ABM RESOURCES NL ABN 58 009 127 020 · ABM Resources – EL 23888, Stafford, Annual Report Y/E 11...

ABM RESOURCES NL

ABN 58 009 127 020

SIXTH

ANNUAL REPORT

EL 23888 ‘Stafford’

From the 12 August 2009 to 11 August 2010

REYNOLDS RANGE PROJECT

Holder ABM Resources NL Operators ABM Resources NL, Deep Yellow Ltd Author J Rohde Date August 2010 Email joe @abmresources.com.au Target Commodity Gold, Uranium Datum/Zone GDA94/ MGA Zone 53 250,000 mapsheet Napperby 100,000 mapsheet Reynolds Range

Distribution: ο NT DoR - digital ο Central Land Council digital ο Deep Yellow Ltd - digital File: jr13 DoR AR2010_Stafford

CONTENTS Page

1. Summary ...................................................................................................................................1 2. Introduction...............................................................................................................................1 3. Tenure........................................................................................................................................2 4. Geology .................................................................................................................................... 2 5. Previous Exploration................................................................................................................3 6. Exploration Completed in Year Six ........................................................................................4 6.1 Surface Sampling ........................................................................................................4 6.2 Drilling ..........................................................................................................................5 7. Bibliography..............................................................................................................................6 TABLES Table 1 Exploration Summary Table 2 Tenement Details Table 3: Exploration Summary for the second year (12 Aug 05 to 11 Aug 06) Table 4 Surface Sampling Details Table 5 Drill Hole Details FIGURES Figure 1 Tenement Location 1 : 1,000,000 Figure 2 Tenement Locality 1 :250,000 PLATES Plate 1 Drill Hole & Surface Sampling Locations over Interpreted Geology and Prospect

Locations 1 : 100,000 APPENDICES FILE DESC EL23888_01_2010_A_DrillCollars Drillhole collar coordinates EL23888_02_2010_A_Lithology Downhole Lithology EL23888_03_2010_A_DHAssay Downhole Samples and Assays

EL23888_04_2010_A_Surv Downhole Survey EL23888_05_2010_A_DHSamp Downhole Weathering EL23888_07_2010_A_Alteration Downhole Alteration EL23888_08_2010_A_Magsusc Downhole Magnetic Susceptibility EL23888_09_2010_A_Vein Downhole Veining EL23888_10_2010_A_Struc Downhole Structural EL23888_11_2010_A_Minerals Downhole Mineralisation EL23888_12_2010_A_SSAssay Surface Sampling Assays EL23888_13_2010_A_SSamp Surface Sampling Coordinates, Lithology

ABM Resources – EL 23888, Stafford, Annual Report Y/E 11 August 2010 1

1.0 SUMMARY EL 23888 was originally granted to Newmont Australia Pty Ltd (Newmont) on 12 August 2004. On 19 December 2006, EL 23888 was transferred to Tanami Exploration NL (TENL) who explored the tenement as part of their Reynolds Range Project area, where TENL identified the potential for quartz-vein-hosted gold mineralisation in the Proterozoic basement rocks. In 2008 TENL introduced a third party, Deep Yellow Limited (DYL) to explore the tenement for the potential of uranium mineralisation. In December 2009, ABM Resources NL (ABM) purchased EL 23888 from TGNL. ABM explores the tenement for the potential of gold mineralisation. EL 23888 lies in Central Australia centred approximately 220 kilometres north-northwest of Alice Springs (Figure 1). It is situated in the central part of the Aileron Province of the Arunta Region. All exploration on EL 23888 during the sixth year of term was carried out by ABM. It included surface sampling as well as RC and diamond drilling. A summary of exploration is listed in Table 1. Table 1 Exploration Summary Exploration Activity Details Rock Chip Sampling 8 samples Termite Hill Sampling 1 sample RC Drilling 4 holes, 1165 metres Diamond Drilling 4 holes, 1092.5 metres Significant surface sample (rock chip) assay results were returned from both the Pine Hill Prospect with a maximum value of 1.79 g/t Au (PH200004) as well as from the Reward Prospect with maximum value of 271g/t Ag (RW 200005) and a 20.30% Cu (RW200006) assay value. In 2010 RC and Diamond drilling tested targets of a high grade sediment hosted veins style along the Stafford Mineralised Zone. The results at the Sabre Prospect extend the mineralised zone to a width of more than 120 metres. Best intercepts were associated with sulphidic quartz veining in metamorphosed silt and sandstones (semipelite and psammite) and included 17meters @ 3.93g/t gold including 2 meters of 18.15g/t Au came from the Sabre Prospect. At the Falchion Prospect the best intersection returned 29m at 2.32g/t Au and 32m at 1.84 g/t Au also in conjunction with quartz veins hosted within metamorphosed sandstone. The one RC hole drilled at the Assegai prospect returned no significant intercepts. 2.0 INTRODUCTION EL 23888 is explored as part of ABM Reynolds Range project and DYL’s Reynolds Range uranium project. EL 23888 is located approximately 220 kilometres north-northwest of Alice Springs (Figure 1). The licence area lies within the Napperby, and Reynolds Range map sheets and is situated about 300 km southeast of the Granites mine. Access to the Reynolds Range project area is via the Tanami Road, and then via an unsealed tracks from Yuendumu. Various station tracks provide further access throughout the licence area. The Lander River truncates the tenement.

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SANDOVER

PLENTY

1 : 1,000,000

kilometres

0 20 40 60

MGA Zone 53 (GDA94)

400 000 mE

23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S23º S

22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S22º S

300 000 mE

7 500 000 mN

7 400 000 mN

J. Rohde Sep 2010 B.Mastaglia

133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E133º 30" E

DATE:

REYNOLDS RANGE

PLAN No:

ORIGINATOR: DRAWN:

EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888EL 23888

Narwietooma

e Camp

Glen Helen

Hamilton Downs

Alice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice Springs

Narwietooma

e Camp

Glen Helen

Hamilton Downs

Alice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice SpringsAlice Springs

Stirling

Anningie

Coniston

Pine Hill

Napperby

Aileron

Bond Springs

Jay Creek Native Settlement

EL 23888TENEMENT LOCATION

RR_1_0_001FIGURE 1

ABM RESOURCES NL

ABMRESOURCES NL


This report covers all exploration carried out for the year ending 11 August 2010 – the sixth year of tenure. Only ABM undertook exploration during the sixth year of tenure. 3.0 TENURE EL 23888 was granted over an area of 149 blocks to Newmont Gold Exploration Pty Ltd (Newmont). TENL entered into an option agreement with Newmont on 28 May 2004. On 19 December 2006, 100% ownership of EL 23888 was transferred to TENL. In 2008, TENL introduced a third party, DYL, which had the right to explore for uranium within EL 23888. At the end of the third year of term, EL23888 was reduced to 75 blocks. The licence area was further reduced to 56 blocks at the end of the fourth year of term. A waiver from the requirement to relinquish ground at the end of the fifth year of term had been approved by DRDPIFR. In December 2009, ABM purchased EL 23888 from TGNL. The current tenement area is shown in Figure 2, with tenement details shown below in Table 2. On the 2nd of June 2010 an application of for the extension of term was lodged. The renewal of the term is currently pending. Table 2: Tenement Details

Tenement No

Tenement Name

Blocks Granted

Current Blocks

Grant Date Expiry Date

EL 23888 Stafford 149 56 12 Aug 04 11 Aug 10, renewal pending

In the first year of tenure, an Indigenous Land Use Agreement covering EL 23888 was negotiated by TENL with the Central Land Council on behalf of the traditional owners. That ILUA excluded exploration for uranium requiring DYL to negotiate a further agreement with the CLC. 4.0 GEOLOGY AND MINERALISATION The Reynolds Range Project covers Palaeoproterozoic metasediments and intrusives in the central Aileron Province of the Arunta region. The surface geology has been mapped and described by the Northern Territory Geological Survey (NTGS) in the 1:250,000 scale Napperby (SF53-09) sheet and in more detail by the Bureau of Mineral Resources on the special edition Reynolds Range Region 1:100,000 scale geological map. The tenement is interpreted to be underlain by a minor degree of Dolerite (P-OD) and Granite (Pgn - low magnetic / mod-high magnetic) and the majority of the tenement area is underlain by low medium – grained turbidites Lander Rock Beds; Pll) (Plate 1). Widespread gold anomalism was identified within greenschist-facies metasediments along the eastern side of the Reynolds Range in the early 1990’s. Gold is hosted by sulphidic quartz veins and has been interpreted to broadly correlate with gold mineralisation in the Tanami region. On a regional scale the area has a very complex geology with polydeformed Palaeoproterozoic Lander Group metasediments, which host gold mineralisation, intruded by numerous felsic and mafic intrusive phases and overlain by slightly younger siliciclastic metasediments, including the Reynolds Range

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132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E132º 30' E

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REY

NO

LDS

RA

NG

E


280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE280 ooo mE


J. R

ohde

Sep

2010

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Group. The area is also covered by very complex regolith, with scree shedding from substantial hills cut by large drainage systems. Most of the gold mineralisation in the Reynolds Range Region appears to be concentrated along a relatively narrow corridor of greenschist facies Lander Rock Formation metaturbidites. Where there is good exposure in the central northeastern part of the belt, in the vicinity of Troutbeck-Bowness, folding in the Lander beds has northwest-striking axes, plunge towards the southeast and verges towards the southwest with steep southwestern limbs and gently dipping northeastern limbs (English, 2006). The highest grade gold mineralisation is at the Sabre and Falchion prospects. A sharp increase in metamorphic grade occurs towards the northeast where granulite facies is encountered and these rocks have been named the Mt Stafford Formation. High grade intercepts do occur in rocks of higher metamorphic grade, such as the Black Knight Prospect, but in this case it appears to be associated with retrograde greenschist facies metamorphism. Gold mineralisation occurs in a number of different geological settings and with a number of different metal associations. 5.0 PREVIOUS EXPLORATION Exploration in the first year of tenure consisted of regional desktop studies, including geophysical and geological interpretations. The study confirmed that a major Trans-Tanami structural corridor which runs through the area hosts the known gold mineralisation. A review of the open file reports by Poseidon Gold, Normandy Exploration and Exodus minerals was completed for the Reynolds Range area. There are numerous untested anomalies (surface geochemical and geophysical) as well as prospects with economic grades and widths. Diamond and RC drilling was completed at Sabre, Falchion, Assegai and Yataghan, but only hammer RAB, blade RAB, vacuum or surface sampling elsewhere. A couple of historic Au-Cu mines (Reward, Pine Hill) are situated southeast of the Sabre-Falchion area (Plate 1). Gold is commonly associated with Sb, Pb and As. Geochemical sampling data obtained from Newmont and from open file reports were transferred to the TGNL database and validated. Diamond drillcore was also retrieved from Newmont’s Ivy camp and relogged. A number of brief reconnaissance trips were undertaken through the area, but the absence of comprehensive work area clearances limited these trips to logistical planning. During the final reconnaissance trip in the Reynolds Range area, previous drilling and grid lines, prospect mapping and sample sites were identified. A total of 24 rockchip samples were collected with some encouraging results:

• RRK004 1494ppb Au, 190ppm As, 10ppm Cu and • RRK009 7775ppb Au, 668 ppm As, 25 ppm Cu from the Sabre area and • RRK023 12,149 ppb Au, 44 ppm As, 1176 ppm Bi and 5405 ppm Cu from a known

prospect ca 1.1 kilometers southwest of Sabre. In the second year of tenure exploration included geological and regolith mapping and interpretation, rock chip and vegetation sampling, RAB, Aircore and SLRC drilling in two drilling phases. The activities details and the results are described in the second annual report in Rohde, C., 2006. An exploration summary is listed below in Table 3. Table 3: Exploration Summary for the second year (12 Aug 05 to 11 Aug 06)


Activety Details Geological and Regolith Mapping / Interpretation 1:100,000 map Rock Chip Sampling 66 samples Vegetation Sampling 29 samples RAB Drilling 76 holes, 2,570 metres Aircore Drilling 16 holes, 863 metres SLRC Drilling 42 holes, 2,220 metres

Significant rock chip results were returned from the known Falchion mineralization with a maximum value of 11.5 ppm. Results of vegetation sampling highlighted detectable concentrations of various metals, including Au. In 2005 RAB, Aircore and slimline RC drilling was completed testing three regional targets and three advanced targets, Falchion, Sabre and Yataghan South. In 2006 RAB drilling was on untested Lander beds south and parallel to Sabre and Falchion. At Falchion the width and tenor of previously identified mineralisation was confirmed, including an intercept of 14m at 3.8g/t Au from 5m (RRA009). Step-out drilling also extended the known mineralised structure along strike in both directions, with intercepts of 4m at 1.5g/t Au from 40m depth (RRA011) over 50 metres to the east, and 4m at 0.5g/t Au from 44m depth (RRB2326) over 100 metres to the northwest. At Yataghan South infill drilling established the main structural orientation and confirmed continuity of previously recognised mineralisation, returning a best result of 20m at 0.5g/t Au from 16m which included 4m at 1.2g/t Au from 20m depth (RRN026). The drilling at Sabre was disappointing with only moderate anomalism returned from the traverse across the interpreted fold hinge and further west across the interpreted opposing limb to the main Sabre mineralisation. In the third year of tenure no field work was conducted. In the fourth year of tenure, TENL introduced a third party, DYL, to the project to assist with exploration funding. DYL carried out a reconnaissance trip to investigate access to the tenement area. No field work was carried out. In the fifth year of tenure exploration was carried out by DYL and comprehended three reconnaissance trips field trips and a night time thermal infrared data interpretation. The field trips and the night time thermal infrared data interpretation resulted in the identification of two east west trending palaeo-ponds, which did not have apparent direct surface expressions of buried paleochannels. 6.0 EXPLORATION COMPLETED IN YEAR SIX 6.1 Surface Sampling A total of eight rock chip samples and one Termite Hill Sample were collected at the Reward and Pine Hill Prospect on EL 23888. All rock chip samples were collected from lose rock or rock float material at surface and were associated with historic workings targeting Breccia hosted mineralization. The samples were submitted to ALS Chemex Ltd. in Alice Spring for preparation and were than send to ALS


Chemex Perth for multi-element analyses. Fire assaying and the ICP-AES method was used to analyse the samples for gold. Silver and base metals the samples were assayed using a 4-acid ICP-MS / ICP-AES method. Sample locations are shown on Plate 1 while all sample and assay data are listed in the digital Appendix. Details are also shown below in Table 4. Table 4 Surface Sampling Details

Sample ID

Prospect Locality

Sample Type

Coordinates MGA94 53

East

Coordinates MGA94 53

North

Gold (g/t)

Silver (g/t)

Copper (%)

Lead (%)

Zinc (%)

FL600001 Falchion

Termite Hill 263458 7459644 0.014 0.15

FL200001 Falchion

Rock chip 263458 7549628 0.007

BY200002 Bayonet Rock chip 264059 7548635 0.003

BY200003 Bayonet Rock chip 264059 7548625 0.002

RW200005 Reward Rock chip 275253 7545114 0.55 271.0 17.80 0.13 0.32


RW200007 Reward Rock chip 275238 7545099 0.20 14.9 0.15 0.23 -


PH200004 Pine Hill Rock chip 272542 7544462 1.79 0.3 0.37 0.07 -

6.2 Drilling In April, May and June 2010 a total of four RC holes fore 1165 meters and four Diamond holes for 1092.5 meters were completed, testing the possible extensions of mineralized zones (quartz veins) in fresh rock beneath previously identified regolith anomalies. All hole intervals drilled with Reverse Circulation were sampled with 1m composite samples. All samples were prepared and analysed by ALS Chemex in Alice Springs and Perth with Fire Assay using a 30g charge. Standards and blanks were inserted into the sample stream to monitor laboratory performance. All four diamond holes were pre-collared with RC and where finished with a NQ core tail. The RC section was sampled as 1m interval samples. All cores were cut in half and sampled in 2m intervals or 1m intervals respectively were it was of geological significance. All samples were submitted to ALS Chemex in Alice Springs and analysed in ALS Chemex’s Perth laboratory for gold and multi element analysis. The remainder of the core is stored at ABM’s office in Alice Springs. Drill hole locations are shown on Plate 1 and all drill hole and assay data is included in the digital appendix. Table 5 Drill Hole Details.


Hole ID

Prospect Location

Type of Drilling

Reverse Circulation

Interval (metres)

Diamond Core Interval

(metres) Total Depth

(metres) AS100001 Assegai RC 0 to 298 298 SB100002 Sabre DDH 0 to 57 57 to 207.6 207.6 SB100003 Sabre DDH 0 to 66 66 to 279.6 279.6 FL100004 Falchion DDH 0 to 23 23 to 274.7 274.7 FL100005 Falchion DDH 0 to 0.4 0.4 to 330.6 330.6 YG100006 Yagathan RC 0 to 295 295 SB100007 Sabre RC 0 to 280 280 SB100008 Sabre RC 0 to 292 292

The results at the Sabre Prospect extend the mineralised zone to width of more than 120 metres. Best intercepts (associated with sulphidic quartz veining hosted in metamorphosed silt and sandstones) included 17meters @ 3.93g/t gold including 2 meters of 18.15g/t Au came from the Sabre Prospect. At the Falchion Prospect the best intersection returned 29m at 2.32g/t Au and 32m at 1.84 g/t Au also in conjunction with quartz veins hosted metamorphosed sandstone. The one RC hole drilled at the Assegai prospect returned no significant intercepts. 7.0 BIBLIOGRAPHY Ding, P. & James, P.R., 1985. Structural evolution of the Harts Range area and its implications for the development of the Arunta Block, Central Australia. Precambrian Research, 27, 251-276. Ding, Puquan, 2001. Pre-Cenozoic solid geology map of the Strangways Range to Harts Range area, Explanatory Note. Unpublished TGNL in-house report. English, L.T.P., 2006. Reynolds Range Project, Northern Territory, Drilling Completion Report. Tanami Exploration NL internal report. Menzies, J., 2009 EL 23655 Lander JV Exploration Summary June 2008 to March 2009. Unpublished report by Deep Yellow Ltd. Robinson, S. 2006. Reynolds Range Drilling Report 2005. Tanami Exploration NL internal report. Rohde, C., 2004. First Combined Annual Report EL’s 9814, 22387, 23483 and 23486 Napperby Project for the Year Ending 3 March 2004. Unpublished Tanami Gold NL In-house report. Rohde, C., 2005. Second Combined Annual Report EL’s 9814, 22387, 23483 and 23486 Napperby Project for the Year Ending 3 March 2005. Unpublished Tanami Gold NL In-house report. Rohde, C., 2005. First Combined Annual Report on Exploration Licences 23486, 23923, 23924 and 23991 Reynolds Range Project for the year ending 31 May 2005. Unpublished report by Tanami Exploration NL.


Rohde, C., 2005. First Annual Report EL 23888 Stafford, Reynolds Range. Unpublished report by Tanami Exploration NL. Rohde, C., 2006. Second Annual Report EL 23888 Stafford, Reynolds Range Project, for the year ending 11 August 2006. Unpublished report by Tanami Exploration NL. Rohde, J., 2006. Fifth Annual Report EL 23888 Stafford, Reynolds Range Project, for the year ending 11 August 2009. Unpublished report by Tanami Exploration NL. Stamoulis, V., 2009. Night-Time Thermal Infrared Data Interpretation Part 1, Deep Yellow Limited Exploration Licences 23655, 23888, 23991, 23923 and 23924. Reynolds Range Project, N.T. Unpublished report by Chrysoar Exploration for Deep Yellow Limited.

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YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006YGRC100006




FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005FLDD100005

FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004FLRCD100004


ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001ASRC100001

YataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghanYataghan

Sabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre NorthSabre North

SabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabreSabre

Black KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack KnightBlack Knight

ClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymoreClaymore

AssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegaiAssegai

ScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarScimitarFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchionFalchion

Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1Trout1

Yataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan SouthYataghan South

Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)Pine Hill (Au, Cu)

Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1Rapier M1

Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7Rapier M7

Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)Reward (Cu,Pb,Zn)

Red Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle eastRed Hackle east

BownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBownessBowness

Tin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomalyTin Bore drainage anomaly

Anzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault ZoneAnzac Dam Fault Zone

Coniston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin WorkingsConiston Tin Workings

Mt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin WorkingsMt Stafford Tin Workings

AurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAurariaAuraria

Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2Trout2

Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)Unknownn (Cu,Pb,Zn)

Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)Lander (Cu)

Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)Ingellina Gap (W)

Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)Coniston Alluvials (Sn)

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Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2Un-named 2

Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3Un-named 3

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VIC

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NT

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ACT

TAS

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EL 23888Drill Hole & Surface Sampling Locations

over Interpreted Geology and Prospect Locations

PLATE 1RR_2_001

Gneiss - undifferentiated ortho+/-paragneiss (P-MG)

Granulite facies meta-turbidites (Mt Stafford Beds; Pls)

Mafic and felsic granulite (Tyson Creek Granulite andWeldon Metamorphics; Pt/e)

Retrograde greenschist facies rock (Pzr)

Medium-grained turbidites (Lander Rock Beds; Pll)

Metacarbonate rocks (Reynolds Range Group; Po/Pra)

Basal conglomeratic quartzite and metasediments (Reynolds Range Group; Prt/p)

Granite - low magnetic/mod-high magnetic (Pgn/Pgm)

Platform cover sandstone-dominated sequence (Ps)

Unconformity

Dolerite (P-OD)

Reynolds Range Geology LegendStratigraphic Unit in brackets

Fold axesPrimary Fault

Magnetic trend linesPhoto/Landsat trend lines

Secondary Fault

Slip DirectionTertiary Fault

Unconformity

Schistose Unit (P-MS)

Legend

Drillhole

ROCK Sample

ABM RESOURCES NL ABN 58 009 127 020 · ABM Resources – EL 23888, Stafford, Annual Report Y/E 11...

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