Carboniferous granites on the northern margin of Gondwana, Anatolide-Tauride Block, Turkey - Evidence for southward subduction of Paleotethys
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- 作者：O. Candana ; osman.candan@deu.edu.tr" class="auth_mail" title="E-mail the corresponding author ; C. Akala ; O.E. Koralaya ; A.I. Okayb ; R. Oberhä ; nslic ; D. Prelevićd ; e ; R. Mertz-Krausd
- 关键词：Carboniferous magmatism ; Paleotethys ; Gondwana ; Afyon zone ; Anatolide-Tauride Block
- 刊名：Tectonophysics
- 出版年：2016
- 出版时间：30 June 2016
- 年：2016
- 卷：683
- 期：Complete
- 页码：349-366
- 全文大小：6756 K
文摘
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Carboniferous metagranites crop out in the Anatolide-Tauride Block of Turkey.
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Arc-type granites are related with southward subduction of Paleotethys.
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Northern active margin of Gondwana switched to a passive margin in the Late Permian.