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《Journal of Palaeogeography》 2005-02
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Geochemistry characteristics and sedimentary micro-environments of No.11 coal seam of the Taiyuan Formation of Upper Carboniferous in Pingshuo Mining District,Shanxi Province

Qin Yong Wang Wenfeng Song Dangyu Zhang Xiaodong Institute of Mineral Resources and Geoscience,China University of Mining and Technology,Xuzhou 221008,Jiangsu  
The No.11 coal seam of the Taiyuan Format ion of Upper Carboniferous in the Pingshuo Mining District is generally characteristic of the medium-s ulfur, high-ash and high-organic sulfur,but there are great differences in the ess en tial identifications among the coal layers,which might imply the remarkable div ersification of the coal-forming micro-environments.The results show that th e C a/?(Ca+Fe),Th/?U,Al/?Ti,V/?Zn,δEu and δCe could be used as the sa linity indica tors,the S t,d and S o,d/?S p,d respectively as the Eh and pH ind icators,and the A d,V/?I and ΣREE as the water-dynamic indicato rs.Based on the indicators,the coal-forming micro-environments and the evolution of th e seam were analyzed.It was considered that the seam was formed under the bracki s h-saline water micro-environments with the fluctuant transgression and the e ffect of the paleo-seawater on the peat swamp experienced three stages.The pea t wa s formed in the slightly brackish-brackish micro-environment with the gradua l ly reinforced water-dynamic condition during the first stage,in the brackish- salt water micro-environment with the rather strong water-dynamic condition d ur ing the second stage,and in the brackish micro-environment with the distinctly weakened water-dynamic condition during the third stage.
【Fund】: 江苏省新世纪优秀科学技术带头人工程基金项目 (2 0 0 2 0 3 0 1);; 研究生创新计划项目资助
【CateGory Index】: P618.11
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