REDBANK COPPER LIMITED NORTHERN TERRITORY

REDBANK COPPER LIMITED

NORTHERN TERRITORY

ELR94 ANNUAL EXPLORATION REPORT ENDING 9TH AUGUST 2012

TO

THE NORTHERN TERRITORY

DEPARTMENT OF PRIMARY INDUSTRY FISHERIES AND MINES

Authors: John Ceplecha 23rd September, 2012 Redbank Copper Limited A.C.N. 059 326 519 Level 1, 141 Hay Street Subiaco WA 6008

Phone: +61 8 6389 6400 Fax: +61 8 6389 6410 Email: [email protected]

mailto:[email protected]

(i)

Title Page

Titles/Tenements ELR 94 Titleholder/Operator Redbank Mine Operations Pty Ltd Tenement Manager M&M Consulting, PO Box 8197 Subiaco WA 6008 (08938158660 Grant Date 10th August 1989 Area 1905 Ha Report Title ELR 94 Annual Exploration Report Ending 9th August 2011 Date of Report / Status 23rd September 2012, Year 23 Personal Authors J Ceplecha Corporate Authors Redbank Copper Limited Target Commodities Cu, Pb, Zn, Au, Ag, Co, Mn, Diamonds Project Name Redbank Datum/Zone GDA94, Zone 53

250,000 sheet Calvert Hills 100,000 sheet Woologorang Expenditure Commit. $800,000 Contact Details S. Fleming

Postal Level 1, 143 Hay Street, Subiaco, Perth WA 6008 Fax 618 63896410 Phone 618 63896400

Email (Technical Data) [email protected] Email (Expenditure) [email protected]

Executive Summary

ELR94 is a granted lease within the Redbank Copper operational area in the Northern Territory, and currently is in its twenty third year of tenure. During the reporting period, the company completed a small RC drilling programme across Charlie prospect within the lease, successfully intersecting copper mineralisation. Proposed drilling of Double Bluff and Quartzite prospects was curtailed due to late drilling start and adverse weather. The purpose of the 2011 RC drilling was to identify any sulphide mineralisation beneath previously identified copper oxide ore, and to add to the copper metal inventory within ERL 94.



CONTENTS

(i) Title Page, Executive Summary

1.0 BACKGROUND - REDBANK COPPER OPERATIONS

2.0 REGIONAL GEOLOGICAL SETTING

3.0 TENEMENT GEOLOGY

4.0 EXPLORATION MODEL

5.0 PREVIOUS EXPLORATION

6.0 EXPLORATION FOR THE PERIOD 10th August 2011 TO 9th August, 2012

6.1 Geophysics 6.2 Drilling

7.0 PROPOSED EXPLORATION FOR THE NEXT 12 MONTHS

FIGURE LIST

Figure 1 Location and regional setting of Redbank Copper Limited Figure 2 Redbank Infrastructure on ELR94, July 2011 Figure 3 Location of ELR94 and Tenement Holding of Redbank Copper Limited Figure 4 Redbank Prospect locations Figure 5 ELR94‐ Ionic Soil geochemistry to date – Copper Values

TABLE 1: Summary of significant copper (CU XRF > 1.0%) Drill Hole intercepts on ELR94, for 2011‐2012 reporting period.

1.0 BACKGROUND - REDBANK COPPER OPERATIONS

The Redbank Copper Mine is located in the north‐east of the Northern Territory a pproximately 30 km from the Queensland border and 70 km from the coast of the Gulf of Carpentaria. It strad dles the Savannah Way which connects the townships of Borroloola in the Northern Territory and Burketown in Que ensland. It is around 1,200 km south east of Darwin by sealed and unsealed road.

Figure 1: Location and regional setting of Redbank Copper Limited

The Redbank Copper field was discovered in 1916 and small scale mining was carriied out until the early 1960’s. Subsequently exploration was carried out during the late 1960’s through to the 1990’s by various groups, culminating in larger scale mining operations being undertaken in the mid 1990’s when the Sandy Flat open pit was developed to supply oxide/sulphide ore to a 250,000 tpa flotation plant built on site. Some very hig h grade (>25% copper) ore was also direct shipped at this time. The operation ceased after less than 2 years because of declining copper prices. With the exception of the mill, the flotation plant and crushing circuit remain on site. Both a re in reasonable condition and are planned to be refurbished to operating condition with a redevelopment of the Proj ect.

The most recent processing was a copper leaching operation that began producing o n an intermittent basis in 2004 and utilised oxide ore that had been stockpiled during the previous mining. The curr ent owners have operated the site since 2005 and some of the remaining ore stockpiles from the previous mining ve nture in the 1990’s have been processed.

In 2009, with new funding and management arrangements, Redbank undertook the fol lowing:

• Placed the site on care and maintenance and embarked on a program to impr ove environmental compliance, in particular to remedy discharges of contaminated water from the site.

• Carried out a review of the project to determine the future direction of its development, and generate a mine study outlining the path to redevelopment.

• Embarked on a well‐funded exploration program that aims to discover new resources and to upgrade the status of the existing resources.

The study undertaken by Redbank examined options for future development of the p roject. Redbank identified that the future of the project is primarily in processing sulphide copper ores, which co mprise more than 86% of the current resources, to make quality copper concentrates. In addition copper cathode can be made from the oxide ores. Further work is required to establish additional resources and better define operating parameters. In May 2011 the total resource was estimated by SRK Consultants as 6,268,000 tonnes at a gra de of 1.53% copper containing 96,500 tonnes of copper metal.

Figure 2: Redbank Infrastructure on ELR94, July 2011

The operational area consists of an Exploration Retention License (ELR94) and seven Mineral Leases (ML631, ML632, ML633, ML634, ML635, ML636 and ML1108) contained within the ELR. The comp any has recently applied for a Mining Lease (MLA27385) to replace ELR94 ahead of a decision to mine in 2012. Red bank Mine Operations Pty Ltd, the holder of ELR94, also has a number of exploration interests within the vicinity of the existing Redbank Mine site (EL24654, EL26758, EL26778, EL26779, EL26780, EL26781, EL26965, EL26999, EL2724 0, EL27241, EL27329, EL27737, ELA28003, EL28288, EL28289, EL28290 and ELA28024). In addition the company has r ecently applied for a tenement contiguous with the land holding over the Queensland border, EPMA18553. These a re located mostly to the north and west of the mine site as shown below in Figure 3.

2.0 REGIONAL GEOLOGICAL SETTING

Regionally the Redbank copper deposits lie within the Proterozoic sequences of th e MacArthur River Basin (see Figure 1). The basin hosts a number of world class base metal deposits. The Redbank c opper mineralisation is hosted by the Lower Proterozoic Gold Creek Volcanics, a sequence of predominantly interm ediate sub volcanic intrusions, extrusions, breccia pipes, and intercalated sediments. The copper mineralisation identified to date has been principally interpreted as being contained in volcanic breccia pipes, of which 30 to 50 have been recognised by various explorers. Only a minority of the breccia pipes are mineralised and only som e of those contain potentially economic concentrations of copper.

The Packsaddle Microgranites locally intrude the Gold Creek Volcanics and are presen t close to the known Redbank copper deposits. Gold Creek Volcanics are present in a significant portion of the region al tenements. Further east the Gold Creek Volcanics are obscured beneath surficial Cainozoic sequences. The Hob blechain Rhyolite, a member of the Masterton Formation overlies the Gold Creek volcanics to the west.

E

ELR94

Figure 3: Location of ELR94 and Tenement Holding of Redbank Copper Limited 3.0 TENEMENT GEOLOGY

The Redbank Mining Centre contains 23 breccia “pipes” or diatremes and shear zon es/veins most of which contain copper mineralization. These structures are mainly hosted by the Hobblechain Rhy olite, the Gold Creek Volcanics and the Wollogorang Formation; however, diatremes have also been recorded in the S ettlement Creek Volcanics and the Seigal Volcanics. Host rocks are brecciated and altered passing out into less alter ed shallow‐dipping host rocks. The volcanic breccias from the Redbank Mining centre appear to be located with in an east‐trending structural corridor although mineralized breccia veins are aligned north‐east with a steep nort herly plunge to the shoots. A conjugate fault system with dextral movement would tend to produce dilation zones alligned along an easterly trend.

The localizing structures are probably faults or fault intersections plunging thro ugh the Tawallah Group into basement containing granite. The copper deposits occur in clusters, exceed 300 m in d epth and have near circular to irregular outlines from 50 m to 150 m across.

Primary mineralization consists of disseminations and veins with chalcopyrite and bornite in breccia. Gangue minerals are dolomite, barite, chlorite, potassium‐feldspar, quartz, pyrite, hematite, a patite and pyrobitumen. Clasts of overlying units are evidence for collapse during breccia formation. In the oxide zo ne from surface to 30 m depth, grades approach 6% copper, the main minerals being malachite, azurite, chalcocite an d chrysocolla.

Breccia and wall rocks are associated with intense potassic alteration consisting off carbonate‐chlorite‐potassium feldspar‐quartz, pyrite, hematite and pyrobitumen.

Past production was 19 600 tonnes grading 5% copper and currently indicated resour ces from two deposits are 2.0 million tonnes grading 1.66% copper at Bluff, and 1.5 million tonnes grading 2% copper at Sandy Flat.

The presence of pyrobitumen of organic origin precludes a purely volcanic origin for the breccia and may support a low pressure, low temperature epithermal source. Several theories have been advanced to explain the origin of the diatremes which are produced by over‐pressured fluids. There is no direct evidence for magmatic fluids and the fluids might be produced by mixing of sulphate and copper‐rich basinal brines, derived from above and lateral to the deposits, with rising, reduced, hydrocarbon‐bearing fluid sourced in the underlying Wollogorang Formation. The significance of a conceptual model based on the mixing of reduced and oxidized fluids is that it increases the potential of the area for more extensive copper deposits in a structural setting that permits oxidized brines to mix with reduced fluids from other formations in the Tawallah Group.

4.0 EXPLORATION MODELS

The consensus of most of the modern era (post‐1970) explorers in the Redbank area is that the mineralisation is contained in the approximately circular volcanic breccia pipes as the result of fluid circulation in the breccia. The breccia pipes development has also been interpreted as involving largely autochthonous brecciation of the trachyandesite host rock, with little displacement.

There have been some suggestion that there has been post volcanic slumping in some pipes causing minor (<10m) vertical displacement of sediments overlying the Gold Creek volcanics into the pipes. Minor normal faults and jointing have been interpreted as exerting a control on the location and form of the pipes. A peculiarity of the more comprehensively mineralised pipes is the association of the mineralisation with pyrobitumen. The origin of the pyrobitumen has been variously speculated as resulting from intense reduction of carbonate to a high temperature derivative of an organic precursor.

RC and diamond core drilling by Redbank on deposits in the area during 2006 to 2009, has indicated that the mineralisation does not display all the characteristics that could be expected solely from the circulation of mineralised fluids through the prepared breccia pathways. While there are clearly veins of sulphidic copper mineralisation contained within the breccia they are typically fragmented. Also much of the primary mineralisation consists of chalcopyrite and chalcocite grains disseminated through the host trachyandesite. The oxide mineralisation retains the characteristics of the primary mineralisation structures and fabrics with cuprite largely replacing the disseminated chalcocite and chalcopyrite, with a minor amount of azurite and malachite vein formation following ground water migration along open weathering fractures.

More detailed studies of petrogenesis and ore formation are planned but the initial indications are that there may be a precursor disseminated style of mineralisation emplaced in the breccia pipes. The source of the precursor mineralisation could represent a major target for large scale disseminated copper mineralisation. As a corollary exploration should not only focus on finding mineralised breccia pipes but should also be trying to discover the source of the precursor disseminated mineralisation which has the potential to be a much larger target.

Conceptually, the possibility exists for ‘Manto’ style stratabound deposits forming at depth below the limit of breccia formation, as a primary mineralisation focus over structural décollements from fluid travelling laterally from major through‐going lineaments, such as the Calvert Hills fault to the south west of the ELR94.

Packsaddle Microgranite (or rhyolitic) intrusions occur in close association with the Redbank copper Mineralisation. It is not yet apparent if there is any paragenetic significance in this spatial association. The Packsaddle Microgranites have interpreted as associated with a regional 1,725Ma felsic intrusive event in the Macarthur River Basin (Page et al, 2000).

5.0 PREVIOUS EXPLORATION ON REGIONAL TENEMENTS

Review of the available historic data for the region indicated that it was disjointed and compilation into a modern GIS system was required. Principal explorers were Carpentaria, Rio Tinto, and then later CRA, mainly exploring for base metals, uranium and diamonds in the general area. Several generations of work starting in the 1960’s can be grouped according to commodity as follows:

(i) 1956 to 1960 – predominantly uranium exploration, (ii) 1965 to 1971 – mainly uranium plus focus on copper, particularly at Redbank, (iii) 1978 to present – uranium, diamonds, gold and base metal, manganese and industrial minerals

(phosphates)

Previous exploration on ELR94 has focussed on copper mineralisation analogous to the historical workings at Redbank and Azurite. This has been comprehensively summarised in Redbank Mines (2005) containing a report prepared by the independent geologists SRK Consulting Pty Ltd. The SRK conclusions on previous exploration and the exploration potential of ELR94 are summarised below.

Previous exploration at Redbank has been sporadic, with a concentration on the known style of relatively small but high grade breccia pipes. Potential targets were identified by the NEWAIM programme in 1971 by assuming the breccia pipes had a surface expression of shallow depressions; the only significant discovery since then was Punchbowl, identified by a similar criterion as the NEWAIM discoveries.

Soil sampling over ELR94 has been carried out in a piecemeal fashion over restricted areas. This data shows that the resources such as Bluff and targets such as Quartzite and Roman Nose are defined by about 120ppm Cu in soil samples; using this criterion, five soil anomalies have been identified that lack any drilling. These are prospective for further breccia pipe style mineralisation.

Analysis of the more recent magnetic data acquired by CRAE allows an interpretation of the underlying structural framework of ELR94. The ESE‐WNW trending structures that host the breccia pipes (Redbank and Masterton Trends) are clearly visible; additionally, a possible parallel structure that hosts Sandy Flat and numerous NNE‐SSW trending structures are evident. The intersection of the ESE‐WNW and NNE‐SSW trending structure may control the location of the breccia pipes.

In the immediate area of the Redbank mine, these structures are expressed by the drainage patterns. An interpretation of the underlying magnetic data and the drainage highlights 10 targets that are currently unexplored, two of which are on ELR94. The poor resolution of the magnetic data for the western half of ELR94 precludes the identification of further magnetic trends except by assuming the correlation between drainage patterns and the underlying geological structure.

Basin‐wide strata with elevated copper levels in the Wollogorang Formation have been noted by Plumb et al. (1990), as well as anomalous copper in the underlying Siegel Volcanics. There is potential that there may be economic concentrations in large tonnage, low grade stratabound orebodies, although previous exploration programmes have not investigated this.

In 2008 a soil geochemistry program was undertaken to complete coverage of the tenement on a nominal 100 by 50m pattern. A total of 1,702 samples were collected and analysed for a suite of elements including copper. Old workings at Redbank, Azurite and Prince were clearly expressed with copper in excess of 500ppm, and likely enhanced by dust dispersion from the old mining activities. The Bluff deposit was also prominent because of mineralisation exposed at the surface. The soil geochemistry for the Sandy Flat deposit was collected before the deposit was identified and mined, and is identifiable by a number of peak soil values of between 300 and 400ppm copper.

Background levels of copper in the host rocks were less than 75ppm, and above 200ppm is considered to be a

significant anomaly. A series of 5 soil geochemistry anomalies numbered An1 to 5 in were previously defined by CRAE (CRA Ltd) in 1995, and the 2008 program defined a further 16 anomalies of equivalent or higher rank (Figure 4 ‐ An6 to An21). The 21 copper soil anomalies thus defined do not necessarily represent copper mineralised breccia pipes, but a number clearly have values and dimensions that are consistent with the known pipe signatures.

Commencing in April 2009, a comprehensive exploration effort was commenced by Redbank, including:

• compilation to digital formats of all historic media, • validation of all drill data, including data entry of geology • confirmatory field mapping • establish AHD survey control over the lease • capture of high resolution orthophoto and generation of DTM • close‐spaced small loop TEM survey of Redbank‐Bluff corridor • complete coverage of lease with gravity survey at minimum 200 x 200m, with infill • partial coverage of the lease with close‐spaced ground magnetics and radiometrics.

In addition, RC Drilling of advanced targets on the ELR commenced in July 2009, with immediate success at the Punchbowl deposit, where ten holes were drilled and significant copper intersections were received, increasing with grade at depth. Significant copper intersections were also delivered at depth from RC drilling of the Quartzite deposit, where five holes were drilled. Three holes were drilled at two bullseye targets generated by the TEM survey near the Prince deposit, but encountered no copper mineralisation. The tenement package included numerous advanced copper targets and has an identified JORC resource of 6.268 million tonnes at a grade of 1.53% copper of which 2.766Mt at 1.55%Cu are Indicated Resources and 3.502Mt at 1.52% Cu are Inferred Resources.

Double

6.0 EXPLORATION FOR THE PERIOD 10th August 2011 TO 9th August, 2012

Work undertaken within ELR 94 during the period consisted of a review of past EM s urveys and RC drilling of oxide and sulphide zones, and determine if results are indicative of potentially significant sullphide mineralisation at depth. Past exploratory drilling has discovered new sulphide breccia beneath oxide at Doub le Bluff, Quartzite and Charlie, and will require further drilling to achieve JORC Indicated Resource category.

Charlie is interpreted as a vein plus breccia system. Charlie is a highly ranked target on the basis of historical activity, geological setting, and anomalous percussion drilling and ionic geochemical response. During November 2011, eight holes for 717m were completed at Charlie. Drilling encountered a structurally‐controll ed mineralised system, appearing to be steep and relatively high angle (NNE‐SSW) to the interpreted E‐W fault zone. 11BCRC‐06 reported 13m @ 1.37% Cu XRF from 9m, and 4m @ 1.2% Cu XRF from 36m (Table 1).

Past drilling at Quartzite (QT1, QT3) indicated sulphide ore at depth. Best assay result returned was 52m @ 1.34% Cu from 119m, which included 8m @ 3.98% Cu from 163m. 2011 field mapping indica tes that the mineralisation remains open to the west and northwest and requires detailed drilling to bring Quartz ite into the Indicated category. Track and drill pads were prepared during 2011, however, early wet season rains curta iled further drilling activity.

Double Bluff is a low grade copper pipe, with a sulphide target open at depth. Double Bluff was highly ranked on the basis of look‐alike targets, with a characteristic gravity low, magnetic low and geoche mically high signature identical to Bluff. During 2010, initial drilling defined an open large low‐grade copper oxide env elope ‐ >0.2% Cu, encountered in most holes (e.g. HoleDBRC10‐04: 35m @ 0.2% from 23m). Low grade sulp hide mineralisation was also encountered at the base of some holes, and a moderately‐ranked sulphide target rem ains at depth. In late 2011, tracks and drill pads were prepared for infill drilling on the 2010 drilling programme to determine the Indicated Resource status of the Double Bluff breccia pipe. Additional drilling was pl anned to determine if there is continuity of mineralisation between the Bluff and Double Bluff breccia pipes. As with the Quartzite drilling programme, inclement weather prevented further drilling at Double Bluff.

Bluff

Figure 4. Redbank Prospect Locations.

C C C C C C C C C

C

N L %

6.1 Geochemical Surveys.

Figure 4: Ionic soil geochemistry to date‐ ELR94‐ Copper values

The re‐focus on exploration has been due to the identification of subtle copper anom alism associated with the newly‐named “Double Bluff” target, which has historically been dismissed as a ‘bleed ’ feature from Bluff itself. However the centre of the new anomalism is some 250m east of Bluff, over a hill and within a setting typical of other pipes, The Company considers the possibility of deeper copper sulphide minera lization, and more buried or sub cropping breccia pipes adjacent to known copper breccias such as Bluff ‐ Doubl e Bluff, Quartzite and AN9 ‐ AN9 Extended as high.

6.2 Geophysics No geophysical surveys were conducted over ELR94 during the reporting perio d.

6.3 Drilling

A limited RC drill programme, targeting sulphide

mineralisation beneat h known copper oxide

mineralisation, was conducted over a number of prospects within ELR 94, and commenced on the 11th

November 2011. Significant results from that drilling programme are detailed below (Table 1). Eight RC holes were drilled for a total advance of 717m.

TABLE 1: Summary of significant copper (CU XRF > 1.0%) Drill Hole intercepts on ELR94, for 2011‐2012 reporting period.

Hole ID

orthing

RL

Dip

Azi

EOH

From

To

Cu‐XRF: Copper Intercept > 1.0 Easting

11BCRC‐01 794896 8096310 21 9 ‐60 180 90 ‐ 11BCRC‐02 794900 8096359 21 9 ‐60 180 96 ‐ 11BCRC‐03 794900 8096335 21 9 ‐60 180 102 27 28 1.31 11BCRC‐04 794950 8096307 21 9 ‐60 180 103 24 25 1.57 11BCRC‐05 795001 8096354 21 9 ‐60 0 97 ‐ 11BCRC‐06 794919 8096291 21 9 ‐60 0 121 4 5 1.16 11BCRC‐06 794919 8096291 21 9 ‐60 0 121 9 22 1.37 11BCRC‐06 794919 8096291 21 9 ‐60 0 121 36 40 1.2 11BCRC‐07 794949 8096358 21 9 ‐60 0 100 ‐ 11BCRC‐08 794965 8096289 21 9 ‐60 0 8 ‐

7.0 PROPOSED EXPLORATION FOR NEXT 12 MONTHS

The company currently intends to continue drilling known copper breccia pipes, for oxide and sulphide potential, to increase the Company’s copper resource inventory. This will involve testing both outcropping and shallow‐covered targets for around 4000m of sulphide resource drilling, with the focus being on a HeliTEM survey to help delineate subtle sulphide targets at depth.

It is expected that expenditure on ELR94 (currently under application for a Mining Lease‐ ML27385) for the next field season will be in the order of $200,000.

REFERENCES

Ahmad M and Wygralak AS (1989) Calvert Hills, Northern Territory. 1:250 000 metallogenic map series explanatory notes SE 53‐08. Northern Territory Geological Survey, Darwin

Orth K, 2010. Geology, vulcanology and mineral potential of the Cliffdale and Seigal volcanics, Calvert Hills 1:250 000 geological mapsheet, SE 53‐08, Northern Territory Geological Survey, Record 2010‐003.

Page R. W., Jackson M. J., Krassay A. A. (2000) Constraining sequence stratigraphy in north Australian basins: SHRIMP U‐Pb zircon geochronology between Mt Isa and McArthur River. Australian Journal of Earth Sciences 47 (3), 431–459.

Appendix 1

Drilling Logs for Charlie Prospect (11BCRC‐01 to 11BCRC‐08).

From To Bag No STRAT LITHO CLR OXID HARD ALT 1 ALT 2 ALT 3 MIN 1 MIN 2 TXT CuXRF GEOLOGISTS NOTES

0 1 11CRC01001 NSR NO SAMPLE RTURN

1 2 11CRC01002 Ptg T-A RD BN 5 5 LA FINE 0.184 MUDSTONE

2 3 11CRC01003 Ptg T-A TN 5 5 LA FINE 0.290 MUDSTONE

3 4 11CRC01004 Ptg T-A TN 5 5 CL FINE 0.146 MUDSTONE


5 6 11CRC01006 Ptg T-A TN 5 4 CL MAL FINE ...093 MUDSTONE








13 14 11CRC01014 Ptg T-A BN 5 4 CL FINE 0.026 MUDSTONE







20 21 BCRC10-023 Ptg T-A BN 5 4 CL FINE 0.026 MUDSTONE

21 22 BCRC10-024 Ptg T-A BN 4 4 CL FINE 0.094 MUDSTONE

22 23 BCRC10-025 Ptg T-A BN 5 5 CL FINE 0.153 CLAYSTONE

23 24 BCRC10-026 Ptg T-A BN 5 5 CL FINE 0.094 CLAYSTONE

24 25 BCRC10-027 Ptg T-A BN 5 5 CL I-OX FINE 0.193 MUDSTONE


26 27 BCRC10-029 Ptg T-A TN 5 4 CL I-OX FINE 0.132 MUDSTONE




30 31 BCRC10-033 Ptg T-A TN 4 3 CL I-OX FINE 0.044 MUDST. WEATHERED VOLCANIC




34 35 BCRC10-037 Ptg T-A TN 4 4 CL I-OX FINE 0.036 MUDSTONE W. TRACE MALACHITE

35 36 BCRC10-038 Ptg T-A GY 4 4 CL FINE 0.030 MUDSTONE AND LITTLE WATER

36 37 BCRC10-039 Ptg T-A GY 4 4 CL FINE 0.033 MUDSTONE







43 44 BCRC10-048 Ptg T-A GY 3 3 CL FINE 0.015 MUDST.- I.E. WEATHERED VOLCANIC ROCK



46 47 BCRC10-051 Ptg T-A GY 1 3 FINE 0.006 VOLCANIC ROCK















61 62 BCRC10-068 Ptg T-A GY 1 3 MAL FINE 0.011 VOLCANIC ROCK - TRACE MALACHITE





66 67 BCRC10-073 Ptg T-A GY 2 3 FINE 0.031 VOLCANIC ROCK - WET

67 68 BCRC10-074 Ptg T-A GY 2 3 FINE 0.012 VOLCANIC ROCK 15/11 - MOIST






















89 90 BCRC10-098 Ptg T-A GY 2 3 FINE 0.015 PROBLEMS

90 91 91 92 92 93 93 94 94 95 95 96 96 97

DRILLING LOG

Start Date: 13-Nov-11 Finish Date: 15-Nov-11 Project: Redbank

Prospect: Black Charlie

Tenement:

ERL94 Hole ID: 11BCRC01

Easting: 794972

Northing: 8096320

RL:

219

Dip: -60 Azimuth: 180 EOH: 90 Geologist: SOM

Contractor: OME DRILLING

Hole Type: RC

Hole Comment:

VOLCANIC ROCK - END OF HOLE - GEOLOGIST DESITION - NO DRILLING

3.5

11BCRC ‐ 01 XRF %Cu

3.0

2.5

2.0

1.5

30 sec

1.0

0.5

0.0

1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 37 39 41 43 45 47 49 51 53 55 57 59 61 63 65 67 69 71 73 75 77 79 81 83 85 87 89 91 93 95 97 99

DRILLING LOG

Start Date: 15-Nov-11 Finish Date: 16/11/2011 to 96m Project:

Redbank

Prospect:

Black Charlie

Tenement:

ERL94 Hole ID:

11BCRC02

Easting:

794935

Northing:

8096323

RL: 206

Dip: -60

Azimuth: 180

EOH: 96m

Geologist:

S. MIKKELSEN

Contractor:

OME DRILLING

Hole Type:

RC

Hole Comment: DEPTH DIP AZIMUTH

SURVEY1 SURVEY2 SURVEY3

From To Bag No STRAT LITHO CLR OXID HARD ALT 1 ALT 2 ALT 3 MIN 1 MIN 2 TXT CuXRF

0 1 BCRC10-001 Ptg T-A GR BN 5 4 I-OX MAL CL F 0.130 1 2 BCRC10-002 Ptg T-A YW BN 5 4 I-OX CL F 0.274 2 3 BCRC10-003 Ptg T-A YW BN 5 4 I-OX CL F 0.288 3 4 BCRC10-004 Ptg T-A BN 5 4 CL FINE 0.093 4 5 BCRC10-005 Ptg T-A BN 5 4 CL FINE 0.042 5 6 BCRC10-006 Ptg T-A BN 5 4 CL FINE 0.091 6 7 BCRC10-007 Ptg T-A TN 4 4 CL FINE 0.048 7 8 BCRC10-008 Ptg T-A TN 4 4 CL FINE 0.021 8 9 BCRC10-009 Ptg T-A TN 4 4 CL FINE 0.030 9 10 BCRC10-010 Ptg T-A TN 4 4 CL FINE 0.005 10 11 BCRC10-011 Ptg T-A TN 4 4 CL FINE 0.020 11 12 BCRC10-012 Ptg T-A TN 4 4 CL FINE 0.053 12 13 BCRC10-013 Ptg T-A TN 4 4 CL FINE 0.160 13 14 BCRC10-014 Ptg T-A TN 4 4 CL FINE 0.155 14 15 BCRC10-015 Ptg T-A TN 4 4 CL FINE 0.025 15 16 BCRC10-016 Ptg T-A TN 4 4 CL FINE 0.006 16 17 BCRC10-017 Ptg T-A TN 4 4 CL FINE 0.008 17 18 BCRC10-018 Ptg T-A TN 4 4 CL FINE 0.041 18 19 BCRC10-019 Ptg T-A TN 4 4 CL FINE 0.077 19 20 BCRC10-020 Ptg T-A TN 4 4 CL FINE 0.054 20 21 BCRC10-021 Ptg T-A TN 4 4 CL FINE 0.059 21 22 BCRC10-022 Ptg T-A TN 4 4 CL FINE 0.121 22 23 BCRC10-023 Ptg T-A TN 4 4 CL FINE 0.100 23 24 BCRC10-024 Ptg T-A TN 4 4 CL FINE 0.071 24 25 BCRC10-025 Ptg T-A TN 4 4 CL FINE 0.186 25 26 BCRC10-026 Ptg T-A TN 4 4 CL FINE 0.044 26 27 BCRC10-027 Ptg T-A TN 4 4 CL FINE 0.075 27 28 BCRC10-028 Ptg T-A TN 4 4 CL FINE 0.045 28 29 BCRC10-029 Ptg T-A TN 4 4 CL FINE 0.094 29 30 BCRC10-030 Ptg T-A TN 4 4 CL FINE 0.081 30 31 BCRC10-031 Ptg T-A TN 4 4 CL FINE 0.118 31 32 BCRC10-032 Ptg T-A TN 4 4 CL FINE 0.113 32 33 BCRC10-033 Ptg T-A TN 4 4 CL FINE 0.137 33 34 BCRC10-034 Ptg T-A TN ODERA 4 CL FINE 0.181 34 35 BCRC10-035 Ptg T-A BL-GY WEAK 3 CHL? FINE 0.027 35 36 BCRC10-036 Ptg T-A BL-GY WEAK 3 FINE 0.081 36 37 BCRC10-037 Ptg T-A BL-GY R M F 0.425 37 38 BCRC10-038 Ptg T-A BL-GY 0.400 38 39 BCRC10-039 Ptg T-A BL-GY 0.558 39 40 BCRC10-040 Ptg T-A BL-GY 0.520 40 41 BCRC10-041 Ptg T-A BL-GY 0.480 41 42 BCRC10-042 Ptg T-A BL-GY 0.321 42 43 BCRC10-043 Ptg T-A BL-GY 0.357 43 44 BCRC10-044 Ptg T-A 0.223 44 45 BCRC10-045 Ptg T-A 0.343 45 46 BCRC10-046 Ptg T-A 0.395 46 47 BCRC10-047 Ptg T-A 0.422 47 48 BCRC10-048 Ptg T-A 0.464 48 49 BCRC2-049 Ptg T-A 0.236 49 50 BCRC2-050 Ptg T-A 0.270 50 51 BCRC2-051 Ptg T-A 0.416 51 52 BCRC2-052 Ptg T-A 0.830 52 53 BCRC2-053 Ptg T-A 0.601 53 54 BCRC2-054 Ptg T-A 0.179 54 55 BCRC2-055 Ptg T-A MAL 0.163 55 56 BCRC2-056 Ptg T-A 0.388 56 57 BCRC2-057 Ptg T-A Bl-GY R S-M CAL CHL? F 0.551 57 58 BCRC2-058 Ptg T-A 0.373 58 59 BCRC2-059 Ptg T-A 0.435 59 60 BCRC2-060 Ptg T-A 0.341 60 61 BCRC2-061 Ptg T-A 0.380 61 62 BCRC2-062 Ptg T-A 0.310 62 63 BCRC2-063 Ptg T-A 0.122 63 64 BCRC2-064 Ptg T-A 0.440 64 65 BCRC2-065 Ptg T-A 0.097 65 66 BCRC2-066 Ptg T-A 0.970 66 67 BCRC2-067 Ptg T-A 0.306 67 68 BCRC2-068 Ptg T-A 0.141 68 69 BCRC2-069 Ptg T-A 0.203 69 70 BCRC2-070 Ptg T-A 0.409 70 71 BCRC2-071 Ptg T-A 0.150 71 72 BCRC2-072 Ptg T-A 0.146 72 73 BCRC2-073 Ptg T-A 0.177 73 74 BCRC2-074 Ptg T-A 0.362 74 75 BCRC2-075 Ptg T-A 0.975 75 76 BCRC2-076 Ptg T-A 0.656 76 77 BCRC2-077 Ptg T-A 0.347

GEOLOGISTS NOTES

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS

WEATHERED VOLCANICS WATER TABLE LEVEL OF PREVIOUS HOLE,REDUCED ROCKS BELOW ?

3.5


3.0

2.5

2.0

1.5

30 sec

1.0

0.5

0.0 1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 37 39 41 43 45 47

DRILLING LOG

CODES LITHO: CLAY=CLY COLOUR: SELF-EXPLANATORY OXID: S=STRONG, M=MODERATE, W=WEAK, R=REDUCED, REDOX=BOTH OXIDISED AND REDUCED PIECES

Start Date:

16-Nov-11

Finish Date:

16-Nov-11

HARDNESS: VH=VERY HARD, H=HARD, M=MODERATELY HARD, S=SOFT, VS=VERY SOFT ALTERATION: CAL=CALCITE, CHL=CHLORITE, QTZ=QUARTZ, LIM=LIMONITE, MINERALIS: MAL=MALACHITE, AZU=AZURITE,

Project: Redbank Prospect: Black Charlie Tenement: ERL94 Hole ID:

11CRC03

Easting:

794908 GDA

Northing:

8096321 RL: 238

Dip: 60

Azimuth: 180 EOH: 102

DRILLER WATER TABLE: NONE BUT REDOX

Geologist:

Antoine

Contractor:

OME Hole Type:

RC

Hole Comment:

SOME CLAY SHORT INTERVALS

DEPTH DIP AZIMUTH SURVEY1 30 60.5 188 SURVEY2 60 64.1 185.2 SURVEY3 90 65.9 151

From To Bag No STRAT LITHO CLR OXID HARD ALT 1 ALT 2 ALT 3 MIN 1 MIN 2 TXT CuXRF

0 1 11CRC03-001 Ptg T-A OG S S F 0.122 1 2 11CRC03-002 Ptg T-A GY-BR M S F 0.123 2 3 11CRC03-003 Ptg T-A GY-BR M S F 0.347 3 4 11CRC03-004 Ptg T-A GY-BR M S F 0.477 4 5 11CRC03-005 Ptg T-A GY-BR M S F 0.402 5 6 11CRC03-006 Ptg T-A GY-BR M S F 0.257 6 7 11CRC03-007 Ptg T-A GY-BR M S F 0.192 7 8 11CRC03-008 Ptg T-A GY-BR M S F 0.156 8 9 11CRC03-009 Ptg T-A GY-BR M S F 0.324 9 10 11CRC03-010 Ptg T-A GY-BR M S F 0.307 10 11 11CRC03-011 Ptg T-A GY-BR M S F 0.221 11 12 11CRC03-012 Ptg T-A BR-GN M S CHL ? MAL? F 0.325 12 13 11CRC03-013 Ptg T-A BR-GN M S CHL ? MAL? F 0.343 13 14 11CRC03-014 Ptg T-A BR-GN M S CHL ? MAL? F 0.448 14 15 11CRC03-015 Ptg T-A BR M S F 0.439 15 16 11CRC03-016 Ptg T-A BR M S F 0.273 16 17 11CRC03-017 Ptg T-A BR M S F 0.182 17 18 11CRC03-018 Ptg T-A BR M S F 0.278 18 19 11CRC03-019 Ptg T-A BR M S F 0.162 19 20 11CRC03-020 Ptg T-A BR M S F 0.335 20 21 11CRC03-021 Ptg T-A BR M S F 0.147 21 22 11CRC03-022 Ptg T-A BR M S F 0.235 22 23 11CRC03-023 Ptg T-A BR M S F 0.230 23 24 11CRC03-024 Ptg T-A BR-OG S S F 0.681 24 25 11CRC03-025 Ptg CLY BR M VS VF 0.406 25 26 11CRC03-026 Ptg CLY BR M VS VF 0.507 26 27 11CRC03-027 Ptg T-A BR-GN ? S MAL F 0.437 27 28 11CRC03-028 Ptg T-A BR-GN ? S MAL F 1.310 28 29 11CRC03-029 Ptg T-A BR-GN ? S MAL F 0.529 29 30 11CRC03-030 Ptg T-A BR M S F 0.202 30 31 11CRC03-031 Ptg T-A BR M S F 0.108 31 32 11CRC03-032 Ptg T-A GY-GN R S CHL ? F 0.183 32 33 11CRC03-033 Ptg T-A GY-GN R S CHL ? F 0.541 33 34 11CRC03-034 Ptg T-A GY-GN R S CHL ? F 0.428 34 35 11CRC03-035 Ptg T-A GY-GN R S CHL ? F 0.207 35 36 11CRC03-036 Ptg T-A GY-OG REDOX S CHL ? F 0.254 36 37 11CRC03-037 Ptg T-A GY-OG REDOX S CHL ? F 0.305 37 38 11CRC03-038 Ptg T-A GY-GN R S-M CHL ? F 0.152 38 39 11CRC03-039 Ptg T-A GY-GN R S-M CHL ? F 0.161 39 40 11CRC03-040 Ptg T-A GY-GN R S-M CHL ? F 0.187 40 41 11CRC03-041 Ptg T-A GY-GN R S-M CHL ? F 0.152 41 42 11CRC03-042 Ptg T-A GY-GN R S-M CHL ? F 0.068 42 43 11CRC03-043 Ptg CLY GY-GN R VS CHL ? VF 0.143 43 44 11CRC03-044 Ptg T-A GY-GN R S CHL ? F 0.046 44 45 11CRC03-045 Ptg T-A GY-GN R S CHL ? F 0.070 45 46 11CRC03-046 Ptg T-A GY-GN R S CHL ? F 0.081 46 47 11CRC03-047 Ptg T-A GY-GN R S CHL ? F 0.239 47 48 11CRC03-048 Ptg T-A GY-GN R S CHL ? F 0.280 48 49 11CRC03-049 Ptg T-A GY-GN R S CHL ? F 0.038 49 50 11CRC03-050 Ptg T-A GY-GN R S CHL ? F 0.349 50 51 11CRC03-051 Ptg T-A GY-GN R S CHL ? F 0.094 51 52 11CRC03-052 Ptg T-A GY-GN R S CHL ? F 0.017 52 53 11CRC03-053 Ptg T-A GY-GN R S CHL ? F 0.248 53 54 11CRC03-054 Ptg T-A GY-GN R S CHL ? F 0.190 54 55 11CRC03-055 Ptg T-A GY-GN R S CHL ? F 0.376 55 56 11CRC03-056 Ptg T-A GY-GN R S CHL ? F 0.049 56 57 11CRC03-057 Ptg T-A GY-GN R S CHL ? F 0.037 57 58 11CRC03-058 Ptg T-A GY-GN R S CHL ? F 0.167 58 59 11CRC03-059 Ptg T-A GY-GN R S CHL ? F 0.181 59 60 11CRC03-060 Ptg T-A GY-GN R S CHL ? F 0.155 60 61 11CRC03-061 Ptg T-A GY-GN R S CHL ? F 0.179 61 62 11CRC03-062 Ptg T-A GY-GN R S CHL ? F 0.141 62 63 11CRC03-063 Ptg T-A GY-GN R S CHL ? F 0.147 63 64 11CRC03-064 Ptg T-A GY-GN R S CHL ? F 0.037 64 65 11CRC03-065 Ptg T-A GY-GN R S CHL ? F 0.031 65 66 11CRC03-066 Ptg T-A GY-GN R S CHL ? F 0.206 66 67 11CRC03-067 Ptg T-A GY-GN R S CHL ? F 0.091 67 68 11CRC03-068 Ptg T-A GY-GN R S CHL ? F 0.181 68 69 11CRC03-069 Ptg T-A GY-GN R S CHL ? F 0.156 69 70 11CRC03-070 Ptg T-A GY-GN R S CHL ? F 0.141 70 71 11CRC03-071 Ptg T-A GY-GN R S CHL ? F 0.118 71 72 11CRC03-072 Ptg T-A GY-GN R S CHL ? F 0.129 72 73 11CRC03-073 Ptg CLY BN-GY REDOX VS CHL ? VF 0.131 73 74 11CRC03-074 Ptg T-A BL-GN R S CHL ? F 0.056 74 75 11CRC03-075 Ptg T-A BL-GN R S CHL ? F 0.108 75 76 11CRC03-076 Ptg T-A BL-GN R S CHL ? F 0.107

GEOLOGISTS NOTES

SOME GREEN VERY SOT CLAY

CONSPICUOUS DARK BROWN CLAY

CONSPICUOUS DARK BROWN CLAY

REDUCED, VADOSE ZONE ?

CLAY

BN AND BL-GY CLAY, SLIGHTY WET

3.5


3.0

2.5

2.0

1.5

30 sec

1.0

0.5

0.0 1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 37 39 41 43 45

CODES

DRILLING LOG

LITHO: CLY=CLAY COLOUR: SELF-EXPLANATORY OXIDATI S=STRONG, M=MODERATE, W=WEAK, R=REDUCED, REDOX=BOTH OXIDISED AND REDUCED PIECES

Start Date:

17-Nov-11

Finish Date:

17-Nov-11

HARDNESS: VH=VERY HARD, H=HARD, M=MODERATELY HARD, S=SOFT, VS=VERY SOFT

ALTERATION: CAL=CALCITE, CHL=CHLORITE, QTZ=QUARTZ, LIM=LIMONITE, PYR=PYRITE MINERALIS: MAL=MALACHITE, AZU=AZURITE, BOR=BORNITE,CHC=CHALCOCITE

Project:

Redbank

Prospect:

Black Charlie

Tenement:

ERL94

Hole ID:

Dip:

Geologist:

11BCRC04

60 ANTOINE

GPS Easting:

MAG Azimuth:

Contractor:

794887

180 OME

GPS Northing: 8E+06 GPS 210 DATUM: GDA

EOH: 103 DRILLER WATER TABLE: NONE

Hole Type: RC

Hole Comment: WEATHERED SOFT ALL THROUGHOUT, REDOX DEPTH DIP AZIM

SURVEY1 30 59 185.6 SURVEY2 60 -63 337.4 SURVEY3 90 67 179.2

From To Bag No

STRATLITHO COLOUR OXID HARD ALT 1 ALT 2 ALT 3 MIN 1 MIN 2 TXT CuXRF EOLOGISTS NOTES

0 1 11CRC04-001 Ptg T-A BN S S CAL F 0.088 FIZZES

1 2 11CRC04-002 Ptg T-A BN S S CAL F 0.292

2 3 11CRC04-003 Ptg T-A BN S S CAL F 0.253 3 4 11CRC04-004 Ptg T-A BN S S CAL F 0.160

4 5 11CRC04-005 Ptg T-A BN S S CAL F 0.170

5 6 11CRC04-006 Ptg T-A GN-BN S S CAL MAL ? F 0.452 FIZZES

6 7 11CRC04-007 Ptg T-A GN R ? S CAL CHL ? MAL ? F 0.343 FIZZES

7 8 11CRC04-008 Ptg T-A GN R ? S CAL F 0.231 8 9 11CRC04-009 Ptg T-A GN R ? S CAL F 0.236

9 10 11CRC04-010 Ptg T-A BR M S CAL F 0.251 FIZZES

10 11 11CRC04-011 Ptg T-A BR M S CAL F 0.104

11 12 11CRC04-012 Ptg T-A BR M S CAL F 0.028 12 13 11CRC04-013 Ptg T-A BR M S CAL F 0.044


15 16 11CRC04-016 Ptg T-A BR M S CAL F 0.074




22 23 11CRC04-023 Ptg T-A BR M S CAL F 0.320 23 24 11CRC04-024 Ptg T-A BL-GN R ? S CAL ? MAL F 0.744 FIZZES

SOME 24 25 11CRC04-025 Ptg T-A BL-GN-YE REDOX S CAL ? MAL F 1.570

25 26 11CRC04-026 Ptg T-A BN-GN S S CAL ? MAL MO 0.329 26 27 11CRC04-027 Ptg T-A BN-GN S S CAL ? F 0.288

27 28 11CRC04-028 Ptg T-A BN-GN S S CAL ? F 0.183 28 29 11CRC04-029 Ptg T-A BN-GN S S CAL ? F 0.330



33 34 11CRC04-034 Ptg T-A BN-GN S S CAL ? F 0.098


36 37 11CRC04-037 Ptg T-A GN R ? S CAL ? MAL F 0.559 37 38 11CRC04-038 Ptg T-A GN-BN REDOX ? S CAL ? MAL F 0.244

38 39 11CRC04-039 Ptg T-A BN S S CAL ? F 0.387 39 40 11CRC04-040 Ptg T-A BL-GN-YE/O REDOX ? S CAL ? MAL F 0.471 40 41 11CRC04-041 Ptg T-A BL-GN-YE/O REDOX ? S CAL ? F 0.227 41 42 11CRC04-042 Ptg T-A BL-GN-YE/O REDOX ? S CAL ? F 0.424

42 43 11CRC04-043 Ptg T-A BL-GN-YE/O REDOX ? S CAL ? F 0.511

43 44 11CRC04-044 Ptg T-A BL-GN-YE/O REDOX ? S CAL ? F 0.123 44 45 11CRC04-045 Ptg T-A BL-GN-YE/O REDOX ? S CAL ? F 0.118

45 46 11CRC04-046 Ptg T-A BL-GN-YE/O REDOX ? S CAL ? F 0.144 46 47 11CRC04-047 Ptg T-A BL-GN-YE/O REDOX ? S CAL ? F 0.195

47 48 11CRC04-048 Ptg T-A BL R S CAL ? F 0.063 48 49 11CRC04-049 Ptg T-A BL R S CAL ? F 0.057




55 56 11CRC04-056 Ptg T-A BL R S CAL ? F 0.125





64 65 11CRC04-065 Ptg T-A BL R S CAL ? F 0.415 65 66 11CRC04-066 Ptg T-A BL R S CAL ? F 0.229 66 67 11CRC04-067 Ptg T-A BL R S CAL ? F 0.189














91 92 11CRC04-092 Ptg T-A BL R S CAL ? F 0.110 92 93 11CRC04-093 Ptg T-A BL R S CAL ? F 0.154 93 94 11CRC04-094 Ptg T-A BL R S CAL ? F 0.095 94 95 11CRC04-095 Ptg T-A BL R S CAL ? F 0.045




100 101 11CRC04-100 Ptg T-A BL R S CAL ? F 0.013 101 102 11CRC04-100 Ptg T-A BL R S CAL ? F 0.012 102 103 11CRC04-100 Ptg T-A BL R S CAL ? F 0.006

BITS 10% MALACHITE MOTTLES WITHIN

MINOR OXIDISED MOTTLES

FREQUENT COATING IN FREQUENT COATING IN FREQUENT COATING IN FREQUENT COATING IN FREQUENT COATING IN FREQUENT COATING IN FREQUENT COATING IN FREQUENT COATING IN FIZZES; veins below 89m

0.0

0.5

1.0

1.5

2.0

2.5

3.0

3.51 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 37 39 41 43 45 47 49 51 53 55 57 59 61 63 65 67 69 71 73 75 77 79 81 83 85 87 89 91 93 95 97 99 101

103

11BCRC ‐ 04XRF %Cu

Series2

Series1

DRILLING LOG CODES

LITHO: CLY=CLAY COLOUR: SELF-EXPLANATORY OXIDATI S=STRONG, M=MODERATE, W=WEAK, R=REDUCED, REDOX=BOTH OXIDISED AND REDUCED PIECES, BL=BLEACHED,FR=FRESH

Start Date:

17-Nov-11

Finish Date:

17-Nov-11

HARDNESS: VH=VERY HARD, H=HARD, M=MODERATELY HARD, S=SOFT, VS=VERY SOFT, CR=CRUMBLY

ALTERATION: CAL=CALCITE, CHL=CHLORITE, QTZ=QUARTZ, LIM=LIMONITE, PYR=PYRITE MINERALIS: MAL=MALACHITE, AZU=AZURITE, BOR=BORNITE,CHC=CHALCOCITE

TXTURE: C=COARSE, F=FINE, V=VERY FINE, MO=MOTTLED, BAN=BANDED, LAM=LAMINATED

Project: Redbank

Prospect:

Black Charlie

Tenement:

ERL94

Hole ID:

Dip:

Geologist:

11CRC05

60 ANTOINE

GPS Easting:

MAG Azimuth:

Contractor:

794895

0 OME

8E+06 RL: 219 DATUM: GDA

EOH: 97m DRILLER WATER TABLE: 60m

Hole Type: RC

Hole Comment: SOFT ALL THRU

DEPTH DIP AZIM SURVEY1 30 61 302.8 SURVEY2 60 61 190.7 SURVEY3 90 63 2.8 From To Bag No

STRA LITHO COLOUR OXID HARD ALT 1 ALT 2 ALT 3 MIN 1 MIN 2 TXT CuXRF COMMENTS

FIZZES; 0 1 11CRC05-001 Ptg T-A BN-BK S S CAL F 0.050 WITH

1 2 11CRC05-002 Ptg T-A BN-BK S S CAL F 0.079 WITH FIZZES;

2 3 11CRC05-003 Ptg T-A BN-OG S S CAL F 0.254 SOME BITS

3 4 11CRC05-004 Ptg T-A BN-OG S S CAL F 0.415




















23 24 11CRC05-024 Ptg T-A GN R ? S CAL ? MAL F 0.406

24 25 11CRC05-025 Ptg T-A GN R ? S CAL ? F 0.357







31 32 11CRC05-032 Ptg T-A BL R S CAL F 0.415

32 33 11CRC05-033 Ptg T-A BL-OG REDOX ? S CAL MAL F 0.743

33 34 11CRC05-034 Ptg T-A BL R S CAL MAL ? F 0.778




























61 62 11CRC05-062 Ptg T-A BL-OG REDOX S CAL F 0.034












73 74 11CRC05-074 Ptg T-A BR-BL REDOX S CAL F 0.005 ON DENSE REDUCED

74 75 11CRC05-075 Ptg T-A BR-BL REDOX S CAL F 0.005 ON DENSE

75 76 11CRC05-076 Ptg T-A BR-BL REDOX S CAL F 0.005 ON DENSE REDOX

76 77 11CRC05-077 Ptg T-A BL-BR REDOX S CAL F 0.009 BITS;NO

77 78 11CRC05-078 Ptg T-A BL-BR REDOX S CAL F 0.009

78 79 11CRC05-079 Ptg T-A BL-BR REDOX S CAL F 0.004






84 85 11CRC05-085 Ptg T-A BL-TAN-OG REDOX S CAL F 0.006













0.0

0.5

1.0

1.5

2.0

2.5

3.0

3.5

1 3 5 7 9 1113151719212325272931333537394143454749515355575961636567697173757779818385878991939597


Series2

Series1

DRILLING LOG CODES

LITHO: CLY=CLAY COLOUR: SELF-EXPLANATORY OXIDATI S=STRONG, M=MODERATE, W=WEAK, R=REDUCED, REDOX=BOTH OXIDISED AND REDUCED PIECES, BL=BLEACHED,FR=FRESH

Start Date:

18th november 2011

Finish Date:

19th november 2011

HARDNESS: VH=VERY HARD, H=HARD, M=MODERATELY HARD, S=SOFT, VS=VERY SOFT, CR=CRUMBLY

ALTERATION: CAL=CALCITE, CHL=CHLORITE, QTZ=QUARTZ, LIM=LIMONITE, PYR=PYRITE MINERALIS: MAL=MALACHITE, AZU=AZURITE, BOR=BORNITE,CHC=CHALCOCITE TXTURE: C=COARSE, F=FINE, V=VERY FINE, MOT=MOTTLED, BAN=BANDED, LAM=LAMINATED

Project:

Redbank

Prospect:

Black Charlie

Tenement:

ERL94

Hole ID:

Dip:

Geologist:

11BCRC06 60 ANTOINE

GPS Easting:

MAG Azimuth:

Contractor:

794919 0 OME

North. : 896291 RL: 211 DATUM: GDA

EOH: 121 DRILLER WATER TABLE: 64m

Hole Type: RC

Hole Comment: hole extended to go through coastean; OBSERVED MORE REDOX VARIATONS AND CALCITE VEINS THERE THAN IN T

DEPTH DIP AZIM SURVEY1 30 61 249.8 SURVEY2 60 62 305 SURVEY3 SURVEY 4

90 63 205.8 120 63 167.7

From To Bag No STRATLITHO COLOUR OXID HARD ALT 1 ALT 2 ALT 3 MIN 1 MIN 2 TXT CuXRF COMMENTS

0 1 11CRC06-001 Ptg T-A RD VS M CAL F 0.060 1 2 11CRC06-002 Ptg T-A RD VS M CAL F 0.066

2 3 11CRC06-003 Ptg T-A RD-BN-GN S S CAL MAL F 0.333

3 4 11CRC06-004 Ptg T-A RD-BN-GN S S CAL MAL F 0.678 4 5 11CRC06-005 Ptg T-A TAN-GN ? VS CLY MAL F 1.160

5 6 11CRC06-006 Ptg T-A GY-GN R S CAL MAL F 0.972

6 7 11CRC06-007 Ptg T-A GY-GN R S CAL MAL F 0.378 7 8 11CRC06-008 Ptg T-A OG-RD-GN S S CAL MAL F 0.630

8 9 11CRC06-009 Ptg T-A BN-OG S S CAL MAL F 0.891

9 10 11CRC06-010 Ptg T-A BK-OG-GN S S CAL MAL F 1.220 10 11 11CRC06-011 Ptg T-A BK-OG-GN S S CAL MAL F 1.460

11 12 11CRC06-012 Ptg T-A BK-OG-GN S S CAL MAL F 1.580

12 13 11CRC06-013 Ptg T-A BK-OG-GN S S CAL MAL F 1.750 13 14 11CRC06-014 Ptg T-A BK-OG-GN S S CAL MAL F 1.020

14 15 11CRC06-015 Ptg T-A BN M S CAL MAL F 1.320

15 16 11CRC06-016 Ptg T-A GN-OG-BK REDOX S CAL MAL F 0.721

16 17 11CRC06-017 Ptg T-A GN-OG-BK REDOX S CAL MAL F 1.910 17 18 11CRC06-018 Ptg T-A GN-OG-BK REDOX S CAL MAL F 0.929



20 21 11CRC06-021 Ptg T-A GN-OG-BK REDOX S CAL MAL F 1.450 21 22 11CRC06-022 Ptg T-A GN-OG-BK REDOX S CAL MAL F 1.350


23 24 11CRC06-024 Ptg T-A BL R S CAL F 0.616 24 25 11CRC06-025 Ptg T-A BL R S CAL F 0.389




29 30 11CRC06-030 Ptg T-A BL-RD REDOX S CAL F 0.493

30 31 11CRC06-031 Ptg T-A GY R S CAL F 0.477

31 32 11CRC06-032 Ptg T-A GY R S CAL F 0.154 32 33 11CRC06-033 Ptg T-A GY R S CAL F 0.255




IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

IS PYROBITU

36 37 11CRC06-037 Ptg T-A GY-OG REDOX S CAL MAL F 1.180 COATINGS OXIDE

37 38 11CRC06-038 Ptg T-A GY-OG REDOX S CAL MAL F 0.642

















COATINGS NOT

VISIBLE NOT

VISIBLE NOT

VISIBLE NOT

VISIBLE

60 61 11CRC06-061 Ptg T-A GY-BN-GN REDOX S CAL MOT 0.077 MOTTLED

61 62 11CRC06-062 Ptg T-A GY-BN-GN REDOX S CAL F 0.032 62 63 11CRC06-063 Ptg T-A GY-BN-GN REDOX S CAL F 0.031

63 64 11CRC06-064 Ptg T-A GY-BN-GN REDOX S CAL F 0.017

64 65 11CRC06-065 Ptg T-A GY-BN-GN REDOX S CAL F 0.012 65 66 11CRC06-066 Ptg T-A GY-BN-GN REDOX S CAL F 0.009

66 67 11CRC06-067 Ptg T-A RD-BL REDOX S CAL F 0.040

67 68 11CRC06-068 Ptg T-A GY-BN R S CAL F 0.125

68 69 11CRC06-069 Ptg T-A GY-BN R S CAL F 0.041 69 70 11CRC06-070 Ptg T-A GY-BN R S CAL F 0.016



72 73 11CRC06-073 Ptg T-A GY-BN R S CAL F 0.008 73 74 11CRC06-074 Ptg T-A GY-BN R S CAL F 0.027



76 77 11CRC06-077 Ptg T-A GY-BN R S CAL F 0.041 77 78 11CRC06-078 Ptg T-A GN R S CAL MAL ? F 0.008

78 79 11CRC06-079 Ptg T-A GY R S CAL MAL ? F 0.012

75

76

11CRC06-076 P tg

T-A

GY-BN

R

S

CAL

F

0.014

76

77

11CRC06-077 P tg

T-A

GY-BN

R

S

CAL

F

0.041

77

78

11CRC06-078 P tg

T-A

GN

R

S

CAL

MAL ? F

0.008

78

79

11CRC06-079 P

tg

T-A

GY

R

S

CAL

MAL ? F

0.012

79

80

11CRC06-080 P

tg

T-A

GY-BN

REDOX

S

CAL

F

0.022 BN COATING ON MICROFRACTURES

80

81

11CRC06-081 P

tg

T-A

GY-BN

REDOX

S

CAL

F


81

82

11CRC06-082 P

tg

T-A

GY-BN

REDOX

S

CAL

F


82

83

11CRC06-083 P

tg

T-A

GY-BN

REDOX

S

CAL

F


83

84

11CRC06-084 P

tg

T-A

GY-BN

REDOX

S

CAL

F

0.008

PERVASIVE OXIDATION, NOT COATINGS LIKE ABOVE

84

85

11CRC06-085 P

tg

T-A

RD-GN-BL

REDOX

S

CAL

F

0.025

85

86

11CRC06-086 P tg

T-A

RD-GN-BL

REDOX

S

CAL

F

0.023

86

87

11CRC06-087 P tg

T-A

RD-GN-BL

REDOX

S

CAL

F

0.017

87

88

11CRC06-088 P tg

T-A

RD-GN-BL

REDOX

S

CAL

F

0.006

88

89

11CRC06-089 P tg

T-A

RD-BL-BN

REDOX

S

CAL

F

0.006

BN COATING

89

90

11CRC06-090 P

tg

T-A

GY

R

S

CAL

F

0.010

90

91

11CRC06-091 P tg

T-A

GY

R

S

CAL

F

0.006

91

92

11CRC06-092 P tg

T-A

GY-RD

REDOX

S

CAL

F

0.009

92

93

11CRC06-093 P tg

T-A

GY

R

S

CAL

F

0.006

93

94

11CRC06-094 P tg

T-A

GY

R

S

CAL

F

0.009

94

95

11CRC06-095 P tg

T-A

GY

R

S

CAL

F

0.008

95

96

11CRC06-096 P tg

T-A

GY

R

S

CAL

F

0.009

96

97

11CRC06-097 P tg

T-A

OG-BL

REDOX

S

CAL

F

0.005

97

98

11CRC06-098 P tg

T-A

RD-BN-GN

REDOX

S

CAL

MAL F

0.023

98

99

11CRC06-099 P

tg

T-A

BL-RD

REDOX

S

CAL

F

0.031

99

100

11CRC06-100 P tg

T-A

GN-BN

R

S

CAL

F

0.011 WITH GREEN COATINGS ON MICROFRACTURES

100 101 11CRC06-101 P tg T-A GN-RD REDOX S CAL F 0.027






106

107

11CRC06-107

P tg

T-A

BL-GN-OG

REDOX

S

CAL

F

0.013

MOSTLY REDUCED

107

108

11CRC06-108

P tg

T-A

GN-OG

REDOX

S

CAL

F

0.007

MORE OXIDISED

108 109 11CRC06-109 P tg T-A GN-OG REDOX S CAL F 0.005


110 111 11CRC06-111 P tg T-A BN-OG REDOX S CAL F 0.007


112

113

11CRC06-113

P tg

T-A

GN-RD

REDOX

S

CAL

F

0.004

MILLIMETRIC CALCITE VEINS

113

114

11CRC06-114

P tg

T-A

GN-RD

REDOX

S

CAL

F

0.003

MILLIMETRIC CALCITE VEINS

114 115 11CRC06-115 P tg T-A GN-BN-OG REDOX S CAL F 0.003

115

116

11CRC06-116

P tg

T-A

GN-BN-OG-RD

REDOX

S

CAL

F

0.004

WITH CALCITE VEINS

116 117 11CRC06-117 P tg T-A RD-GN REDOX S CAL F 0.004

117 118 11CRC06-118 P tg T-A RD S S CAL F 0.007

118 119 11CRC06-119 Ptg T-A RD-GN REDOX S CAL F 0.015

119 120 11CRC06-120 Ptg T-A RD-GN REDOX S CAL F 0.012


0.0

0.5

1.0

1.5

2.0

2.5

3.0

3.5

1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 37 39 41 43 45 47 49 51 53 55 57 59 61 63 65 67 69 71 73 75 77 79 81 83 85 87 89 91 93 95 97 99 101

103

105

107

109

111

113

115

117

119

121


Series2

Series1

V

V

V

a

A

C D S

LITH C O: e COLO G UR: et

DRILLIN

OO EE LLY=CLAY c... YY=GREY c...

G LOG

t

OXID ATIO

t S=STRONG, M=MODERATE, W=WEA KKK , R=REDUCED, REDOX=BOTH OXIDISED AND

N: REDUCED PIECES, BL=BLEACHED,FR=FRES HHH HARD NESS : ALTE RATI ON: MINE RALI

VH=VERY HARD, H=HARD, M=MODER AAA TELY HARD, S=SOFT, VS=VERY SOFT, CR=CRUMBLY CAL=CALCITE, CHL=CHLORITE, QTZ= QQQ UARTZ, LIM=LIMONITE, PYR=PYRITE, CLY=CLAY

S: MAL=MALACHITE, AZU=AZURITE, BOR === BORNITE,CHC=CHALCOCITE

Start Date: 19-Nov-11 Finish Date: 20-Nov-11

TXTUR E: C=COARSE, F=FINE, V= VVVERY FINE, MOT=MOT TTT LED, BAN=BANDED, LAM=LAMINATED

Project: Redbank Prospect: Black Charlie Tenement: ERL94

Hole ID: 11CRC07 GPS Easting: 794942

8E North. +0 : 6

RL: 238

G D

DATUM: A

Dip: 60 MAG zimuth: 0

E DRILLER O WATER H: TABLE:

Geologist: ANTOINE Contractor: OME Hole Type: RC

Hole Comment:

DEPTH

DIP

AZI M

SURVE Y1

SURVE Y2

SURVE Y3

From

To

Bag No

STR AT

LIT HO

COLOUR

OXID

HA RD

A L T 1

ALT 2

A LT 3

MIN

1

MIN

2

TX T

Cu XR F

COMMENTS

0

1

11CRC07- 001

Ptg

IRO

RD

S

H

VF

0.1 70

IRONSTONE ?

1

2

11CRC07- 002

Ptg

T-A

OG-TAN-BK

S

S

0.2 88

BK=PYOBIT UUU MEN OR HEMATIT E ?

2

3

11CRC07- 003

Ptg

T-A

0.3 37

3

4 11CRC07-

004

Ptg

T-A 0.0

72

4

5

11CRC07- 005

Ptg

T-A

0.1 72

5

6 11CRC07-

006

Ptg

T-A 0.2

32

6

7

11CRC07-

007

Ptg

T- A,P YR

OG-YE-RD- TAN-BK-GN

S

S

C A L

LIM?

MA L ?

F

0.3 27

WITH PYROBITUM EEE N

7

8

11CRC07- 008

Ptg

T-A

0.3 58

8

9 11CRC07-

009

Ptg

T-A 0.3

44

9

10

11CRC07- 010

Ptg

T-A

RD

S

S

F

0.6 88

10

11 11CRC07-

011

Ptg

T-A

PP

M

S 0.5

30

11

12

11CRC07- 012

Ptg

T-A

0.2 23

12

13 11CRC07-

013

Ptg

T-A 0.2

25

13

14

11CRC07- 014

Ptg

T-A

0.1 01

14

15 11CRC07-

015

Ptg

T-A 0.0

97

15

16

11CRC07-

016

Ptg

T-A

PP-YE

M

S

0.0 77

STRONGER YYY E OXIDES IN MICRORACT URES

16

17

11CRC07- 017

Ptg

T-A

0.0 53

17

18 11CRC07-

018

Ptg

T-A

BN-GY

REDO

X?

S 0.0

25

18

19

11CRC07-

019

Ptg

T-A

GY-BN

REDO

X

0.0 57

BN OXIDE COATING IN MICROFRACTURE S

19

20

11CRC07- 020

Ptg

T-A

0.0 62

20

21 11CRC07-

021

Ptg

T-A 0.0

85

21

22

11CRC07- 022

Ptg

T-A

0.1 03

22

23 11CRC07-

023

Ptg

T-A 0.0

57

23

24

11CRC07- 024

Ptg

T-A

F

0.1 36

24

25

11CRC07- 025

Ptg

T-A

GY-WH-RD

REDO X

S

C A L

F+

0.1 62

CONSPICUOUSLY COARSER THAN ABOVE, WITH UP TO 15% CALCITE VEINS, DECREASING TO 0% DOWNWARDS

25

26

11CRC07- 026

Ptg

T-A

0.0 32

26

27 11CRC07-

027

Ptg

T-A 0.0

43

27

28

11CRC07- 028

Ptg

T-A

0.0 35

28

29

11CRC07-

029

Ptg

T-A

BN-BL

REDO

X

S

C L Y

F

0.1 09

BACK TO FINER TEXTURE; DRILLING SLOWED BY CLY

29

30

11CRC07- 030

Ptg

T-A

0.1 12

30

31 11CRC07-

031

Ptg

T-A 0.0

61

31

32

11CRC07- 032

Ptg

T-A

0.0 85

32

33 11CRC07-

033

Ptg

T-A 0.0

61

33

34

11CRC07- 034

Ptg

T-A

0.1 08

34

35 11CRC07-

035

Ptg

T-A 0.0

95

35

36

11CRC07- 036

Ptg

T-A

0.1 16

36

37 11CRC07-

037

Ptg

T-A

BL-GN REDO

X

S

F 0.0 64

37

38

11CRC07-

038

Ptg

T-A

BL-OG

REDO

X

S

F

0.0 80

OG OXIDE COATING OF BL CHIPS

38

39

11CRC07- 039

Ptg

T-A

F

0.0 67

39

40 11CRC07-

040

Ptg

T-A

F 0.1 67

40

41 11CRC07-

041

Ptg

T-A

BL-RD REDO

X

S

F 0.3 64

41

42 11CRC07-

042

Ptg

T-A

F 0.4 92

42

43 11CRC07-

043

Ptg

T-A

BL

R

S

F 0.0 90

43

44 11CRC07-

044

Ptg

T-A

F 0.0 32

44

45 11CRC07-

045

Ptg

T-A

F 0.0 37

45

46 11CRC07-

046

Ptg

T-A

F 0.0 37

46

47 11CRC07-

047

Ptg

T-A

F 0.0 27

47

48 11CRC07-

048

Ptg

T-A

F 0.0 19

48

49 11CRC07-

049

Ptg

T-A

F 0.0 15

49

50 11CRC07-

050

Ptg

T-A

F 0.0 13

50

51 11CRC07-

051

Ptg

T-A

F 0.0 19

51

52 11CRC07-

052

Ptg

T-A

F 0.0 31

52

53 11CRC07-

053

Ptg

T-A

F 0.0 47

53

54 11CRC07-

054

Ptg

T-A

BL-GN

R

S

F 0.0 14

54

55 11CRC07-

055

Ptg

T-A

F 0.0 09

55

56 11CRC07-

056

Ptg

T-A

F 0.0 09

56

57 11CRC07-

057

Ptg

T-A

F 0.0 10

57

58 11CRC07-

058

Ptg

T-A

F 0.0 16

58

59 11CRC07-

059

Ptg

T-A

F 0.0 20

59

60 11CRC07-

060

Ptg

T-A

F 0.0 30

60

61

11CRC07- 061

Ptg

T-A

BN-GN

REDO

X

S

F 0.0 90

61

62 11CRC07-

062

Ptg

T-A

RD-GN REDO

X

S

F 0.0 11

62

63 11CRC07-

063

Ptg

T-A

F 0.0 09

63

64 11CRC07-

064

Ptg

T-A

F 0.0 07

64

65 11CRC07-

065

Ptg

T-A

F 0.0 05

65

66 11CRC07-

066

Ptg

T-A

F 0.0 00

66

67 11CRC07-

067

Ptg

T-A

F 0.0 11

67

68 11CRC07-

068

Ptg

T-A

F 0.0 09

68

69

11CRC07- 069

Ptg

T-A, PY R

BN-GN-OG- BK

REDO X

S

C L Y

CAL

F

0.0 04

WITH MINOR PYROBIYUMEN/PY ROLUSITE/MANGA NESE-RICH- SIDERITE BUT ONLY FROM 68 TO 69m

69

70

11CRC07- 070

Ptg

T-A

F

0.0 04

70

71 11CRC07-

071

Ptg

T-A

F 0.0 04

71

72 11CRC07-

072

Ptg

T-A

F 0.0 04

72

73 11CRC07-

073

Ptg

T-A

F 0.0 06

73

74

11CRC07-

074

Ptg

T-A

GY-BN

R

S

C L Y

CAL

0.0 03

74

75

11CRC07-

075

Ptg

T-A

GN-OG-BK

REDO

X ?

S

C L Y

CAL

0.0 05

WITH PYROBITUMEN

75

76

11CRC07- 076

Ptg

T-A

0.0 04

76

77 11CRC07-

077

Ptg

T-A 0.0

05

77

78

11CRC07- 078

Ptg

T-A

0.0 07

78

79 11CRC07-

079

Ptg

T-A 0.0

07

79

80

11CRC07- 080

Ptg

T-A

0.0 23

80

81 11CRC07-

081

Ptg

T-A 0.0

17

81

82

11CRC07- 082

Ptg

T-A

0.0 03

82

83 11CRC07-

083

Ptg

T-A 0.0

00

83

84

11CRC07- 084

Ptg

T-A

0.0 00

84

85 11CRC07-

085

Ptg

T-A 0.0

07

85

86

11CRC07- 086

Ptg

T-A

0.0 06

86

87 11CRC07-

087

Ptg

T-A 0.0

04

87

88

11CRC07- 088

Ptg

T-A

0.0 04

88

89 11CRC07-

089

Ptg

T-A 0.0

04

89

90

11CRC07- 090

Ptg

T-A

0.0 05

90

91 11CRC07-

091

Ptg

T-A 0.0

05

91

92

11CRC07- 092

Ptg

T-A

92

93 11CRC07-

093

Ptg

T-A

93

94

11CRC07- 094

Ptg

T-A

94

95 11CRC07-

095

Ptg

T-A

95

96

11CRC07- 096

Ptg

T-A

96

97 11CRC07-

097

Ptg

T-A

97

98

11CRC07- 098

Ptg

T-A

98

99 11CRC07-

099

Ptg

T-A

99

10 0

11CRC07- 100

Ptg

T-A

0.0

0.5

1.0

1.5

2.0

2.5

3.0

3.51 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 37 39 41 43 45 47 49 51 53 55 57 59 61 63 65 67 69 71 73 75 77 79 81 83 85 87 89 91 93 95 97 99 101

103

105

107

109

111

113


Series2

Series1

Start Date:

20th nov 11

Finish Date:

20th nov 11

DRILLING LOG CODES

LITHO: PYR=PYROBITUMEN, T-A=TRACHYANDESITE, REG=REGOLITH, SOL=SOIL, SST=SANDSTONE, CLY=CLAY, etc... COLOUR: GY=GREY etc... OXIDATI S=STRONG, M=MODERATE, W=WEAK, R=REDUCED, REDOX=BOTH OXIDISED AND REDUCED PIECES, BL=BLEACHED,FR=FR HARDNESS: VH=VERY HARD, H=HARD, M=MODERATELY HARD, S=SOFT, VS=VERY SOFT, CR=CRUMBLY

ALTERATION: CAL=CALCITE, CHL=CHLORITE, QTZ=QUARTZ, LIM=LIMONITE, PYR=PYRITE, CLY=CLAY MINERALIS: MAL=MALACHITE, AZU=AZURITE, BOR=BORNITE,CHC=CHALCOCITE TXTURE: C=COARSE, F=FINE, V=VERY FINE, MOT=MOTTLED, BAN=BANDED, LAM=LAMINATED

Project:

Redbank

Prospect:

Black Charlie

Tenement:

ERL94

Hole ID:

11BCRC08

GPS Easting:

794965

North. : 8096289 RL: 217 DATUM: GDA

Dip: 60 MAG Azimuth: 0 EOH: DRILLER WATER TABLE: NONE

Geologist:

ANTOINE

Contractor:

OME

Hole Type: RC

Hole Comment: HOLE ABORTED AT HEAVY RAIN TO MOVE TO MASTERTON BEORE GROUND CONDITIONS GET UNSTABLE.

DEPTH DIP AZIM SURVEY1 N/A SURVEY2 N/A SURVEY3 N/A From To Bag No STRATLITHO COLOUR OXID HARD ALT 1 ALT 2 ALT 3 MIN 1 MIN 2 TXT CuXRF COMMENTS

0 1 11CRC08-001 tg-RE T-A RD S H-S CAL QTZ HEM? 0.060 WITH QUARTZITIC HARD CHIPS

1 2 11CRC08-002 Ptg T-A TAN-RD-GN S S CAL MAL? 0.044 2 3 11CRC08-003 Ptg T-A TAN-RD S S-VS CLY CAL 0.046 3 4 11CRC08-004 Ptg T-A TAN ? S CLY CAL 0.062 4 5 11CRC08-005 Ptg T-A TAN-BN-OG S S CLY CAL 0.099 5 6 11CRC08-006 Ptg T-A TAN ? S-VS CLY CAL 0.072

6 7 11CRC08-007 Ptg T-A TAN-OG-YE S S-VS CLY CAL 0.046 7 8 11CRC08-008 Ptg T-A TAN-OG SVB S-VS CLY CAL 8 9 11CRC08-009 Ptg T-A 9 10 11CRC08-010 Ptg T-A 10 11 11CRC08-011 Ptg T-A 11 12 11CRC08-012 Ptg T-A 12 13 11CRC08-013 Ptg T-A 13 14 11CRC08-014 Ptg T-A 14 15 11CRC08-015 Ptg T-A 15 16 11CRC08-016 Ptg T-A 16 17 11CRC08-017 Ptg T-A 17 18 11CRC08-018 Ptg T-A 18 19 11CRC08-019 Ptg T-A 19 20 11CRC08-020 Ptg T-A 20 21 11CRC08-021 Ptg T-A 21 22 11CRC08-022 Ptg T-A 22 23 11CRC08-023 Ptg T-A 23 24 11CRC08-024 Ptg T-A 24 25 11CRC08-025 Ptg T-A 25 26 11CRC08-026 Ptg T-A 26 27 11CRC08-027 Ptg T-A 27 28 11CRC08-028 Ptg T-A 28 29 11CRC08-029 Ptg T-A 29 30 11CRC08-030 Ptg T-A 30 31 11CRC08-031 Ptg T-A 31 32 11CRC08-032 Ptg T-A 32 33 11CRC08-033 Ptg T-A 33 34 11CRC08-034 Ptg T-A 34 35 11CRC08-035 Ptg T-A 35 36 11CRC08-036 Ptg T-A 36 37 11CRC08-037 Ptg T-A 37 38 11CRC08-038 Ptg T-A 38 39 11CRC08-039 Ptg T-A 39 40 11CRC08-040 Ptg T-A 40 41 11CRC08-041 Ptg T-A 41 42 11CRC08-042 Ptg T-A 42 43 11CRC08-043 Ptg T-A 43 44 11CRC08-044 Ptg T-A 44 45 11CRC08-045 Ptg T-A 45 46 11CRC08-046 Ptg T-A 46 47 11CRC08-047 Ptg T-A 47 48 11CRC08-048 Ptg T-A 48 49 11CRC08-049 Ptg T-A 49 50 11CRC08-050 Ptg T-A 50 51 11CRC08-051 Ptg T-A 51 52 11CRC08-052 Ptg T-A 52 53 11CRC08-053 Ptg T-A 53 54 11CRC08-054 Ptg T-A 54 55 11CRC08-055 Ptg T-A 55 56 11CRC08-056 Ptg T-A 56 57 11CRC08-057 Ptg T-A 57 58 11CRC08-058 Ptg T-A 58 59 11CRC08-059 Ptg T-A 59 60 11CRC08-060 Ptg T-A 60 61 11CRC08-061 Ptg T-A 61 62 11CRC08-062 Ptg T-A 62 63 11CRC08-063 Ptg T-A 63 64 11CRC08-064 Ptg T-A 64 65 11CRC08-065 Ptg T-A 65 66 11CRC08-066 Ptg T-A 66 67 11CRC08-067 Ptg T-A 67 68 11CRC08-068 Ptg T-A 68 69 11CRC08-069 Ptg T-A 69 70 11CRC08-070 Ptg T-A 70 71 11CRC08-071 Ptg T-A 71 72 11CRC08-072 Ptg T-A 72 73 11CRC08-073 Ptg T-A 73 74 11CRC08-074 Ptg T-A 74 75 11CRC08-075 Ptg T-A 75 76 11CRC08-076 Ptg T-A

POSSIBLY GOETHITE/

3.5

3.0

2.5

2.0

1.5

1.0

0.5

0.0

11BCRC‐08 XRF %Cu

1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 37 39 41 43 45 47

Series1

Date post:	09-Apr-2022
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REDBANK COPPER LIMITED NORTHERN TERRITORY

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