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《Journal of Jilin University(Earth Science Edition)》 2010-02
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Elemental Geochemical Characteristics of the Xiaoping Formation in Late Triassic Epoch in Gaoming Area of the Western Guangdong Province

XU Zhong-jie1,CHENG Ri-hui1,LI Fei1,WANG Liao-liang2,ZHANG Li21.College of Earth Sciences,Jilin University,Changchun 130061,China2.Guangzhou Marine Geological Survey,Guangzhou 510075,China  
8 fresh samples of carbonaceous mudstone were featured from Xiaoping Formation,Late Triassic epoch in Gaoming area of the western Guangdong Province.The constant of whole-rock main element,trace element and REE content were determined using X-ray fluorescence spectrometer and ICP-MS.The values of m(m=100×MgO/Al_2O_3) and Ca/Mg,B/Ga and Rb/K are used to study the paleosalinity in this area.The result shows that the Fenggang Member of Xiaoping Formation is brine neritic facies sedimentation.The paleosalinity showed lowhigh-low-change process.The paleosalinity reaches the highest value in the middle-upper part and decreases to the lowest value at the top.The values of P and Sr/Cu reflect the change of the paleoclimate.Fenggang period is mainly affected by warm-humid climate.And the dry-hot climate occurred in the central and upper part of the period.The discrimination diagrams of Zr-Th and La-Th-Sc and REE show that the tectonic setting of Gaoming area was the depression basin on passive continental margin.All the samples were characterized with high ∑REE(214.15-455.85),LREE enrichemnt(LREE/HREE =7.51-12.02) and Eu negative anomaly(δEu=0.47-0.60).The source rocks are mainly granite partially mixed with basalt and sedimentary rock based on the data.
【Fund】: 国家“973”项目(2009CB219303);; 国家自然科学基金项目(40972074);; 国家油气专项(XQ-2007-03(08)-03)
【CateGory Index】: P618.13
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