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《Seismology and Geology》 2008-02
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CRUST SHORTENING OF DALIANGSHAN TECTONIC ZONE IN CENOZOIC ERA AND ITS IMPLICATION

CHEN Chang-yun HE Hong-lin(Institute of Geology,China Earthquake Administration,Beijing 100029,China)  
Daliangshan tectonic zone is the rhombic area east of the Anninghe and Zemuhe Fault zones,southeast of the Tibetan Plateau.The Daliangshan tectonic zone is enclosed by three tectonic units:the Bayan Har terrane in its northwest,the Yangzi platform in its southeast and the Longmen Mountain-Yanyuan nappe tectonic belt in the middle.The Daliangshan Fault zone is the most important fault zone in the Dalianshan tectonic zone.This fault zone,together with the Anninghe Fault zone and the Zemuhe Fault zone,make up of the middle part of the Xianshuihe-Xiaojiang Fault zone.The Daliangshan Fault zone consists of 4 branches:the Shimian-Yuexi Fault,the Puxiong Fault,the Butuo Fault and the Jiaoji River Fault.Since Cenozoic,the neotectonic deformation in Daliangshan zone has shown not only sinistral slip and reverse faulting along Dalianshan Fault zone,but also crust shortening.It was estimated that the average crust shortening in Daliangshan zone is(10.9±1.6)km and the crust shortening rate is(17.8±2.2)% by using balanced cross-sections.The crust shortening by folding occurred mainly in the Miocene and the Pliocene,lasting no more than 8.6Ma.Then,the crust shortening velocity of(1.3±0.2)mm/a can be estimated.Comparing with the left offset along the Daliangshan Fault zone,it is recognized that the crust shortening by folding plays an important part in transferring crust deformation southeastward along the Xianshuihe-Xiaojiang Fault system.
【Fund】: 国家自然科学基金(40472109);; 国家重点基础研究发展计划项目(2004CB418410);; 地震科学联合基金(105066)共同资助
【CateGory Index】: P534.6
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