Chromite, platinum group elements and nickel mineralisation in relation to the tectonic evolution of the Dun Mountain Ophiolite Belt, east Nelson, New Zealand-Reference-Cited by-同舟云学术

Chromite, platinum group elements and nickel mineralisation in relation to the tectonic evolution of the Dun Mountain Ophiolite Belt, east Nelson, New Zealand

Published:2017-05-03 Issue:3 Volume:60 Page:255-269
ISSN:0028-8306
Container-title:New Zealand Journal of Geology and Geophysics
language:en
Short-container-title:New Zealand Journal of Geology and Geophysics

Author:

Brathwaite R. L.¹,Christie A. B.¹,Jongens R.²

Affiliation:

1. GNS Science, PO Box 30-368, Lower Hutt, New Zealand

2. Anatoki Geoscience, 64 Skibo Street, Dunedin, New Zealand

Funder

Ministry of Economic Development

Ministry of Business, Innovation and Employment

Publisher

Informa UK Limited

Subject

Earth and Planetary Sciences (miscellaneous),Geology,Geophysics

Link

https://www.tandfonline.com/doi/pdf/10.1080/00288306.2017.1313279

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4. Podiform chromitites of the Tari-Misaka ultramafic complex, southwestern Japan, as mantle-melt interaction products

5. Opaque mineral assemblage formed during serpentinization in the Coolac ultramafic belt, New South Wales

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