Neoproterozoic IAT intrusion into Mesoproterozoic MOR Miaowan Ophiolite, Yangtze Craton: Evidence for evolving tectonic settings

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• 作者：Hao Deng^a ; ^b ; Songbai Peng^a ; ^b ; ^{psongbai@aliyun.com} ; Ali Polat^a ; ^b ; ^c ; Timothy Kusky^a ; ^b ; Xingfu Jiang^d ; Qingsen Han^a ; Lu Wang^a ; ^b ; Yang Huang^a ; Junpeng Wang^a ; Wen Zeng^b ; Zhengxiang Hu^e
• 关键词：Yangtze Craton ; Huangling Dome ; Kongling terrane ; Miaowan Ophiolite ; Arc-continent collision ; Rodinia
• 刊名：Precambrian Research
• 出版年：2017
• 出版时间：February 2017
• 年：2017
• 卷：289
• 期：Complete
• 页码：75-94
• 全文大小：7947 K
• 卷排序：289

文摘

The Miaowan Complex includes an ophiolite suite and a late magmatic suite. The ophiolite suite initially formed in an oceanic spreading center at ca. 1115 Ma. The late magmatic suite formed in a fore-arc setting at ca. 1000–970 Ma. A Neoproterozoic arc-continent collision model proposed for the Northern Yangtze.