• 责任者：Geng Quanru (Chengdu Institute of Geology and Mineral Resources ; Chengdu 610082 ; China) ; Pan Guitang
• 刊名：Geological Bulletin of China
• 出版年：2011
• 卷期：30(8)
• 关键词：特提斯构造带 ; Tethyan Tectonic Zone ; 西藏 ; Tibet
• 页码：p.1261-1274
• 图表：illus., 1 plate, 73 refs.
• 分类号：0300
• issnNo：ISSN1671-2552
• isbnNo：CN11-4648/P

Early Paleozoic-Devonian sediments of the study area are mainly composed of shelf clastic rocks and platform carbonate, representing the northern margin of Gondwana and south Tethyan passive continental margin. Permian-Carboniferous archipelagos were formed to the south and north of the Tethyan Ocean, resulting in the formation of magmatic arcs to the north of the Longmuco-Shuanghu belt and the south of the Jinshajiang and in the Gangdise zone one after another. Mesozoic archipelagos occurred to the south of the Tethyan Ocean, where Cr, Ni and Pt group metallic type deposits of magmatic segregation occurred in the SSZ-type ophiolite. Petrological and geophysical evidence supports a bilateral subduction scenario that resulted in arc magmatism to the north and south of the Bangong Co-Nujiang suture zone.