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《Acta Scicentiarum Naturalum Universitis Pekinesis》 2004-04
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Jurassic Coal in Yanqi Basin (Xinjiang,China): Geochemical Characteristics of Trace Elements and Their Implications

CUI Guanglai 1) QUAN Shujin 2) WU Chaodong 1) ( 1) School of Earth and Space Sciences, Peking University, Beijing, 100871; 2) Henan Oilfield Branch of China Petroleum and Chemical Corporation,Nanyang,473132)  
Trace elements data for the coal seams in the Jurassic system are used to assess the sedimentary environments of Yanqi Basin, Xinjiang, China.The concentrations,distribution and occurrences of state about trace elements are discussed. Detailed geochemical characteristics on trace elements reveal that: (1) the content of trace elements is low as a whole, but P, V, Ti values are relatively high, indicating that Yanqi Basin belongs to a kind of inland lake environment;(2)they are concentrated obviously on the edge of the basin, the roof and floor and interlayer of the coal seams; (3) P,Sr,Co show affinities with organic matter, however, Cu and Ti mainly associated with clay minerals;(4) the geochemical features, the colors of sediments and the appearance of coarse detritus in Xishanyao Formation demonstrate that the coal\|accumulating environment was gradually transferring from freshwater to brackish in the Jurassic system, and correspondingly the palaeoclimate was changing from humidity to drought.
【Fund】: 国家重点基础研究发展规划资助项目 (G1 9990 4 330 4 )
【CateGory Index】: P595
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