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Ashley, P. M. (1975): Opaque mineral assemblage formed during serpentinization in the Coolac ultramafic belt, New South Wales. Journal of the Geological Society of Australia 22, 91-102.

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Year1975
Original EntryAshley, P. M. (1975): Opaque mineral assemblage formed during serpentinization in the Coolac ultramafic belt, New South Wales. Journal of the Geological Society of Australia 22, 91-102.
Mindat Ref. ID16028509Long-form Identifiermindat:1:5:16028509:9
GUID44003fa8-8083-4d4b-9c52-0b4e9d0a6f16
Full ReferenceAshley, P. M. (1975): Opaque mineral assemblage formed during serpentinization in the Coolac ultramafic belt, New South Wales. Journal of the Geological Society of Australia 22, 91-102.
Plain TextAshley, P. M. (1975): Opaque mineral assemblage formed during serpentinization in the Coolac ultramafic belt, New South Wales. Journal of the Geological Society of Australia 22, 91-102.

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LocalityCitation Details
Serpentinite occurrence, Coolac, Harden Co., New South Wales, Australia

Mineral Occurrences

LocalityMineral(s)
Serpentinite occurrence, Coolac, Harden Co., New South Wales, Australiaⓘ Awaruite, ⓘ Clinopyroxene Subgroup, ⓘ Fayalite-Forsterite Series, ⓘ Heazlewoodite, ⓘ Mackinawite, ⓘ Magnetite, ⓘ Millerite, ⓘ Orthopyroxene Subgroup, ⓘ Pentlandite, ⓘ Pyrrhotite, ⓘ Spinel, ⓘ Violarite

See Also

These are possibly similar items as determined by title/reference text matching only.

Ashley, P. M. (1975) Opaque mineral assemblage formed during serpentinization in the Coolac ultramafic belt, New South Wales. Journal of the Geological Society of Australia, 22 (1) 91-102 doi:10.1080/00167617408728877
Ashley, PaulM. (1973) Petrogenesis of sulphide-bearing reaction zones in the Coolac ultramafic belt, New South Wales, Australia. Mineralium Deposita, 8 (4) doi:10.1007/bf00207518
Ashley, P. M., Franklin, B. J., Ray, A. S. (1983) Plagiogranites in the Coolac ophiolite suite, New South Wales, Australia. Geological Magazine, 120 (1) 1-20 doi:10.1017/s0016756800024997
Ashley, P. M. (1974) Stratabound pyritic sulphide occurrences in an ophiolite rock assemblage near Tumut, New South Wales. Journal of the Geological Society of Australia, 21 (1) 53-62 doi:10.1080/00167617408728833
Golding, H. G., Bayliss, P. (1968) Altered chrome ores from the Coolac Serpentine Belt, New South Wales, Australia. American Mineralogist, 53 (1-2) 162-183
Ashley, P. M., Creelman, R. A. (1975) The mount black lead‐zinc deposit, a probable Mississippi valley‐type sulphide occurrence at cooleman plains, southern New South Wales. Journal of the Geological Society of Australia, 22 (4) 423-433 doi:10.1080/00167617508728908
Brown, P.F. (1979) A sheeted dyke complex within the Coolac Ophiolite, southeastern New South Wales. Journal of the Geological Society of Australia, 26 (7) 411-417 doi:10.1080/00167617908729107
Leitch, Evan C. (1975) Zonation of low grade regional metamorphic rocks, Nambucca slate belt, northeastern New South Wales. Journal of the Geological Society of Australia, 22 (4) 413-422 doi:10.1080/00167617508728907
MacNevin, A.A. (1975) Woolomin-Texas Block: Great Serpentinite Belt. In Markham N.L. & Basden H. eds. The Mineral Deposits of New South Wales, Geological Survey of New South Wales, Sydney. pp. 393-403.
Golding, H. G. (1975) Relict textures of chromitites from New South Wales. Journal of the Geological Society of Australia, 22 (4) 397-412 doi:10.1080/00167617508728906
MacNevin, A.A. (1975) Woolomin - Texas Block: Great Serpentinite Belt. In Markham N.L. & Basden H. eds. The Mineral Deposits of New South Wales, Department of Mines, Geological Survey of New South Wales, pp. 393-403.
 
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