Petrogenesis and tectonic significance of the plagiogranites in the Zhaheba ophiolite, Eastern Junggar orogen, Xinjiang, China
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- 作者：Lingjun Zenga ; b ; Hecai Niua ; niuhc@gig.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Zhiwei Baoa ; Qiang Shana ; He Lia ; Ningbo Lia ; b ; Wubin Yanga
- 关键词：Zhaheba ; Ophiolite ; Plagiogranites ; Gabbros ; Amphibolites ; Anatexis
- 刊名：Journal of Asian Earth Sciences
- 出版年：2015
- 出版时间：1 December 2015
- 年：2015
- 卷：113
- 期：part_P1
- 页码：137-150
- 全文大小：2557 K
文摘
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The Zhaheba albitites were formed by early stage albite accumulation.
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The albite granites were formed by residual magma consolidation.
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The plagiogranites were derived from the anatexis of metasomatised gabbro.
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The Zhaheba–Armantai ophiolites were formed at intra-oceanic backarc basin.