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《Geotectonica Et Metallogenia》 2002-04
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MESOZOIC CENOZOIC CONTINENTAL STRIKE SLIP FAULT SYSTEM AND ITS ROLES ON URANIUM MINERALIZATION IN HUNAN AND GUANGXI, CHINA

CHEN Xiao dong1, LIU Xiang2, DENG Guo quan2 and HUANG Ru song1(1. No.301 Geologic Team, Hunan Bureau of Nuclear Industry, Hengyang 421003, China;2. Hunan Bureau of Nuclear Industry, Changsha 410011, China)  
The southern Hunan northwestern Guangxi region is one of the most important uranium metallogenic zones in China. Mesozoic geology of this area is predominated by continental strike slip deformation that resulted from the oblique subduction of the palaeo Pacific plate underneath east China continent since the Late Triassic Early Jurassic. Regional structural analyses indicate that the strike slip fault system evolves at two stages under distinct tectonic regimes, i.e., transpressional stage in the whole Jurassic and transtensional stage from Early Cretaceous to early Tertiary. Three NNE striking principal strike slip faults and their subsidiary P fault (NE trending) and R′ fault (NW trending) form a complex fault network that plays significant roles on the formation and distribution of the Mesozoic uranium rich granites and fault basins. The intimately spatial and temporal relationship between uranium deposits and strike slip faults demonstrates that uranium mineralization results from transtensional activity of this huge strike slip fault system.
【Fund】: 核工业中南地质局科研项目(9512)资助.
【CateGory Index】: P619.14
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