A review of structural patterns and melting processes in the Archean craton of West Greenland: Evidence for crustal growth at convergent plate margins as opposed to non-uniformitarian models
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- 作者：Ali Polata ; b ; c ; polat@uwindsor.ca" class="auth_mail" title="E-mail the corresponding author ; Lu Wangb ; c ; Peter W.U. Appeld
- 关键词：West Greenland ; Archean tectonics ; Convergent margins ; Shear zone ; Accretionary complex ; Sulu Orogen
- 刊名：Tectonophysics
- 出版年：2015
- 出版时间：1 November 2015
- 年：2015
- 卷：662
- 期：Complete
- 页码：67-94
- 全文大小：15629 K
文摘
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Archean supracrustal belts in West Greenland formed at subduction zones
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Supracrustal belts represent fragment of Archean ophiolites.
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Regional- and outcrop-scale structures have similar patterns.
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Structures in the Archean cratons and Phanerozoic orogenic belts are similar.
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Archean continental crust grew at convergent plate margins.