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《Earth Science-Journal of China University of Geosciences》 1993-05
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TECTONIC EVOLUTION OF PALAEO-TETHYS POLY-ISLAND-OCEAN IN CHANGNING-MENGLIAN AND LANCANGJIANG BELTS,SOUTHWESTERN YUNNAN,CHINA

Liu Benpei Feng Qinglai Fang Nianqiao Jia Jinhua He Fuxiang (China University of Geosciences, Beijing 100083)  
The Changning-Menglian belt,located between the Baoshan-Gengma and Simao-Lin-cang massives in Southwestern Yunnan,preserves the complete record of a suture zone and the most continuous sequence of oceanic basin, representing the main branch of palaeo-Tethys poly-island-ocean during Devonian to Middle Triassic. The Lincang massif was probably a isolated Gondwana-affinity terrane and accreted to the western margin of Simao massif in Middle Permian. The Lancangjiang belt and Changning-Menglian belt therefore, consisted of a unified ocean which may connected by the Nan-Uttaradit suture of Northern Thailand before Late Permian. It should be pointed out that the palaeo-Tethys had been closed by small massives accretion in Late Indosinian Orogeny , moreover the Himalayan Orogeny of the Neo-Tethys stage had happened strongly in these belts.
【Fund】: 国家自然科学基金项目(49172101)、博士导师基金项目联合资助
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