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《JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY》 1997-04
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THE TECTONIC NATURE AND EVOLUTION OF MESOZOIC LANPING SIMAO BASIN

Zhu Chuangye, Xia Wenjie, Yi Haisheng (Chengdu University of Technology, China) Wei Yuanjiang (Xi′an Petroleum Institute)  
The Lanpin Simao basin lies between the Lancangjiang and Jinshajiang suture zones. With disappearance of the Lancangjiang ocean and Jinshajiang ocean, Lanping Simao region developed into a Mesozoic Cenozoic intracontinental basin. In Mesozoic era, the formation and evolution of the Mesozoic Lanping Simao basin were controlled by the Tethys tectonic zone. Based on the analysis of the stratigraphic framework, framework mineral composition, chemical composition, minor elements of clastic rock and composition of volcanic rock in this basin, the authers regard the Mesozoic Lanping Simao sedimentary basin as a polycyclic superposed basin which was fomed by stacking two different type basins. Firstly, it was a back orogenic rift basin. Lastly, it became a down warping basin. The formation and evolution of this Mesozoic basin may feedback the information about the evolution of the Tethys tectonic zone in Western Yunnan.
【CateGory Index】: P544.4
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