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《Geotectonica Et Metallogenia》 2006-01
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MICROSTRUCTURAL CHARACTERISTICS OF CHONGSHAN SHEAR ZONES IN YUNNAN PROVINCE AND ~(40)AR-~(39)AR GEOCHRONOLOGICAL CONSTRAINTS

CHEN Xinyue 1,2, WANG Yuejun1, FAN Weiming1 and PENG Touping 1,2(1. Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. Graduate School of the Chinese Academy of Sciences, Beijing 100039, China)  
All the structural and microstructural observations suggest a tectonic movement of a sinistral strike-slip shearing for the Chongshan-Lincang shear zones. A kinematic scenario was presented for the Chongshan-Lincang shear zones: a sinistral strike-slip transport (top-to-SE extrusion) for the northern Chongshan-Lincang shear zones (Chongshan shear zones) under deformational temperature from ~550 ℃ to ~300 ℃, i.e., from greenschist facies to low amphibolite facies, and a sinistral strike-slip shearing with a WNW-ESE shortening for the southern Chongshan- Lincang shear zones (Lincang shear zones) under deformation temperature from ~450 ℃ to ~300 ℃ and greenschist facies deformational condition as being representative of transition from ductile to brittle condition during progressive deformation. Biotite separated from sample 02DX-139 of mylonitic rocks acquired from Xiaowan in Chongshan shear zones yields well-defined 40Ar- 39Ar plateau age of 28.3±0.1 Ma for about 95% released 39Ar. Muscovite separated from sample 02DX-51 of mylonitic rocks from Xuyi in Lincang shear zones yields well-defined 40Ar- 39Ar plateau age of 31.5±0.2 Ma for about 92% released 39Ar. These ages are interpreted to represent cooling following the synkinematic growth of mica as a consequence of mylonitic overprinting, based on the 40Ar- 39Ar closure temperatures, and to represent the deformation of Chongshan-Lincang shear zones. Chongshan- Lincang shear zones are similar to the Ailaoshan-Honghe shear zones in kinematics and deformation epoch concerning southeastern Tibetan syntaxis. It can offer new information on the Cenozoic structural development of west Yunnan Province and the effect of India-Asia colliding, even on the opening of the South China Sea.
【Fund】: 国家自然科学基金(40334039 40421303 40473019);; 973项目(2002CB412603);; 中国科学院知识创新工程项目(KZCX1-102)的联合资助
【CateGory Index】: P542.3;P597.3
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