Meta Minerals — An Open-File Forensic Look at the Birdwood Cu-Mo System, EL 9090
"Some ground is judged by the assays that were run. Better ground is judged by the assays that weren't."
The Birdwood field, 35 miles east of Wauchope in the upper Hastings of northern New South Wales, is now held under Exploration Licence 9090 by Meta Minerals Pty Ltd (ACN 634 190 060). It sits in the western Hastings Block of the southern New England Orogen — Lower Devonian to Lower Permian shales, greywackes, sandstones and tuffs, intruded by an Upper Permian Trondhjemite stock that has hornfelsed a belt roughly one mile wide around its outcrop, and by a north-trending corridor of Lower Permian alpine-type ultramafics that runs from Port Macquarie to Birdwood parallel to the Hastings River Valley.
Unlike a goldfield, Birdwood has no production history. What it has instead is something rarer: nine diamond drill holes for 7,704 feet (2,348 m), drilled 1968–69, whose complete logs and assay sheets survive, and whose core still sits in the racks at Londonderry. That core survives by a margin of days — a point we return to below.
The system is a fracture-controlled copper-molybdenum-silver system in hornfels, sourced from the late stages of the Trondhjemite intrusion. It was tested once, by one operator, against one anomaly, under one commodity model, and then abandoned. The operator's own conclusion — "uneconomic mineralisation associated with fracturing in hornfels" — has stood unchallenged for fifty-five years.
Reading the raw assay sheets rather than the summary produces a different picture. Eight of nine holes stopped above 307 metres. Three ended in mineralisation. Two of the field's three soil anomalies were never drilled at all. Molybdenum was assayed to 6,250 ppm and never pursued. Gold was assayed on four of roughly five hundred surface samples. And the single best copper interval in the field does not appear anywhere in the company's summary — it emerges only from recomputing the raw sheet.
2. Exploration History — One Era, One Operator at a Time
1966: Placer Explorations (EL 189)Regional stream-sediment sampling across the Hastings, including ground later covered by MEL 636. Placer "did not find that the survey warranted further investigation and so relinquished the area without further work" (per GS1970/300). Departure on a reconnaissance-threshold call, at a time when a single-element stream survey was the entire screening toolkit.
1968–70: Pickands Mather & Co. International (EL 130 → EL 198)The field's only substantive campaign, and the source of everything that matters. EL 130 (ELA 273) held 18 July 1968 to 18 July 1969 over 174 square miles; halved and re-granted as EL 198 (ELA 613) from 23 July 1969; a six-month extension on 23 July 1970 cut it to 13 square miles; relinquished 10 September 1970.
Work completed: regional stream sampling; a cut and chained grid with an 18,500-foot main baseline, crosslines every 500 feet (250 feet over anomalous ground), 55 line miles total; soil sampling at 100-foot spacing; full geological mapping; a magnetometer survey at 50-foot stations; induced polarisation by both dipole-dipole and time-domain gradient array; and nine diamond holes for 7,704 feet, all reported as targeting the northern anomaly.
Departure was on grade against a fracture-controlled model at 1969–70 copper prices, by a company whose core business was iron ore. Final report filed by R.R. Schellekens, 1 March 1971.
1970–71: Pickands Mather (H.K. Herbert) — platinum appraisalA separate program over the ultramafic belt, October–December 1970, reported April 1971 (GS1971/475). Seven soil grids, A through G, at 200-foot line spacing and 50-foot stations. Serpentinite bodies located partly by "stands of 'black-boy' trees, specific geobotanical indicators for serpentinite in the area." Conclusion: "the Pt potential of the area is considered minimal." Departure on the absence of visible chromite concentrations and sulphide segregations — the accepted proxies of the day.
1969–70: Bundarra Tin Pty Ltd (MEL 636 — I.R. Plimer, D.N. Camiller)Reconnaissance stream-sediment and geological survey over 200 square miles adjoining to the south and west (GS1970/300). 180 wet-sieved −80-mesh samples, assayed Ni-Cu-Zn by AAS at Minex Laboratories to ±15% relative accuracy. Explicitly budget-constrained: "The cost of adequately covering the exploration licence area would have been in the order of ten thousand dollars ($10000) and so to keep costs to approximately two thousand dollars ($2000) it was necessary to select areas thought to be most favourable." Cobalt, lead and silver were deliberately omitted; heavy-mineral analyses for platinoids and chromite "were not conducted because of insufficient time."
1980–82: Theiss Bros. Pty Ltd / CSR (EL 1219, Tinebank)Stream-sediment programs on a tin-tungsten model. The 1980 batch (R00015894, 28 samples) assayed Cu-Pb-Zn-Ag-Mo; the 1982 batch (R00014994, 79 samples) assayed As-Cu-Pb-Sn-W-Zn. Arsenic to 300 ppm, tin to 55 ppm. No gold assays in either batch.
1982: CRA Exploration Pty Ltd (EL 1450 / EL 1468, Pappinbarra)158 stream sediments plus 5 other samples (R00012678, R00012680). Copper to 960 ppm, zinc to 320 ppm. Gold was assayed on four samples only, all below detection. Relinquished without follow-up.
July 1971: the core rescueOn 5 July 1971 Pickands Mather wrote to the Chief Inspector of Mines: "We have stored at Birdwood, diamond drill cores from nine holes drilled during prospecting operations, under E.L. 198... Unless otherwise advised by you, we intend to dispose of this core in two weeks." A handwritten annotation dated 12 July 1971 directs the core to Londonderry. A hand-written note on the report's final page records the location — "Core stored at Birdwood at the farm of Geoff Harris. Ask at Birdwood P.O." — and a tally dated 15 July 1971: B105, B103, B101, B102 and B104 collected, 3,589 feet, 173 boxes, other holes to be collected later. The entire modern dataset over this field descends from a departmental officer answering that letter inside seven days.
1994–1999: institutional re-samplingThe University of Technology Sydney sampled B108 and B109 on 22 December 1994. The NSW Department of Mineral Resources assayed B102 and B103 core on 15 May 1999 (GSNSW core library records). Results for neither program appear in the open-file material reviewed.
2007: Anchor Resources LimitedCore inspection and sampling at Londonderry (fax of 5 July 2007; sampling sheet of 11 July 2007), covering B103 and B108, with thin sections taken from B108 as AHR PET 001–006.
2014: Anchor Resources Limited (EL 6459, "Birdwood Project")On 11–12 February 2014, 246 handheld-XRF spot analyses on half core across six of the nine holes — B101 (38), B102 (49), B103 (27), B105 (37), B108 (50), B109 (45) — using a Niton XL3t in TestAll Geo mode at 80-second duration, reported to the Department in the DG1 template. Semi-quantitative, and readings are on core surfaces rather than prepared pulps. The program was not followed by any lab re-assay identified in the open file.
2021–present: Meta Minerals Pty LtdEL 9090 (Act 1992) granted 15 March 2021 in satisfaction of ELA 5989, over 62 units for Group 1 minerals, with low-impact conditions. Varied to standard prospecting operations on 28 September 2021 on application of 13 August 2021 (AMP17 Notice of Variation) — the licence ceased to be low-impact. Renewed 1 May 2024, current to 15 March 2027. This chapter puts the field in the hands of a single holder with an intact core library, a complete assay archive, and three untested anomalies on the same grid.
3. Why this didn't progress in 1970
Cross-referencing the eras shows the same pattern as any under-tested system: each generation tested one slice, and no two slices overlap enough to close the question.
The Depth Axis is UntestedEight of the nine holes bottomed at or above 307 metres. Only B106 went deeper, to 1527 feet 4 inches (465.5 m). Three holes ended with the rocks still talking: B106 returned 7 feet at 0.52% Cu from 1268 feet (386.5 m) and then ran a further 250 feet before stopping; B108's 5-foot-3-inch interval at 1.0% Cu with 11 ppm Ag sits just 48 feet above end of hole; and B101's final assay of the hole, 1000–1005 feet, reads 470 ppm Cu with 375 ppm Mo. No downhole geophysics of any kind — no DHEM, no downhole IP, no televiewer — appears anywhere in the record for any of the nine holes.
The Anomaly Axis is Two-Thirds UnopenedSoil sampling defined three separate anomalies on the Birdwood grid. All nine holes were reported as testing one of them.
Northern — 800,000 square feet, soils to 2,200 ppm Cu and 132 ppm Mo, magnetics erratic across an 8,000-gamma range (+5,000 to −3,000 against −400 background), read as pyrrhotite. Drilled.
Western — soils to 1.0% Cu with 5 ppm Mo, flat magnetic profiles, low-to-medium dipole-dipole IP response; a granitic dyke at 5500W 4800S on Kindee Creek rock-chipped 0.7% Cu. The report states plainly: "No drilling was undertaken in the area."
Southern — a +400 ppm Cu envelope over 1.6 million square feet with a core zone 1,500 × 200 feet, soils to 0.55% Cu, no anomalous molybdenum; one 50-foot-dipole IP line across L. Steep's vein lease returned frequency effects of 7–8%. The report states: "No drilling was attempted in the area of the southern anomaly."
A fourth anomaly, Boss Creek — 50 ppm CxCu, 150 ppm Cu, 600 ppm Zn in stream sediment — was found in the initial reconnaissance and never revisited by anyone: "No follow-up work was done in this area as all the work was concentrated at Birdwood."
The Geometry Axis Needs ReconcilingThe final report states that "most of the geophysical surveys and all of the diamond drilling was concentrated on the northern anomaly." The collar coordinates on the logs do not obviously agree: they range from 2950'N to 2000'S and from 1300'E to 2250'W — roughly 5,000 feet north-south and 3,500 feet east-west — against a northern anomaly of 800,000 square feet, or about 900 feet square. Either the logs use more than one local grid origin, or the summary statement is a simplification. Any modern re-modelling of this field must resolve collar positions before it resolves anything else. [Reconciliation item — see flag list]
The Molybdenum Axis Was Measured and DiscardedMolybdenum sits in the assay column beside the copper on every sheet, and reaches grades nobody chased. B107 returned 6,250 ppm Mo (0.625%) with 17 ppm Ag over 3 feet 7 inches from 500 feet, and 2,500 ppm Mo at 375 feet 4 inches. B101 returned 1,000 ppm Mo at 211 feet 9 inches, 500 ppm at 326 feet 9 inches, 450 ppm at 790 feet, and 375 ppm in its final sample. B102 carries 500 ppm intervals at 46–64 feet, 400 ppm at 345 feet and 300 ppm at 479 feet. The field's mineralogy — quartz-molybdenite veins of a demonstrably younger stage than the copper — was described in detail and never targeted, because molybdenum in 1969 was a smelter by-product, not a reason to drill.
The Gold Axis is Essentially Blank Across roughly 500 stream-sediment samples filed over this ground between 1966 and 1982, gold was assayed on four — CRA's, in 1982, all below detection. In core the coverage is barely better: B103's sheet carries an Au column with three entries reading "TR" and one reading ".05" with units unstated, across 180–222 feet; B105 carries a single mark at 465–470 feet. That is the entire gold dataset for the Birdwood field.
This matters because the loggers recorded gold's classic pathfinder assemblage without ever testing for it. B104 logs arsenopyrite and marcasite through the 85–140-foot interval; B109 logs pyrite-arsenopyrite veins at 43 feet 5 inches to 45 feet 7 inches. Both holes were assayed for Cu, Ag and Mo only.
The Sampling-Support Axis is Selective Assaying was concentrated around logged sulphide, not run continuously. B108's log carries detailed lithology and mineralised-zone marks from surface to 370 feet with the assay columns blank throughout; comparable unassayed runs appear in B106 and B109. The operator's conclusion that copper averaged 300–500 ppm across the holes is therefore a statement about the intervals selected for assay, not about the holes.
The PGE Axis Was Closed Without a MeasurementGS1971/475 is titled Platinum Investigations in the Birdwood Area and contains no platinum or palladium determination. Herbert assayed Cu, Ni, Co and Cr as proxies across grids A–G and logged outcrops visually for chromite. His own text is careful about this: "it is pertinent to note that no protore Pt accumulations have been discovered in the alpine serpentinites of northern New South Wales." Separately, one chip sample from the western edge of the serpentinite belt running north-east from Mt Jasper returned 1.0% Ni over 100 feet, and soils on the grids reached 0.6% Ni. Chromite pods have been mined historically at Kennedys Mountain.
Two Intercepts Were Never Headlined The company summary quotes exactly one number: "The best intersection was 52' of 0.62% Cu in DDH B-103 between 180' and 232'." Recomputing that interval from the raw sheet gives ~0.66% Cu. But the same sheet carries a note the summary omits: "N.B. True width of above section 189'-219'6" is approx. 10'." Recomputing 189 to 219 feet 6 inches returns 30.5 feet at 0.84% Cu, including 5 feet at 1.8% Cu and 5 feet at 1.0% Cu — at an estimated true width of about 10 feet (3.0 m). That is a materially better and materially narrower result than the one that has represented this field for fifty-five years, and it exists only on the raw sheet.
The second omission is B102. At 98 to 100 feet the logger recorded "50% chalcopyrite (or yellow sulphide); 10% calcite, 10% pyrrhotite, 30% quartz" and the assay returned 3.1% Cu with 90 ppm Ag — the highest copper assay in the field. It appears in no summary, no conclusion, and no subsequent report.
The 2014 XRF Independently Validates the 1969 AssaysAnchor's Niton readings are not free-floating. Every high-value spot falls inside an interval Pickands Mather assayed in a laboratory forty-five years earlier:
Anchor XRF spot (2014) | Pickands Mather assay (1968–69) |
B102 @ 30.18 m — 27.96% Cu, 453 ppm Ag | 98–100 ft (29.9–30.5 m): 3.1% Cu, 90 ppm Ag |
B108 @ 292.21 m — 27.89% Cu, 164 ppm Ag | 954'6"–959'9" (290.9–292.5 m): 1.0% Cu, 11 ppm Ag |
B103 @ 62.06 m — 14.57% Cu | 202–207 ft (61.6–63.1 m): 9,200 ppm Cu |
B101 @ 139.32 m — 14.63% Cu | 455–460 ft (138.7–140.2 m): 3,200 ppm Cu |
Four of four. The spot-to-interval ratio of 3× to 30× is exactly what a point analysis on a sulphide vein should return against a 5- to 10-foot composite. Two independent measurement systems, separated by forty-five years and a change of custody, agreeing in the manner the physics requires. Both datasets are sound, and neither has been superseded.
The historical Miss, Precisely
Birdwood was gridded across 55 line miles, geochemically anomalous in three separate places, and then tested by nine holes into one of them — eight of which stopped above 307 metres, three of which ended in mineralisation, all of which were assayed selectively for copper, silver and molybdenum and effectively never for gold, against a fracture-controlled model at a copper price that made 0.35% uneconomic and a molybdenum price that made 0.625% invisible. Every constraint that closed this field — the commodity deck, the assay suite, the depth budget, the single-anomaly focus — is a 1969 artifact. The core is in the racks at Londonderry. The assay sheets are in the open file. Both are resolvable at re-assay-and-desktop cost by the current holder.
4. Significant Intercepts
Historical results, not verified to JORC 2012, reproduced from open-file reports. Handheld-XRF readings are semi-quantitative spot analyses on core surfaces, not assays.
Hole | Operator (year) | Intercept | Source | Why It Matters |
B103 | Pickands Mather (1969) | 30.5 ft (9.3 m) @ 0.84% Cu from 189 ft (57.6 m), incl. 5 ft @ 1.8% Cu and 5 ft @ 1.0% Cu; true width noted ~10 ft (3.0 m) | R00025322 | Field's best copper. Emerges only from raw-sheet recomputation; never headlined |
B103 | Pickands Mather (1969) | 52 ft (15.8 m) @ 0.62% Cu from 180 ft — as filed; recomputes to ~0.66% | R00025322 | The single number the company summary quotes for the entire field |
B102 | Pickands Mather (1968) | 2 ft (0.6 m) @ 3.1% Cu, 90 ppm Ag from 98 ft (29.9 m) | R00025322 | Highest Cu assay in the field; logged "50% chalcopyrite"; absent from every summary |
B106 | Pickands Mather (1969) | 5 ft (1.5 m) @ 0.825% Cu, 15 ppm Ag from 485 ft (147.8 m) — logged "massive chalcopyrite band" | R00025322 | Second-highest Cu; in the field's deepest hole; never reported |
B106 | Pickands Mather (1969) | 7 ft (2.1 m) @ 0.52% Cu, 6 ppm Ag from 1268 ft (386.5 m) | R00025322 | Deepest good copper on the field; hole continued 250 ft and stopped |
B108 | Pickands Mather (1969) | 5 ft 3 in (1.6 m) @ 1.0% Cu, 11 ppm Ag from 954 ft 6 in (290.9 m) | R00025322 | 48 ft above end of hole; independently matched by 2014 XRF at 292.21 m |
B107 | Pickands Mather (1969) | 3 ft 7 in (1.1 m) @ 0.625% Mo, 17 ppm Ag from 500 ft (152.4 m) | R00025322 | Highest Mo in the field; a by-product metal in 1969, never pursued |
B101 | Pickands Mather (1968) | 20 ft (6.1 m) @ 0.35% Cu from 440 ft (134.1 m), incl. 5 ft @ 0.56% Cu | R00025322 | Best continuous Cu run; matched by 2014 XRF at 139.32 m |
B101 | Pickands Mather (1968) | 5 ft @ 470 ppm Cu, 375 ppm Mo from 1000 ft (304.8 m) | R00025322 | Final assay of the hole — ended in Cu-Mo |
B105 | Pickands Mather (1969) | 5 ft (1.5 m) @ 0.34% Cu, 5.1 ppm Ag from 320 ft (97.5 m) | R00025322 | Central grid; hole intersected Trondhjemite/granodiorite from 437 ft 6 in |
B104 | Pickands Mather (1969) | 5 ft (1.5 m) @ 0.44% Cu from 340 ft (103.6 m) | R00025322 | Arsenopyrite and marcasite logged in the same hole; no Au assay run |
B109 | Pickands Mather (1969) | 3 ft (0.9 m) @ 0.45% Cu from 263 ft 4 in (80.3 m) | R00025322 | Pyrite-arsenopyrite veins logged at 43 ft; no Au assay run |
Surface | Pickands Mather (1969) | Rock chip 0.7% Cu, granitic dyke, 5500W 4800S, Kindee Creek | R00025322 | Western anomaly — never drilled |
Surface | Pickands Mather (1969) | Soils to 1.0% Cu (western anomaly); 0.55% Cu (southern anomaly) | R00025322 | Neither anomaly drilled; southern IP returned 7–8% frequency effect |
Surface | Pickands Mather (1971) | Chip 1.0% Ni over 100 ft, west edge of serpentinite belt NE of Mt Jasper | GS1971/475 | Ultramafic belt; no Pt or Pd determination ever run on this ground |
Stream | Pickands Mather (1969) | 50 ppm CxCu, 1,250 ppm Cu, 40 ppm Mo — Maughans and Kindee Creeks | R00025322 | The anomaly that started the whole program |
Drilling metadata: B101 1005 ft (306.3 m), B102 503 ft 8 in (153.5 m), B103 500 ft (152.4 m), B104 902 ft 8 in (275.1 m), B105 653 ft 8 in (199.3 m), B106 1527 ft 4 in (465.5 m), B107 1003 ft (305.7 m), B108 1007 ft 2 in (307.0 m), B109 601 ft 8 in (183.4 m). Total 7,704 ft (2,348 m). All NQWL, all logged vertical except B109 (logged inconsistently — see flag list). Core held at Londonderry.
5. Geological Setting
Birdwood lies on the eastern edge of the New England Plateau, uplifted to 2,000–3,000 feet and deeply dissected, with local relief approaching 1,500 feet, slopes to 45°, and small rock cliffs on the steepest ground. Thick soil covers most of the area; bedrock cover thins to nothing on the steeper slopes. Weathering of the hornfels runs down joints to about 150 feet, but fresh rock is available at surface.
The host sequence is Lower Devonian to Lower Permian shale, greywacke, sandstone and tuff. An Upper Permian granitic suite — Trondhjemite, aplite and greisen — intrudes the eastern third of the licence area, with the Trondhjemite stock outcropping near the centre of the grid at "Hillview" on the Birdwood–Kindee track: a grey, medium-grained, porphyritic rock of plagioclase, quartz, biotite and hornblende. The sediments and tuffs are metamorphosed to hornfels in a belt approximately one mile wide surrounding that outcrop. Tertiary basalt and trachyte overlie the Palaeozoic sequence to the south.
Mineralisation is fracture- and vein-controlled, not replacement. Two stages are described: an older pyrrhotite-pyrite-chalcopyrite assemblage in quartz veins up to 2 inches wide and as fracture fillings down to 1/10 inch, and a younger pyrite-molybdenite stage in quartz veins up to 2 inches. Alteration is tight — silicification or bleaching confined to within 2–3 inches of quartz veins and ¼–1 inch of fractures. Disseminated sulphide in the hornfels is rare, and where present is associated with alteration adjacent to fracture fillings. Total sulphide content of the core averaged 0.5% by visual estimate; sulphur assays where run on B103 range 0.41% to 2.19%. The report attributes the mineralisation to the late stages of the Trondhjemite intrusion, while allowing that "some of the sulphides may be of syngenetic origin, and were remobilised during the emplacement of the granitic intrusion."
Separately, and structurally distinct, a corridor of Lower Permian alpine-type ultramafics — gabbro, amphibolite and serpentinite, the serpentinite occurring as sheared north-south pods carrying minor magnetite and chromite — runs through the western third of the licence area, from Grass Tree Creek in the north to Yarras Mountain in the south, and extends regionally from Port Macquarie parallel to the Hastings River Valley. Nickel in these bodies is bound in the magnetic fraction rather than in sulphide.
Three pre-existing occurrences are recorded within the licence area: Mt Jasper, 4 miles south-west of Birdwood, where a shallow shaft was sunk on quartz-chalcopyrite veins in serpentinite; Maughans Creek, one mile east, where quartz-molybdenite veins are visible in hornfels; and two mineralised copper-lead-zinc-silver aplite dykes within a mineral lease held by L. Steep near what became the southern end of the Birdwood grid.
6. Top 3 Targets
Target 1 — The Western and Southern Soil Anomalies (Data-Supported, Never Drilled)
Two of the three anomalies defined by Pickands Mather's own soil grid have never had a hole put in them. The western anomaly carries soils to 1.0% Cu and a 0.7% Cu rock chip from a granitic dyke; the southern carries a +400 ppm Cu envelope over 1.6 million square feet with a 1,500 × 200-foot core, soils to 0.55% Cu, and a 7–8% IP frequency effect over the L. Steep vein lease. Both were mapped as the same tuffaceous hornfels as the drilled northern anomaly. The 1970 comparison notes the western anomaly's flat magnetics and weaker IP as evidence of lower pyrrhotite content — which, in a copper-hunting context, was read as a negative, but says nothing about copper itself. This is the cheapest ground on the licence to move from historical anomaly to first-pass drill test, and it requires no new geochemistry to justify.
Target 2 — Depth Below the 1969 Floor (Conceptual)
Eight of nine holes stopped above 307 metres. The one hole that went deeper returned its best deep copper at 386–389 metres and then stopped. Two other holes ended in mineralisation, one with molybdenum rising in the final sample. No downhole geophysics has ever been run in any hole. The whole field, in other words, has been tested only to the depth that a 1968–69 rig program was budgeted to reach, against a model that expected fracture-controlled mineralisation to weaken with distance from surface — a model the deep B106 result does not obviously support. Re-entry of the surviving collars for downhole EM or IP is the lowest-cost way to establish whether anything sits below the drilled floor before committing to new metres.
Target 3 — Molybdenum and Gold as Primary Commodities (Data-Supported, Re-Assay Only)
This target requires no drilling at all. The core is at Londonderry, catalogued hole by hole, box by box. Molybdenum was assayed to 6,250 ppm and never followed; gold was effectively never assayed anywhere, in a system whose loggers recorded arsenopyrite and marcasite in two separate holes; silver reached 90 ppm in B102 and 17 ppm in B107 on a sparse suite; and long runs of core — including the top 370 feet of B108 — carry no assay at all. A systematic re-assay of the existing core on a modern multi-element suite, with proper sample support across the unassayed intervals, would test three commodity questions and one sampling question simultaneously, at a cost measured in laboratory invoices rather than rig days. The 2014 XRF work has already demonstrated that the core is intact, in place, and returning results consistent with the 1969 laboratory data.
Disclaimer
Not a JORC-compliant statement; historical results reported from open-file sources and not verified by a Competent Person. Handheld-XRF readings referenced above are semi-quantitative spot analyses on core surfaces, not assays. Recomputed intervals are derived by CAADIA Metals from raw open-file assay sheets and are not reported Mineral Resources.
All data sourced from publicly available NSW DIGS open-file records (GS1969/494 / R00025322; R00032578; R00032579; R00032580; R00029134; GS1971/475 / R00000891; GS1970/300 / R00023887; R00012678; R00012680; R00014994; R00015894), GSNSW drillhole and geochemistry databases, NSW titles instruments for EL 9090, and the Anchor Resources 2014 exploration data file for EL 6459.
CAADIA Metals has no interest in, and no commercial relationship with, Meta Minerals Pty Ltd; EL 9090 is wholly held by Meta Minerals Pty Ltd. Nothing in this article is a statement about the prospectivity of EL 9090 or of any adjoining tenement. Targets described are observations about gaps in the historical record and are working hypotheses requiring testing.
This article is general information only and not investment advice.
