.01 | 1 | 1m@ 3.81g/t Au, 1.20% Cu, 0.01% Bi | ||||||
| BBRC‐6 | 203 | **448440 ** | 7827030 | 328 | ‐60 | 126 | 135 | 0.89 | 0.36 | 0.04 | 9 | 9m @ 0.89% Cu, 0.36g/t Au, 0.04% Bi | |
| includes | 126 | 128 | 0.09 | 1.21 | 0.01 | 2 | 2m @ 1.21g/t Au, 0.09% Cu, 0.01% Bi | ||||||
| and | 128 | 130 | 2.50 | 0.13 | 0.06 | 2 | 2m@ 2.50% Cu, 0.13g/t Au, 0.06% Bi | ||||||
| 146 | 149 | 0.80 | 1.57 | 0.02 | 3 | 3m @ 1.57g/t Au, 0.80% Cu, 0.02% Bi | |||||||
| 154 | 160 | 0.05 | 0.56 | 0.03 | 6 | 6m @ 0.56g/t Au, 0.05% Cu, 0.03% Bi | |||||||
| BBRC‐7 | 137 | **448360 ** | 7827081 | 328 | ‐60 | 0 | 87 | 90 | 0.38 | 0.69 | 0 | 3 | 3m @ 0.69g/t Au, 0.38% Cu |
| 100 | 105 | 0.29 | 0.06 | 0 | 5 | 5m @ 0.29% Cu, 0.06g/t Au | |||||||
| BBRC0008 | 140* | **448420 ** | 7827052 | 329 | ‐60 | 0 | 110 | 134 | 0.73 | 0.31 | 0.05 | 24 | 24m@ 0.73% Cu, 0.31g/t Au, 0.05% Bi |
| includes | 111 | 113 | 1.85 | 1.29 | 0.16 | 2 | 2m @ 1.29g/t Au, 1.85% Cu, 0.16% Bi | ||||||
| and | 121 | 123 | 2.72 | 0.04 | 0.01 | 2 | 2m @ 2.72% Cu, 0.04g/t Au, 0.01% Bi | ||||||
| BBRC0009 | 100 | **448420 ** | 7827106 | 330 | ‐60 | 0 | 73 | 76 | 0.43 | 0.04 | 0 | 3 | 3m @ 0.43% Cu, 0.04g/t Au |
| BBRC0010 | 120 | **448380 ** | 7827082 | 329 | ‐60 | 0 | 77 | 88 | 0.68 | 0.98 | 0.03 | 11 | 11m@ 0.98g/t Au, 0.68% Cu, 0.03% Bi |
| Includes | 77 | 79 | 0.25 | 3.54 | 0.06 | 2 | 2m@ 3.54g/t Au, 0.25% Cu, 0.06% Bi | ||||||
| BBRC0011 | 245 | **448380 ** | 7827009 | 329 | ‐60 | 0 | 167 | 169 | 1.2 | 0.07 | 0.05 | 2 | 2m @ 1.20% Cu, 0.07g/t Au |
| 206 | 209 | 0.35 | 0.08 | 0 | 3 | 3m @ 0.35% Cu, 0.08g/t Au | |||||||
| BBRC0012 | 149* | **448380 ** | 7827049 | 329 | ‐60 | 0 | 116 | 147 | 2.48 | 0.21 | 0.03 | 31 | 31m@ 2.48% Cu, 0.21g/t Au, 0.03% Bi |
| includes | 125 | 137 | 4.41 | 0.23 | 0.02 | 12 | 12m@ 4.41% Cu, 0.23g/t Au, 0.02% Bi | ||||||
| and | 142 | 143 | 11.5 | 1.44 | 0.04 | 1 | 1m @ 11.50% Cu, 1.44g/t Au, 0.04% Bi | ||||||
| BBRC0013 | 179* | **448360 ** | 7827040 | 329 | ‐60 | 0 | 124 | 130 | 1.44 | 0.05 | 0.01 | 6 | 6m @ 1.44% Cu, 1.05g/t Au |
| 161 | 179 | 1.09 | 0.43 | 0.02 | 18 | 18m @ 1.09% Cu, 0.43g/t Au, 0.02% Bi | |||||||
| includes | 166 | 167 | 3.91 | 0.78 | 0.02 | 1 | 1m@ 3.91% Cu, 0.78g/t Au, 0.02% Bi |
Table 1 - Drill hole intersection summary results, Bluebird prospect. Copper cut-off grade 0.2%. Gold cut-off grade 0.2g/t.
Reverse circulation (RC) drilling samples are collected as 1m composite samples through a cyclone which are cone split for analysis. Each 1m split sample is analysed with a handheld XRF analyser. Anomalous 1m split samples are submitted to Bureau Veritas Laboratory in Perth for more precise analysis. All other samples are sampled as 4m composites by sampling with a spear and submitted to the laboratory. Diamond drill core is cut in half with an Almonte core saw and sampled on nominal 1m intervals for analysis.
All drill samples submitted to the laboratory are crushed and pulverised followed by a four acid total digest and multielement analysis by inductively coupled plasma optical emission spectrometry (ICP-OES) and inductively coupled plasma mass spectrometry (ICP-MS). Gold and precious metal analysis are completed by a 40g fire assay collection and inductively coupled plasma optical emission spectrometry (ICP-OES). Sample preparation and analysis are undertaken at Bureau Veritas Laboratory in Darwin, NT and Perth, WA.
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Figure 9 – Region a l prospectivity map of the Bar k ly Cu-Au project. Blue lines s h ow ironstone t r ends througho u t the lice n ce. Ironstones a re prospective for other high- g rade Tennant C reek style de p osits. The whi t e stars show t h e high priority explor a tion targets ba s ed on magneti c and gravity d a ta interpretatio n
Competent Person Declaration
The i nformation in t his report that relates to Exp l oration Result s , Mineral Res o urces or Ore R eserves is ba s ed on infor m ation compile d by Luke Mar s hall, who is a Full time empl o yee of Golde n Deeps Limite d , consulting t o Blaze Inter n ational Limite d , and a me m ber of The A u stralasian Ins t itute of Geos c ientists. Mr M arshall has s u fficient experience that is r e levant to the st y le of mineralis a tion and type o f deposit unde r consideration a nd to the acti v ity that he i s undertaking t o qualify as a C ompetent Pe r son as define d in the 2012 E dition of the “ A ustralasian C o de for Rep o rting of Explor a tion Results, M ineral Resour c e and Ore Re s erves”. Mr Marshall consents to the inclusio n in the repo r t of the matter s based on his i n formation in th e form and con t ext in which it a ppears.
Forward-Looking Statements
This document ma y include forwa r d-looking stat e ments. Forwar d -looking state m ents include, but are not li m ited to, statements concerning Blaze Inter n ational Limited ’ s planned expl o ration progra m me and other s tatements that are not histo r ical facts. Wh e n used in this d ocument, the w ords such as "could," "plan," "estimate," "e x pect," "intend, " "may”, "pot e ntial," "should, " and similar e xpressions ar e forward-looki n g statements. Although Blaz e International Limited belie v es that its ex p ectations refle c ted in these f o rward-looking s tatements are reasonable, s u ch statements involve risks and uncertainties and no ass u rance can be g iven that actu a l results will be consistent wit h these forward - looking statements.
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APPENDIX 1 – JORC 2012
JORC TABLE 1, Section 1 Sampling Techniques and Data
| Criteria | Explanation |
|---|---|
| Sampling techniques |
Exploration results are based on industry best practices, including sampling, assay methods, and appropriate quality assurance quality control (QAQC) measures. Reverse circulation (RC) drilling samples are collected as 1m composite samples through a cyclone which are cone split for analysis. Each 1m bulk sample is analysed with a handheld XRF analyser. Anomalous 1m split samples are submitted to Bureau Veritas Laboratory in Perth for more precise analysis. Core samples are taken as half NQ core and sampled on nominal 1m intervals, with sampling breaks adjusted to geological boundaries where appropriate. All drill samples submitted to the laboratory are crushed and pulverised followed by a four acid total digest and multi-element analysis by inductively coupled plasma optical emission spectrometry (ICP-OES) and inductively coupled plasma mass spectrometry (ICP-MS). Gold and precious metal analysis are completed by a 40g fire assay collection with inductively coupled plasma optical emission spectrometry (ICP-OES) finish. Sample preparation and analysis are undertaken at Bureau Veritas Laboratory in Darwin, NT and Perth, WA. |
| Drilling techniques |
RC drilling is completed by a 5 ¼ inch diameter hole drilled with a face sampling hammer. Diamond drillholes are collared using RC and switch to NQ2 approximately 30m before the target position is intersected. All coordinates are quoted in GDA94 datum unless otherwise stated. |
| Drill Sample Recovery |
The quality of RC drilling samples is optimised by the use of cone splitters and the logging of various criteria designed to record sample size, recovery and contamination, and use of field duplicates to measure sample precision. The quality of diamond core samples is monitored by the logging of various geotechnical parameters, and logging of core recovery and competency. The quality of analytical results is monitored by the use of internal laboratory procedures together with certified standards, duplicates and blanks and statistical analysis on a monthly basis to ensure that results are representative and within acceptable ranges of accuracy and precision. |
| Logging | All logging is completed according to industry best practice. RC drill chips are wet sieved on 1m intervals, logged and then stored in plastic chip trays for future reference. Diamond core is stored in clearly labelled core trays. Logging is completed using a standard Maxwell logging template. The resulting data is uploaded to a Datashed database and validated. Once validated, the data is exported to 3D modelling software for visual validation and interpretation. Detailed information on lithology, sample quality, structure, geotechnical information, alteration and mineralisation are collected in a series of detailed self-validating logging templates. |
| Sub- sampling techniques and sample preparation |
Core is cut using a brick saw fitted with a special blade designed for cutting core. Half core is taken for sampling. RC samples are riffle split on 1m intervals when dry. When wet, samples are dried out before riffle splitting takes place. RC drilling is generally stopped when samples become wet. For all sample types, the nature, quality and appropriateness of the sample preparation technique is considered adequate as per industry best practice. Two field duplicates are taken per RC hole to ensure the samples are representative; one 4m duplicate and one 1m duplicate. The duplicates are taken in anomalous copper grades where possible. Quality control reports are undertaken routinely to monitor the performance of field |
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| standards and duplicates, and laboratory accuracy and precision. Sample sizes are appropriate to the grain size of the material being sampled. |
|
|---|---|
| Quality of assay data and laboratory tests |
The samples have been sorted, dried, crushed and pulverised. Primary preparation has been by crushing the whole sample. The samples have been split with a riffle splitter, if required, to obtain a 3kg sub-fraction which has then been pulverised in a vibrating pulveriser. The sample(s) have been digested with a mixture of four Acids including Hydrofluoric, Nitric, Hydrochloric and Perchloric Acids for a total digest. Ag, As, Cd, Co, Bi, In, Mo, Sn, W have been determined by Inductively Coupled Plasma (ICP) Mass Spectrometry. Al, Ca, Cu, Fe, K, Mg, Mn, Na, Pb, S, V, Zn have been determined by Inductively Coupled Plasma (ICP) Optical Emission Spectrometry. Au and PGEs are determined by a 40g fire assay collection with Inductively Coupled Plasma (ICP) Optical Emission Spectrometry finish. Field Standards and Blanks are inserted every 20 samples, Laboratory inserts its own standards and blanks at random intervals, but several are inserted per batch regardless of the size of the batch. |
| Verification of sampling and assaying |
All significant intercepts are reviewed and confirmed by at least three senior personnel before release to the market_._ No adjustments are made to the raw assay data. Data is imported directly to Datashed in raw original format. All data are validated using the QAQCr reporter validation tool with Datashed. Visual validations are then carried out by senior staff members. |
| Location of data points |
Holes are set out using a sub 20mm RTDGPS. Collars are picked up by a licenced surveyor by RTDGPS on completion of the hole. |
| Data spacing and distribution |
Data spacing and distribution used to determine geological continuity is dependent on the deposit type and style under consideration. Where a mineral resource is estimated, the appropriate data spacing and density is decided and reported by the competent person. For mineral resource estimations, grades are estimated on composited assay data. The composite length is chosen based on the statistical average, usually 1m. Sample compositing is never applied to interval calculations reported to market. A sample length weighted interval is calculated as per industry best practice. |
| Orientation of data in relation to geological structure |
Orientation of sampling is as unbiased as possible based on the dominating mineralised structures and interpretation of the deposit geometry. If structure and geometry is not well understood, sampling is orientated to be perpendicular to the general strike of stratigraphy and/or regional structure. If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this would be assessed and reported if considered material. Drilling is at an angle to surface and drilled to maximise perpendicular intersection with the known interpretation of the strike of previously intersected mineralisation. |
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| Sample security | All samples remain in the custody of company geologists, and are fully supervised from point of field collection to transport depot drop-off. |
|---|---|
| Audits and reviews |
None yet undertaken for this dataset. |
Section 2 Reporting of Exploration Results
| Criteria | Explanation |
|---|---|
| Mineral tenement and land tenure status |
The Company controls one Exploration Licences, EL28620 in the Tennant Creek area. All tenure was in good standing at the time of reporting. There are no known impediments with respect to obtaining a licence to operate in the area. The Company is earning an 80% interest in the EL28620. There are no known native title interests, historical sites, and wilderness or national park areas of environmental impediments. |
| Exploration done by other parties |
Several other parties have undertaken exploration in the area between the 1930’s through to 2007. These parties include Posgold and Meteoric Resources. |
| Geology | At Bluebird, copper-gold-bismuth mineralisation is concentrated in an east west striking ironstone host unit. The host unit cross cuts stratigraphy which is mostly made up of siltstone and greywacke sediments. |
| Drill hole Information |
All relevant drillhole information is supplied in appendix 1 of the announcement. |
| Data aggregation methods |
All exploration results are reported by a length weighted average. This ensures that short lengths of high grade material receive less weighting than longer lengths of low grade material. No high grade cut-offs are applied. A nominal low grade cut-off of 0.2% Cu and 0.2g/t Au are used with a maximum internal dilution of 5m for reporting of results. These cut-off grades give the best representation of the overall mineralised envelope at Bluebird. |
| Relationship between mineralisation widths and intercept lengths |
Mineralisation at Bluebird is interpreted to be striking at east west with a dip of -70 to -80 degrees towards the south. All holes are drilled to be as perpendicular as practicable to the above orientation. |
| Diagrams | A comprehensive set of relevant diagrams are included in the body of the announcement. |
| Balanced reporting |
All background available information is discussed in the body of the announcement. No data is excluded. Full drilling results for copper and gold assay information are shown in Appendix 2 of the report. |
| Further work | Plans for further work are outlined in the body of the announcement. |
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APPENDIX 2 – Detailed Drilling Laboratory Assay Results. BDL – Indicates results below assay detection limit
| Hole ID | Easting | Northing | RL | **mFrom ** | mTo | **Au ppm ** | Cu % | **Bippm ** |
|---|---|---|---|---|---|---|---|---|
| BBDD0003 | 448400 | 7826997 | 325 | 160 | 161 | BDL | 0.002 | 2.6 |
| BBDD0003 | 161 | 162 | BDL | 0.0012 | 1.4 | |||
| BBDD0003 | 162 | 163 | BDL | 0.0254 | 3.3 | |||
| BBDD0003 | 163 | 164 | 0.045 | 0.499 | 21.1 | |||
| BBDD0003 | 164 | 165 | 0.035 | 0.164 | 206 | |||
| BBDD0003 | 165 | 166 | 0.023 | 0.0146 | 13.6 | |||
| BBDD0003 | 166 | 167 | 0.06 | 0.0054 | 11 | |||
| BBDD0003 | 167 | 168 | 0.167 | 0.0736 | 139 | |||
| BBDD0003 | 168 | 169 | 0.343 | 1.08 | 188 | |||
| BBDD0003 | 169 | 170 | 0.189 | 0.287 | 127 | |||
| BBDD0003 | 170 | 171 | 0.012 | 0.095 | 23.5 | |||
| BBDD0003 | 171 | 172 | 0.005 | 0.478 | 38 | |||
| BBDD0003 | 172 | 173 | 0.005 | 0.302 | 27.1 | |||
| BBDD0003 | 173 | 174 | 0.012 | 0.906 | 27.3 | |||
| BBDD0003 | 174 | 175 | 0.026 | 1.19 | 30.4 | |||
| BBDD0003 | 175 | 176 | 0.001 | 0.252 | 7 | |||
| BBDD0003 | 176 | 177 | 0.026 | 0.411 | 21.4 | |||
| BBDD0003 | 177 | 178 | 0.016 | 1.15 | 156 | |||
| BBDD0003 | 178 | 179 | 0.033 | 0.206 | 37.8 | |||
| BBDD0003 | 179 | 180 | 0.001 | 0.0322 | 11.1 | |||
| BBDD0003 | 180 | 181 | BDL | 0.016 | 4.9 | |||
| BBDD0003 | 181 | 182 | BDL | 0.0052 | 2.5 | |||
| BBDD0003 | 182 | 183 | BDL | 0.005 | 2 | |||
| BBDD0003 | 183 | 184 | 0.001 | 0.0062 | 2.7 | |||
| BBDD0003 | 184 | 185 | 0.002 | 0.003 | 2.8 | |||
| BBDD0003 | 185 | 186 | 0.002 | 0.013 | 4.5 | |||
| BBDD0003 | 186 | 187 | BDL | 0.0066 | 6.6 | |||
| BBDD0003 | 187 | 188 | BDL | 0.0072 | 3.2 | |||
| BBDD0003 | 188 | 189 | 0.201 | 0.774 | 1160 | |||
| BBDD0003 | 189 | 190 | 0.057 | 0.886 | 100 | |||
| BBDD0003 | 190 | 191 | 0.017 | 0.308 | 55.2 | |||
| BBDD0003 | 191 | 192 | 0.065 | 1.01 | 91.3 | |||
| BBDD0003 | 192 | 193 | 0.068 | 0.551 | 17.6 | |||
| BBDD0003 | 193 | 194 | 0.01 | 0.21 | 9.1 | |||
| BBDD0003 | 194 | 195 | 0.056 | 0.726 | 65.6 | |||
| BBDD0003 | 195 | 196 | 0.027 | 0.126 | 64.3 | |||
| BBDD0003 | 196 | 197 | 0.004 | 0.048 | 19.7 | |||
| BBDD0003 | 197 | 198 | 0.016 | 0.0782 | 75.4 | |||
| BBDD0003 | 198 | 199 | 0.005 | 0.0706 | 13.2 | |||
| BBDD0003 | 199 | 200 | 0.123 | 0.753 | 53.8 |
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| BBDD0003 | 200 | 201 | 0.048 | 0.323 | 110 | |||
|---|---|---|---|---|---|---|---|---|
| BBDD0003 | 201 | 202 | 0.002 | 0.0062 | 29.2 | |||
| BBDD0003 | 202 | 203 | 0.143 | 0.0374 | 204 | |||
| BBDD0003 | 203 | 204 | 0.774 | 0.396 | 1830 | |||
| BBDD0003 | 204 | 205 | 0.065 | 0.0704 | 130 | |||
| BBDD0003 | 205 | 206 | 0.024 | 0.0366 | 202 | |||
| BBDD0003 | 206 | 207 | 0.015 | 0.0326 | 89.5 | |||
| BBDD0003 | 207 | 208 | 0.009 | 0.02 | 37.5 | |||
| BBDD0003 | 208 | 209 | 0.03 | 0.138 | 111 | |||
| BBDD0003 | 209 | 210 | 0.249 | 0.099 | 1810 | |||
| BBDD0003 | 210 | 211 | 0.054 | 0.0998 | 210 | |||
| BBDD0003 | 211 | 212 | 0.049 | 0.118 | 54.5 | |||
| BBDD0003 | 212 | 213 | 0.005 | 0.0114 | 10.5 | |||
| BBDD0003 | 213 | 214 | 0.018 | 0.108 | 39.2 | |||
| BBDD0003 | 214 | 215 | BDL | 0.008 | 21.1 | |||
| BBDD0003 | 215 | 216 | 0.004 | 0.182 | 72 | |||
| BBDD0003 | 216 | 217 | 0.006 | 0.147 | 29.5 | |||
| BBDD0003 | 217 | 218 | 0.006 | 0.0848 | 13.5 | |||
| BBDD0003 | 218 | 219 | 0.015 | 0.135 | 10.9 | |||
| BBDD0003 | 219 | 220 | BDL | 0.022 | 14.7 | |||
| BBDD0003 | 220 | 221 | 0.002 | 0.0032 | 2.9 | |||
| BBDD0003 | 221 | 222 | BDL | 0.0024 | 7 | |||
| BBDD0003 | 222 | 223 | BDL | 0.0016 | 9.3 | |||
| BBDD0003 | 223 | 224 | BDL | 0.0012 | 16.1 | |||
| BBDD0003 | 224 | 225 | BDL | 0.0014 | 2.9 | |||
| BBDD0003 | 225 | 226 | BDL | 0.0022 | 6.8 | |||
| BBDD0003 | 226 | 227 | BDL | 0.0016 | 4.3 | |||
| BBDD0003 | 227 | 228 | 0.002 | 0.0284 | 10.5 | |||
| BBDD0003 | 228 | 229 | 0.007 | 1.05 | 66.2 | |||
| BBDD0003 | 229 | 230 | 0.038 | 0.334 | 51.1 | |||
| BBDD0003 | 230 | 231 | 0.004 | 0.119 | 56.6 | |||
| BBDD0003 | 231 | 232 | 0.001 | 0.0444 | 30.4 | |||
| BBDD0003 | 232 | 233 | 0.004 | 0.15 | 61.1 | |||
| BBDD0003 | 233 | 234 | 0.017 | 0.445 | 109 | |||
| BBDD0003 | 234 | 235 | 0.066 | 0.244 | 114 | |||
| BBDD0003 | 235 | 236 | 0.008 | 0.127 | 54.7 | |||
| BBDD0003 | 236 | 237 | 0.003 | 0.132 | 11.6 | |||
| BBDD0003 | 237 | 238 | 0.006 | 0.0878 | 8.5 | |||
| BBDD0003 | 238 | 239 | 0.002 | 0.0464 | 6.8 | |||
| BBDD0003 | 239 | 240 | 0.001 | 0.0078 | 3.2 | |||
| BBRC0008 | 448420 | 7827052 | 325 | 99 | 100 | 0.023 | 0.0384 | 14.9 |
| BBRC0008 | 100 | 101 | 0.108 | 0.0764 | 40.6 | |||
| BBRC0008 | 101 | 102 | 0.062 | 0.096 | 53.4 | |||
| BBRC0008 | 102 | 103 | 0.105 | 0.0834 | 38.4 |
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| BBRC0008 | 103 | 104 | 0.012 | 0.183 | 120 | |||
|---|---|---|---|---|---|---|---|---|
| BBRC0008 | 104 | 105 | 0.028 | 0.0744 | 34.5 | |||
| BBRC0008 | 105 | 106 | 0.01 | 0.064 | 12.9 | |||
| BBRC0008 | 106 | 107 | 0.012 | 0.062 | 13.2 | |||
| BBRC0008 | 107 | 108 | 0.05 | 0.201 | 54.4 | |||
| BBRC0008 | 108 | 109 | 0.143 | 0.155 | 33.4 | |||
| BBRC0008 | 109 | 110 | 0.193 | 0.148 | 126 | |||
| BBRC0008 | 110 | 111 | 0.485 | 0.156 | 737 | |||
| BBRC0008 | 111 | 112 | 0.358 | 2.52 | 1690 | |||
| BBRC0008 | 112 | 113 | 2.22 | 1.18 | 1580 | |||
| BBRC0008 | 113 | 114 | 0.201 | 0.252 | 921 | |||
| BBRC0008 | 114 | 115 | 1.5 | 0.247 | 2260 | |||
| BBRC0008 | 115 | 116 | 0.662 | 0.225 | 1450 | |||
| BBRC0008 | 116 | 117 | 0.653 | 0.165 | 1310 | |||
| BBRC0008 | 117 | 118 | 0.602 | 0.114 | 561 | |||
| BBRC0008 | 118 | 119 | 0.378 | 0.158 | 456 | |||
| BBRC0008 | 119 | 120 | 0.126 | 0.137 | 131 | |||
| BBRC0008 | 120 | 121 | 0.068 | 0.841 | 138 | |||
| BBRC0008 | 121 | 122 | 0.044 | 2.44 | 152 | |||
| BBRC0008 | 122 | 123 | 0.036 | 3 | 150 | |||
| BBRC0008 | 123 | 124 | 0.059 | 0.63 | 182 | |||
| BBRC0008 | 124 | 125 | 0.022 | 1.09 | 130 | |||
| BBRC0008 | 125 | 126 | 0.022 | 0.486 | 59.3 | |||
| BBRC0008 | 126 | 127 | 0.024 | 0.603 | 97.1 | |||
| BBRC0008 | 127 | 128 | 0.02 | 0.386 | 111 | |||
| BBRC0008 | 128 | 129 | 0.012 | 0.203 | 83.9 | |||
| BBRC0008 | 129 | 130 | 0.007 | 0.242 | 50 | |||
| BBRC0008 | 130 | 131 | 0.013 | 0.251 | 56.1 | |||
| BBRC0008 | 131 | 132 | 0.009 | 0.675 | 88 | |||
| BBRC0008 | 132 | 133 | 0.018 | 0.752 | 112 | |||
| BBRC0008 | 133 | 134 | 0.01 | 0.837 | 175 | |||
| BBRC0008 | 134 | 135 | 0.004 | 0.174 | 78 | |||
| BBRC0008 | 135 | 136 | 0.002 | 0.143 | 109 | |||
| BBRC0008 | 136 | 137 | 0.004 | 0.11 | 66.2 | |||
| BBRC0008 | 137 | 138 | 0.002 | 0.0612 | 48.1 | |||
| BBRC0008 | 138 | 139 | BDL | 0.0868 | 83.6 | |||
| BBRC0008 | 139 | 140 | BDL | 0.078 | 30.5 | |||
| BBRC0008 | 96 | 97 | 0.001 | 0.003 | 2.4 | |||
| BBRC0008 | 97 | 98 | BDL | 0.0022 | 2 | |||
| BBRC0008 | 98 | 99 | 0.002 | 0.0232 | 7.3 | |||
| BBRC0009 | 448420 | 7827106 | 325 | 44 | 45 | BDL | 0.0022 | 4.3 |
| BBRC0009 | 45 | 46 | 0.001 | 0.0048 | 14.2 | |||
| BBRC0009 | 46 | 47 | 0.012 | 0.0288 | 112 | |||
| BBRC0009 | 47 | 48 | 0.007 | 0.023 | 114 |
16
==> picture [364 x 63] intentionally omitted <==
| BBRC0009 | 48 | 49 | 0.009 | 0.0286 | 66.2 | |||
|---|---|---|---|---|---|---|---|---|
| BBRC0009 | 49 | 50 | 0.01 | 0.0236 | 47.4 | |||
| BBRC0009 | 50 | 51 | 0.009 | 0.055 | 21.9 | |||
| BBRC0009 | 51 | 52 | 0.005 | 0.128 | 12.5 | |||
| BBRC0009 | 52 | 53 | 0.002 | 0.12 | 24.8 | |||
| BBRC0009 | 53 | 54 | 0.01 | 0.124 | 26.3 | |||
| BBRC0009 | 54 | 55 | 0.007 | 0.0608 | 27.1 | |||
| BBRC0009 | 55 | 56 | 0.009 | 0.04 | 22.6 | |||
| BBRC0009 | 56 | 57 | 0.003 | 0.0574 | 18 | |||
| BBRC0009 | 57 | 58 | 0.063 | 0.0494 | 43.5 | |||
| BBRC0009 | 58 | 59 | 0.041 | 0.0288 | 31.1 | |||
| BBRC0009 | 59 | 60 | 0.037 | 0.0182 | 33.4 | |||
| BBRC0009 | 60 | 61 | 0.195 | 0.0096 | 20.7 | |||
| BBRC0009 | 61 | 62 | 0.027 | 0.0078 | 40.1 | |||
| BBRC0009 | 62 | 63 | 0.011 | 0.0076 | 129 | |||
| BBRC0009 | 63 | 64 | 0.026 | 0.0104 | 547 | |||
| BBRC0009 | 64 | 65 | 0.016 | 0.0184 | 1950 | |||
| BBRC0009 | 65 | 66 | 0.005 | 0.0208 | 103 | |||
| BBRC0009 | 66 | 67 | 0.013 | 0.0216 | 106 | |||
| BBRC0009 | 67 | 68 | 0.018 | 0.0078 | 41 | |||
| BBRC0009 | 68 | 69 | 0.03 | 0.0046 | 88.7 | |||
| BBRC0009 | 69 | 70 | 0.018 | 0.0078 | 68.1 | |||
| BBRC0009 | 70 | 71 | 0.016 | 0.0176 | 558 | |||
| BBRC0009 | 71 | 72 | 0.008 | 0.0552 | 374 | |||
| BBRC0009 | 72 | 73 | 0.156 | 0.115 | 60.8 | |||
| BBRC0009 | 73 | 74 | 0.051 | 0.458 | 37.6 | |||
| BBRC0009 | 74 | 75 | 0.03 | 0.484 | 60.3 | |||
| BBRC0009 | 75 | 76 | 0.045 | 0.337 | 25.1 | |||
| BBRC0009 | 76 | 77 | 0.012 | 0.0906 | 24.6 | |||
| BBRC0009 | 77 | 78 | 0.039 | 0.0946 | 13.5 | |||
| BBRC0009 | 78 | 79 | 0.036 | 0.0438 | 7.8 | |||
| BBRC0009 | 79 | 80 | 0.001 | 0.0256 | 6.2 | |||
| BBRC0010 | 448380 | 7827082 | 325 | 76 | 77 | 0.001 | 0.0166 | 2.5 |
| BBRC0010 | 77 | 78 | 3.56 | 0.218 | 761 | |||
| BBRC0010 | 78 | 79 | 3.52 | 0.286 | 462 | |||
| BBRC0010 | 79 | 80 | 0.571 | 0.753 | 278 | |||
| BBRC0010 | 80 | 81 | 0.502 | 0.465 | 158 | |||
| BBRC0010 | 81 | 82 | 0.982 | 0.451 | 204 | |||
| BBRC0010 | 82 | 83 | 0.319 | 0.332 | 93.9 | |||
| BBRC0010 | 83 | 84 | 0.337 | 0.333 | 58.6 | |||
| BBRC0010 | 84 | 85 | 0.224 | 0.679 | 61.5 | |||
| BBRC0010 | 85 | 86 | 0.313 | 1.2 | 145 | |||
| BBRC0010 | 86 | 87 | 0.056 | 0.136 | 279 | |||
| BBRC0010 | 87 | 88 | 0.427 | 2.67 | 648 |
17
==> picture [364 x 63] intentionally omitted <==
| BBRC0010 | 88 | 89 | 0.046 | 0.129 | 14.1 | |||
|---|---|---|---|---|---|---|---|---|
| BBRC0010 | 89 | 90 | 0.042 | 0.14 | 14.6 | |||
| BBRC0010 | 90 | 91 | 0.04 | 0.117 | 17 | |||
| BBRC0010 | 91 | 92 | 0.011 | 0.0926 | 3.6 | |||
| BBRC0010 | 92 | 93 | 0.01 | 0.0232 | 3.6 | |||
| BBRC0010 | 93 | 94 | 0.022 | 0.0148 | 8 | |||
| BBRC0010 | 94 | 95 | 0.017 | 0.0034 | 4.8 | |||
| BBRC0010 | 95 | 96 | 0.116 | 0.018 | 27.6 | |||
| BBRC0011 | 448380 | 7827009 | 325 | 163 | 164 | 0.002 | 0.004 | 3.2 |
| BBRC0011 | 164 | 165 | BDL | 0.0058 | 4.1 | |||
| BBRC0011 | 165 | 166 | BDL | 0.006 | 4.7 | |||
| BBRC0011 | 166 | 167 | 0.011 | 0.0086 | 7 | |||
| BBRC0011 | 167 | 168 | 0.087 | 2.09 | 528 | |||
| BBRC0011 | 168 | 169 | 0.05 | 0.316 | 492 | |||
| BBRC0011 | 169 | 170 | 0.035 | 0.0544 | 21.9 | |||
| BBRC0011 | 170 | 171 | 0.008 | 0.0262 | 16.1 | |||
| BBRC0011 | 171 | 172 | 0.033 | 0.0174 | 16.9 | |||
| BBRC0011 | 192 | 193 | 0.004 | 0.052 | 40.9 | |||
| BBRC0011 | 193 | 194 | 0.004 | 0.099 | 15.1 | |||
| BBRC0011 | 194 | 195 | 0.004 | 0.063 | 19.8 | |||
| BBRC0011 | 195 | 196 | BDL | 0.0274 | 12.5 | |||
| BBRC0011 | 196 | 197 | 0.001 | 0.012 | 7.1 | |||
| BBRC0011 | 197 | 198 | 0.007 | 0.0254 | 5.5 | |||
| BBRC0011 | 198 | 199 | 0.014 | 0.07 | 12.4 | |||
| BBRC0011 | 199 | 200 | 0.011 | 0.126 | 26.3 | |||
| BBRC0011 | 200 | 201 | 0.051 | 0.186 | 42.1 | |||
| BBRC0011 | 201 | 202 | 0.117 | 0.117 | 255 | |||
| BBRC0011 | 202 | 203 | 0.089 | 0.21 | 338 | |||
| BBRC0011 | 203 | 204 | 0.024 | 0.0334 | 179 | |||
| BBRC0011 | 204 | 205 | 0.006 | 0.161 | 100 | |||
| BBRC0011 | 205 | 206 | 0.014 | 0.118 | 81.6 | |||
| BBRC0011 | 206 | 207 | 0.073 | 0.449 | 104 | |||
| BBRC0011 | 207 | 208 | 0.051 | 0.121 | 61.9 | |||
| BBRC0011 | 208 | 209 | 0.118 | 0.491 | 40 | |||
| BBRC0011 | 209 | 210 | 0.021 | 0.113 | 14.4 | |||
| BBRC0011 | 210 | 211 | 0.01 | 0.115 | 24.4 | |||
| BBRC0011 | 211 | 212 | 0.007 | 0.0584 | 18.2 | |||
| BBRC0012 | 448380 | 7827082 | 325 | 107 | 108 | BDL | 0.0056 | 1.4 |
| BBRC0012 | 108 | 109 | BDL | 0.0026 | 1.7 | |||
| BBRC0012 | 109 | 110 | BDL | 0.004 | 2.5 | |||
| BBRC0012 | 110 | 111 | 0.001 | 0.0172 | 3.5 | |||
| BBRC0012 | 111 | 112 | BDL | 0.0176 | 7.6 | |||
| BBRC0012 | 112 | 113 | 0.003 | 0.029 | 8 | |||
| BBRC0012 | 113 | 114 | 0.001 | 0.0188 | 9.8 |
18
==> picture [364 x 63] intentionally omitted <==
| BBRC0012 | 114 | 115 | 0.002 | 0.0178 | 14.2 | |||
|---|---|---|---|---|---|---|---|---|
| BBRC0012 | 115 | 116 | 0.002 | 0.0588 | 11.7 | |||
| BBRC0012 | 116 | 117 | 0.159 | 0.401 | 959 | |||
| BBRC0012 | 117 | 118 | 0.149 | 1.69 | 218 | |||
| BBRC0012 | 118 | 119 | 0.096 | 0.856 | 167 | |||
| BBRC0012 | 119 | 120 | 0.007 | 0.104 | 14.2 | |||
| BBRC0012 | 120 | 121 | 0.055 | 0.362 | 781 | |||
| BBRC0012 | 121 | 122 | 0.096 | 0.663 | 912 | |||
| BBRC0012 | 122 | 123 | 0.229 | 1.52 | 1350 | |||
| BBRC0012 | 123 | 124 | 0.147 | 1.09 | 1010 | |||
| BBRC0012 | 124 | 125 | 0.049 | 0.62 | 130 | |||
| BBRC0012 | 125 | 126 | 0.224 | 5.84 | 381 | |||
| BBRC0012 | 126 | 127 | 0.054 | 3.11 | 62.3 | |||
| BBRC0012 | 127 | 128 | 0.091 | 6.2 | 182 | |||
| BBRC0012 | 128 | 129 | 0.649 | 11.1 | 515 | |||
| BBRC0012 | 129 | 130 | 0.381 | 3.7 | 246 | |||
| BBRC0012 | 130 | 131 | 0.341 | 3.19 | 261 | |||
| BBRC0012 | 131 | 132 | 0.216 | 2.01 | 181 | |||
| BBRC0012 | 132 | 133 | 0.086 | 0.919 | 75.9 | |||
| BBRC0012 | 133 | 134 | 0.215 | 2.36 | 49.3 | |||
| BBRC0012 | 134 | 135 | 0.241 | 7.92 | 123 | |||
| BBRC0012 | 135 | 136 | 0.073 | 1.79 | 87.2 | |||
| BBRC0012 | 136 | 137 | 0.193 | 4.77 | 302 | |||
| BBRC0012 | 137 | 138 | 0.03 | 1.05 | 82.4 | |||
| BBRC0012 | 138 | 139 | 0.005 | 0.169 | 46.3 | |||
| BBRC0012 | 139 | 140 | 0.005 | 0.114 | 37.1 | |||
| BBRC0012 | 140 | 141 | 0.058 | 0.743 | 31.7 | |||
| BBRC0012 | 141 | 142 | 0.025 | 0.201 | 43.5 | |||
| BBRC0012 | 142 | 143 | 1.44 | 11.5 | 383 | |||
| BBRC0012 | 143 | 144 | 0.669 | 1.51 | 230 | |||
| BBRC0012 | 144 | 145 | 0.405 | 0.867 | 168 | |||
| BBRC0012 | 145 | 146 | 0.085 | 0.38 | 113 | |||
| BBRC0012 | 146 | 147 | 0.037 | 0.226 | 104 | |||
| BBRC0012 | 147 | 148 | 0.037 | 0.199 | 81.8 | |||
| BBRC0012 | 148 | 149 | 0.011 | 0.063 | 46.3 | |||
| BBRC0013 | 448360 | 7827040 | 325 | 124 | 125 | 0.13 | 2.38 | 348 |
| BBRC0013 | 125 | 126 | 0.047 | 2.7 | 178 | |||
| BBRC0013 | 126 | 127 | 0.021 | 0.958 | 52.6 | |||
| BBRC0013 | 127 | 128 | 0.023 | 0.473 | 27.6 | |||
| BBRC0013 | 128 | 129 | 0.033 | 1.07 | 23 | |||
| BBRC0013 | 129 | 130 | 0.044 | 1.08 | 18.5 | |||
| BBRC0013 | 130 | 131 | 0.006 | 0.111 | 3.7 | |||
| BBRC0013 | 131 | 132 | 0.008 | 0.175 | 3.4 | |||
| BBRC0013 | 132 | 133 | 0.018 | 0.273 | 9 |
19
==> picture [364 x 63] intentionally omitted <==
| BBRC0013 | 133 | 134 | 0.003 | 0.0604 | 4.8 | |||
|---|---|---|---|---|---|---|---|---|
| BBRC0013 | 134 | 135 | 0.006 | 0.0588 | 6.8 | |||
| BBRC0013 | 135 | 136 | 0.002 | 0.0304 | 5.8 | |||
| BBRC0013 | 136 | 137 | 0.001 | 0.0234 | 7.6 | |||
| BBRC0013 | 137 | 138 | BDL | 0.0244 | 10.1 | |||
| BBRC0013 | 138 | 139 | BDL | 0.013 | 5.8 | |||
| BBRC0013 | 139 | 140 | 0.021 | 0.0114 | 11.3 | |||
| BBRC0013 | 140 | 141 | 0.559 | 0.025 | 609 | |||
| BBRC0013 | 141 | 142 | 0.017 | 0.0064 | 18.8 | |||
| BBRC0013 | 142 | 143 | 0.004 | 0.0092 | 9.8 | |||
| BBRC0013 | 143 | 144 | 0.012 | 0.137 | 16.2 | |||
| BBRC0013 | 144 | 145 | 0.005 | 0.114 | 7.9 | |||
| BBRC0013 | 145 | 146 | 0.028 | 0.371 | 21.1 | |||
| BBRC0013 | 146 | 147 | 0.034 | 0.747 | 56.4 | |||
| BBRC0013 | 147 | 148 | 0.003 | 0.0598 | 8.4 | |||
| BBRC0013 | 148 | 149 | 0.005 | 0.0666 | 24 | |||
| BBRC0013 | 149 | 150 | BDL | 0.0316 | 2.5 | |||
| BBRC0013 | 150 | 151 | 0.001 | 0.0348 | 4.1 | |||
| BBRC0013 | 151 | 152 | 0.03 | 0.463 | 142 | |||
| BBRC0013 | 152 | 153 | 0.004 | 0.171 | 22.5 | |||
| BBRC0013 | 153 | 154 | 0.069 | 0.0408 | 100 | |||
| BBRC0013 | 154 | 155 | 0.022 | 0.21 | 91.5 | |||
| BBRC0013 | 155 | 156 | 0.005 | 0.0934 | 69.5 | |||
| BBRC0013 | 156 | 157 | 0.014 | 0.123 | 26.7 | |||
| BBRC0013 | 157 | 158 | 0.012 | 0.0562 | 24.1 | |||
| BBRC0013 | 158 | 159 | 0.005 | 0.0592 | 20.8 | |||
| BBRC0013 | 159 | 160 | 0.004 | 0.105 | 15 | |||
| BBRC0013 | 160 | 161 | 0.013 | 0.165 | 11.3 | |||
| BBRC0013 | 161 | 162 | 0.128 | 0.345 | 13.7 | |||
| BBRC0013 | 162 | 163 | 0.896 | 0.546 | 32.9 | |||
| BBRC0013 | 163 | 164 | 0.974 | 1.64 | 51.4 | |||
| BBRC0013 | 164 | 165 | 1.57 | 1.46 | 102 | |||
| BBRC0013 | 165 | 166 | 0.15 | 0.416 | 37.5 | |||
| BBRC0013 | 166 | 167 | 0.784 | 3.91 | 231 | |||
| BBRC0013 | 167 | 168 | 0.261 | 1.24 | 183 | |||
| BBRC0013 | 168 | 169 | 0.442 | 1.59 | 961 | |||
| BBRC0013 | 169 | 170 | 0.248 | 1.75 | 505 | |||
| BBRC0013 | 170 | 171 | 0.177 | 0.932 | 401 | |||
| BBRC0013 | 171 | 172 | 0.508 | 1.76 | 500 | |||
| BBRC0013 | 172 | 173 | 0.186 | 0.669 | 212 | |||
| BBRC0013 | 173 | 174 | 0.33 | 0.943 | 269 | |||
| BBRC0013 | 174 | 175 | 0.672 | 0.695 | 221 | |||
| BBRC0013 | 175 | 176 | 0.352 | 0.777 | 221 | |||
| BBRC0013 | 176 | 177 | 0.03 | 0.324 | 24.6 |
20
==> picture [364 x 63] intentionally omitted <==
| BBRC0013 | 177 | 178 | 0.039 | 0.397 | 41.4 | |||
|---|---|---|---|---|---|---|---|---|
| BBRC0013 | 178 | 179 | 0.038 | 0.283 | 41 |
21