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《成都地质学院学报》 1989-02
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CREEP DEFORMATION——A DISCUSSION ON TECTONIC DEFORMATON IN THE EAST MARGIN OF THE QINGHAI-XIZANG PLATEAU AND ITS ADJACENT AREAS

Fang Mingze  
Many geologists believe that the Qinghai-Xizang Plateau has subjected to south-north compression. Due to this compression, theplateau material must have had lateral creep-flow to form a series of characteristic structures presently observed in the east margin. 1) Arcuate structural zone: It consists of arcuate folds and faults with apexes pointing to south or southeast and showing the materialcreep-flow to the same directions. 2) Frontal compression upwarping zone and nappe zone: The compression upwarping zone formed at the outlying front part of thecreep-flow, where Prepalaeozoic and Palaeozoic strata are often outcropped. Folds and thrusts are also common. Their axis-planes andfault-planes dip west. Nappes are observed in the area between the compression upwarping zone and the arcuate structural zone,wherethe plateau material creep-flowing eastward and overlaping onto the upwarping zone. 3) All the above mentioned three zones were successively displaced into three sections by a giant NW sinistral strike-slip. The dis-tance of displacement is 90-130km to SE. Development of this structural pattern is believed to have commenced at the end of Triassic, highlighted at Pliocene, and is being stillactive presently.
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1 Ge Xiaohong;A DISCUSSION ON NAPPE STRUCTURE IN YANYUAN, WEST SICHUAN[J];;1984-01
2 Chen Qi Wang Ping;THE MULTIPERIODIC ACTIVITY OF THE PAN-XI RIFT AND ITS SIGNIFICANCE IN DEEP GEOLOGY[J];;1987-01
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1 Wang Tonghe(Geophysient Exploration Bureau, Ministry of Petroleum fntustry);GEOMETRIC AND KINEMATIC CHARACTERISTICS OF NORMAL FAULTS AND DYNAMIC PROCESSES OF BASINS IN EXTENSION AREA IN EAST CHINA[J];;1988-01
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