On the processes that formed Archaean Ni-Cu sulfide mineralisation in the deep continental crust, Thrym Complex, southeastern Greenland
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- 作者：Leon Bagasa ; leon.bagas@uwa.edu.au" class="auth_mail" title="E-mail the corresponding author ; Jochen Kolbb ; Marco L. Fiorentinia ; Nicolas Thebauda ; John Owena ; Steven Rennicka ; Bo Mø ; ller Stensgaardb
- 关键词：Greenland ; Archaean ; North Atlantic Craton ; Thrym Complex ; Granulite facies ; Ni-Cu sulfide mineralisation ; Lower crust
- 刊名：Precambrian Research
- 出版年：2016
- 出版时间：May 2016
- 年：2016
- 卷：277
- 期：Complete
- 页码：68-86
- 全文大小：12303 K
文摘
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Archaean ultramafics and mafic granulite in SE Greenland contain Ni-Cu sulfides.
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The Ni-Cu sulfides formed at lower crustal levels between ∼25 and 40 km deep.
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This is the first documented occurrence of deep-seated Ni-sulfide mineralisation.
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Exhumed deeper crustal levels terrains could have potential for Ni sulfides.