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《Bulletin of Mineralogy,Petrology and Geochemistry》 2015-03
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Geochemical Characteristics and Environmental Significance of the Upper Triassic Riganpeicuo Formation in Gaize,Tibet

HOU En-gang;GAO Jin-han;WANG Xun-lian;WANG Gen-hou;HU Xin-rui;MA Zhan-chuan;School of Earth Sciences and Resources,China University of Geoscience(Beijing);  
The Riganpeicuo Formation in Garze,Tibet,is a series of carbonate platform facies strata. By the geochemical analysis of 39 carbonate samples,this paper discusses the sedimentary geochemistry characteristics and the palaeosedimentary environment significance of the Riganpeicuo Formation. The results indicate that: 1Mn/Sr ratio of all tested samples is less than 1,with the mean value of 0. 28,which shows that the Riganpeicuo Formation carbonate rocks were little affected by the diagenesis. 2Al2O3,K2 O and Fe2O3 are positively correlated,they negatively correlate with Ga O,and positively correlate with Ni,V; Fe2O3 correlates positively with Mn,Ba,and Ni. 3the contents of Sr,V,Ba,Mn,show an deepening trend from shallow to deep water environment. 4according to the contents of Sr,K,Na,Ca and the ratio characteristics of Sr/Ba,V /( V+Ni) etc.,this paper analyzes the paleoclimate and palaeoenvironment of development period of the Riganpeicuo Formation. In brief,the Riganpeicuo Formation is epicontinental deposits developed in warm humid climate and reducing environment,with a transgressive process.
【Fund】: 中国地质调查局地质调查项目(2-5-2011-67);; 中央高校基本科研业务费项目(2011YYL118)
【CateGory Index】: P588.245
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