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Allibone, A, Ashley, P, MacKenzie, D, Craw, D (2010) Shear-hosted base metal mineralisation at the Dana Peaks, Murchison Mountains, Fiordland, New Zealand. New Zealand Journal of Geology and Geophysics, 53 (4) 271-294 doi:10.1080/00288306.2010.498406

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Reference TypeJournal (article/letter/editorial)
TitleShear-hosted base metal mineralisation at the Dana Peaks, Murchison Mountains, Fiordland, New Zealand
JournalNew Zealand Journal of Geology and Geophysics
AuthorsAllibone, AAuthor
Ashley, PAuthor
MacKenzie, DAuthor
Craw, DAuthor
Year2010 (December)Volume53
Issue4
PublisherInforma UK Limited
DOIdoi:10.1080/00288306.2010.498406Search in ResearchGate
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Mindat Ref. ID259097Long-form Identifiermindat:1:5:259097:8
GUID0
Full ReferenceAllibone, A, Ashley, P, MacKenzie, D, Craw, D (2010) Shear-hosted base metal mineralisation at the Dana Peaks, Murchison Mountains, Fiordland, New Zealand. New Zealand Journal of Geology and Geophysics, 53 (4) 271-294 doi:10.1080/00288306.2010.498406
Plain TextAllibone, A, Ashley, P, MacKenzie, D, Craw, D (2010) Shear-hosted base metal mineralisation at the Dana Peaks, Murchison Mountains, Fiordland, New Zealand. New Zealand Journal of Geology and Geophysics, 53 (4) 271-294 doi:10.1080/00288306.2010.498406
In(2010, December) New Zealand Journal of Geology and Geophysics Vol. 53 (4) Informa UK Limited

See Also

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Allibone, AH, MacKenzie, D, Turnbull, R, Tulloch, A, Craw, D (2016) Polymetallic mineralisation associated with Carboniferous I-type granitoids in central Stewart Island, New Zealand. New Zealand Journal of Geology and Geophysics, 59 (3) 436-456 doi:10.1080/00288306.2016.1174946
Allibone, A.H., MacKenzie, D., Tulloch, R., Tulloch, A., Craw, D. (2016) Polymetallic mineralisation associated with carboniferous I-type granitoids in central Stewart Island New Zealand, New Zealand Journal of Geology and Geophysics, 59:3, 436-456.
Allibone, A.H., MacKenzie, D., Turnbull, R., Turnbull, A., Craw, D. (2016) Polymetallic mineralisation associated with carboniferous I-type granitoids in central Stewart Island New Zealand, New Zealand Journal of Geology and Geophysics, 59:3, 436-456.
Allibone, A.H., MacKenzie, D., Turnbull, R., Tulloch, A., Craw, D. (2016) Polymetallic mineralisation associated with carboniferous I-type granitoids in central Stewart Island New Zealand, New Zealand Journal of Geology and Geophysics, 59:3, 436-456.
Ashley, P, Craw, D, MacKenzie, D, Rombouts, M, Reay, A (2012) Mafic and ultramafic rocks, and platinum mineralisation potential, in the Longwood Range, Southland, New Zealand. New Zealand Journal of Geology and Geophysics, 55 (1) 3-19 doi:10.1080/00288306.2011.623302
MacKenzie, D. J., Craw, D. (1993) Structural control of gold‐scheelite mineralisation in a major normal fault system, Barewood, eastern Otago, New Zealand. New Zealand Journal of Geology and Geophysics, 36 (4) 437-445 doi:10.1080/00288306.1993.9514589
Mackie, C., Mackenzie, D. J., Craw, D. (2009) Structural and lithological controls on gold mineralisation at Oturehua on the northeastern margin of the Otago Schist, New Zealand. New Zealand Journal of Geology and Geophysics, 52 (2) 43-57 doi:10.1080/00288300909509877
Ashley, P. M., Craw, D. (1995) Carrick Range Au and Sb mineralisation in Caples Terrane, Otago Schist, Central Otago, New Zealand. New Zealand Journal of Geology and Geophysics, 38 (2) 137-149 doi:10.1080/00288306.1995.9514646
Allibone, AH, MacKenzie, D, Turnbull, R, Tulloch, A, Craw, D, Palin, M (2016) Polymetallic mineralised veins in ferroan/A-type Cretaceous leucogranite, Stewart Island, New Zealand. New Zealand Journal of Geology and Geophysics, 59 (3) 457-474 doi:10.1080/00288306.2016.1174947
Craw, D. (1979) MĂ©langes and associated rocks, Livingstone Mountains, Southland, New Zealand. New Zealand Journal of Geology and Geophysics, 22 (4) 443-454 doi:10.1080/00288306.1979.10424152
MacKenzie, D. J., Craw, D. (2007) Contrasting hydrothermal alteration mineralogy and geochemistry in the auriferous Rise & Shine Shear Zone, Otago, New Zealand. New Zealand Journal of Geology and Geophysics, 50 (2) 67-79 doi:10.1080/00288300709509822
 
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