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《EARTH SCIENCE FRONTIERS》 1999-03
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COUPLING MECHANISM OF STRIKE-SLIP OROGEN AND BASIN

Liu Hefu; Xia Yiping; Yin Jinyin; Shang Peile(China University of Geosciences, Beijing, 100083)  
Strike-slip orogen is one of the major orogenic types of continental orogenic chain.There are four types of strike-slip fault depending on the depth of the fault involved: ① trans-form fault, ②transcurrent fault, ③transfer fault, and ④ tear fault. The contractive-resistantbending can produce the strike-slip contractive belt, and the extensional-relaxed bending can re-sult in the strike-slip extensional belt. The forming of strike-slip orogen and positive flowerstructure is due to the contractive strike-slip. The contractive strike-slip can also produce thestrike-slip contractive basin along the one side or the two sides of strike-slip orogen. The exten-sional strike-slip can produce the strike-slip type basin-range system and the negative flowerstructure. The pull-apart basin and wedge-shaped depression can also be developed along oneside or both sides of the strike-slip orogen. Due to the Indian plate's wedging and the Siberiaplate's blocking up, the slip-line field is formed in the China continental plate, which can pro-duce the strike-slip orogen and the strike-slip basin in the eastern China and in the broad mid-western China. The strike-slip field can also adjust the compression of the western part of Chi-na, and the escaping-creeping of the eastern China. Therefore, the strike-slip orogen andstrike-ship-flexural basin are formed in the mid-western part of China, while the strike-slipbasin-range system and pull-apart basin are developed in the eastern China.
【Fund】: 国家自然科学基金!49672154
【CateGory Index】: P54
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