Remnants of a Late Triassic ocean island in the Gufeng area, northern Tibet: Implications for the opening and early evolution of the Bangong-Nujiang Tethyan Ocean

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• 作者：Jian-Jun Fan ; ^{fanjj03@163.com} ; Cai Li ^{licai010@126.com} ; Ming Wang ^{wm609@163.com} ; Yi-Ming Liu ^{992702229@qq.com} ; Chao-Ming Xie ^{xcmxcm1983@126.com}
• 关键词：Tibetan Plateau ; Bangong&ndash ; Nujiang Suture Zone ; Gufeng ocean island ; Late Permian ; Late Triassic ; Geochemistry
• 刊名：Journal of Asian Earth Sciences
• 出版年：2017
• 出版时间：March 2017
• 年：2017
• 卷：135
• 期：Complete
• 页码：35-50
• 全文大小：4318 K
• 卷排序：135

文摘

The Late Triassic Gufeng ocean island (GFOI) is a typical ocean island that formed within the Bangong–Nujiang Tethyan Ocean. The range of basalts from MORB to OIB types is found within the GFOI. Geochemical analyses of the GFOI cherts show that they contain terrigenous material, indicating the proximity of a continental margin. The western segment of the Bangong–Nujiang Tethyan Ocean has developed as a mature ocean during the Late Triassic.