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《GEOTECTONICA ET METALLOGENIA》 2000-03
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A STUDY OF THRUST TECTONICS OF JIAGOU- TAOSHANJI AREA, NORTHERN ANHUI

CHEN Yun- tang, SHU Liang- shu (Department of Earth Sciences,Nanjing University,Nanjing 210093,China)  
Large scale thrust tectonics occurred in Early Mesozoic in the Xuzhou- Suzhou region,southern margin of North China plate.The strata that were involved in this thrust tectonics are Neo- Proterozoic- Paleozoic sedimentary layers,characterized by strongly brittle deformation of step- type thrusting and fault- related folding (fault propagation fold).Thrust flakes with various scales and shapes were developed well in the Jiagou- Taoshanji area;each flake consists of upper rock- block,slipping fault and lower rock- block.Eight slipping beds that are related to thrust tectonics were reported.The paper researched geometry,kinematics,timing of emplacement and shortening rate of thrust bodies.Thrust structural styles include superimposition- type and step- type; duplex- type and klippe- type also develop in the region.The Xuzhou- Suzhou arc tectonics can be divided into three parts from east to west:(1) the Tan- Lu thrust root zone,marked by lower- angle thrust of Neo- Proterozoic with weakly ductile shear deformation,(2) the Jiagou- Taoshanji middle zone,characterized by fault- related fold,step- type thrust with lower- middle dip angle of fault,(3) the northern Anhui- Xiaoxian County front zone of superimposion thrust with high- angle of fault.Regional detachment fault is located between the Neo- Proterozoic rocks and Paleo- Proterozoic metamorphic basement in the deep crust;thrust structures that occur at surface are a cover thrust of the Paleozoic sedimentary rocks.Authors described in detail the three typical structural phenoma,that is,the Lihuashan- Zhangzhuang superimposition thrust zone,the Wuyanquan step- type thrust zone and the Dashankou- Changwo klippe zone.The movement of thrust is from ESE to WNW,namely from Tan- Lu fault zone to North Anhui.Large- scale thrust tectonics in the studied area constrained the distribution and richness of coal beds.Study results suggest that the large- scale thrust event was caused by Early Mesozoic intracontinental subduction and took place after Late Triassic and prior to Late Jurassic,corresponding with a collision between the North China continent and Yangzi continent along the Dabieshan suture zone.
【Fund】: 国家自然科学基金重点资助项目!(批准号:49632080)
【CateGory Index】: P542.3
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