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《Geotectonica Et Metallogenia》 2002-01
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TECTONOLITHOSTRATIGRAPHIC UNITS OF THE AILAOSHAN AREA IN YUNNAN,CHINA AND THEIR IMPLI CATIONS OF TECTONIC EVOLUTION

FANG Wei-xuan1,2,HU Rui-zhong1,XIE Gui-qing 1,SU Wen-chao1 (1.Laboratory of Ore Deposit Geochemis try,Institute of Geochemistry,Chi nese Academy of Sciences,Guiyang550002,China;2.Northwest Geological Exploration B ureau,CNNC,Xi ' an710054,China)  
Based on the recently known data of is otopic dating and tectonolithostra tigraphic units of the Ailaoshan area,tectonic evolution s of the Ailaoshan orogenic belt have been reconsidered.The Proterozoic high-grade metamorphic rock series consist of base tectonic layer.Pre-orogenic tectonolithostratigraph ic units of the Ailaoshan area are the Siluria n detrital rocks of deep sea facies fo rmed on passive,western margin of the Yangtze Plate,the Devonian volc anic-sedimentary rocks in a passive rifted basin on western margin of the Yangtze Plate,the Carboniferous op hiolite suite in the Ailaoshan limit ed oceanic basin and the Upper Per-mian-Early Triassic volcanic-arc v olcanic rocks-terrestrial detrita l rocks formed during ocean-land collision in the Ailaoshan area.Main orogenic te ctonolithostratigraphic units of t he Ailaoshan area in the Yanshanian orogenesis include the Upper Triassic-Jurassic molasses formation in t he foreland basin,syn-orogenic int er-mediate-acidic intrusions,the Yan shanian brittle-ductile shear zones and tectonite.Tectonolithostratigraphic units of intracontinental orogenesis and formation of tectonic plateau in the Himalayan comprise the Ter-tiary-Quaternary molasses formation in intracontinental basin,post-orogenic alkaline -rich intru-sions-lamprophyre and the Honghe du ctile shear zone and tectonite.
【Fund】: 国家重大基础研究规划项目(G1999043200;;2001CB4C9805);; 国家杰出青年科学基金项目(49925309);; 云南省院校科技合作项目(YK98008-3)共同资助.
【CateGory Index】: P542
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