Ophiolites and Intra‐Oceanic Island Arc Assemblages of Eastern Australia, New Caledonia and New Zealand
Throughout the Phanerozoic the eastern margin of Gondwana and related fragments such as New Caledonia and New Zealand that are now dispersed from it grew through the addition of ophiolites and associated intra‐oceanic island arc assemblages. Exactly how and why this occurred remains controversial wi...
Published in: | Acta Geologica Sinica - English Edition |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
2017
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Online Access: | http://dx.doi.org/10.1111/1755-6724.13148 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2F1755-6724.13148 https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.13148 |