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《长春地质学院学报》 1997-04
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STRIKE SLIP ORIGIN AND REVERSE STRUCTURE OF THE YUXI BASIN IN THE CENTRAL PART OF YUNNAN

Zhu Yanming (China University of Mining and Technology, Xuzhou 221008)  
Yuxi Basin is located at the south part of the Puduhe fault zone. The upper Tertiary coal bearing strata are composed of allurival fan lacustrine swamp and flurial lacustrine sequences. The variations in structural settings and the styles of strike slip of the boundary faults of the basin(the Puduhe fault), led to the formation, development and tectonic reverse of Yuxi Basin under a transtentional or transpressional tectonic enviroment. Based on detailed sedimentary and structural analyses, a geodynamic model for the basin formation and its tectonic reverse is built in the present study.
【Fund】: 国家自然科学基金
【CateGory Index】: P541
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