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《JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY》 2000-03
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GEOCHRONOLOGIC STUDY ON THE FORMATION AND EVOLUTION OF TAN-LU FAULT

CHEN Xuan_hua 1, WANG Xiao_feng 1, ZHANG Qing 1, CHEN Bai_lin 1, CHEN Zheng_le 1,HARRISON T Mark 2, YIN An 2 (1.Institute of Geomechanics, CAGS, Beijing 100081,China;2.Department of Earth and Space Sciences, UCLA, California 90095-1567, USA)  
The formation and development of the Tan-Lu fault zone in eastern China was constrained here through the 40 Ar- 39 Ar timing of muscovites from Zhangbaling blueschist belt, K-feldspar from gneissic granite at Qiaotouji, K-Ar timing of gouge and ESR timing of dynamic-generated quartz films in the fault zone. Considering relative geologic and paleomagnetic data, we propose four stages for the formation and development of the Tan-Lu fault zone: (1) the formation of the Tan-Lu fault zone during 244~209 Ma due to the collision of the North China and Yangtze Blocks; (2) rotation of the Yantze block, east of the Tan-Lu fault zone during 189~164 Ma; (3) normal faulting with strike-slip displacement during 103~94 Ma; and (4) right-lateral strike-shift compressive stage in later K 2-E. The relationship between the Tan-Lu fault zone and the Dabie-Sulu metamorphic belt is also discussed here.
【Fund】: 原地矿部“八五”重要基础项目!(85 0 2 2 10 )资助
【CateGory Index】: P597.3
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