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《Acta Sedimentologica Sinica》 2006-01
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Geochemical Characteristics on Brine and Potash Perspective in the Western Tarim Basin

MA Wan-dong~1 MA Hai-zhou~2(1.College of Environment & Planning,Henan University,Kaifeng,Henan 475004;2.Qinghai Institute of Salt Lakes,Chinese Academy of Sciences,Xining 810008)  
In the geological evolution of Tarim Basin,many transgressions and regressions of the ancient Terishappened,especially in the Cretaceous and Tertiaryperiod,and broughtplentyof salt sources.What's more,because of uttermost drought and proper sedimentary facies and paleogeography,many salt,gypsum,carbonate and mud-salt weredeposited.By our fieldwork,above 300 samples were collected including brine and solid.Among these samples,43 brine samples and 99 solid halite samples were analyzed.The item of analysis included K~(+),Na~(+),Ca~(2+),Mg~(2+),Cl~(-),SO~(2-)_4,CO~(2-)_3,HCO~-_3,Br~(-),B~(3+)and so on.This paper discussed the variety of the content of K~(+)and the characteristicscoefficients of geochemistry,the model of salt formation,the concentration stage of brine and the possibility of potash formation by geochemical analysis of the brine from Tarim Basin.In the end,the potash perspectivewas proposed.From the geochemical parametersof brine in WesternTarim Basin,we could conclude that the perspective of potashis Kashi Sag and Yangxia Sag.By comparing the content of microelementand the geochemical parametersof brine with that of normal condensed brine,it is known that there is little microelementssuch as Br and B in Tarim Basin,so we could not completely depend on these indexes to judge the condense stage of brine and halite as well as potashresources,and this viewpoint indicates that Tarim Basin is the intricate area of salt formation.
【CateGory Index】: P592;P618.2
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7 Zhang Pengxi Zhang Baozhen(Qinghai Institute of Salt Lakes, Acadcmia Sinicn, Xining 810008)T. K. Lowenstein(Department of Geological Sciences and Environmental Studies, State University of New York at Binghamton, Binghamton, NY 13901 U. S. A.)R. J. Spencer(Department of Geology and Geophysics, University of Calgary, Calgary, Alberta T2N IN4 Canada);ON THE ORIGIN OF ANCIENT ANOMALOUS EVAPORITES: EVIDENCE FROM QAIDAM BASIN[J];Geochimica;1991-02
8 Liu Weiguo ;Peng Zicheng ; Xiao Yingkai ; Wang Zhaorong ; Nie Baofu ;An Zhisheng (Dept. of Earth and Space Science, University of Scicnce and Technology of China, Hofei 230026)(Qinghai Instutae of Salt Lakes, Chinese Academy of Sciences, Xining 810008)(So;Boron isotopic composition of corals from South China Sea and their environmental significance[J];GEOCHIMICA;1999-06
9 LIN Qing1, PENG Ping- an2, LIU Rong- mo3 (1. State Key Laboratory of Geocryology and Engineering, Institute of Cold and Arid Regions Environmental and Engineering, Chinese Academy of Sciences, Lanzhou 730000, China; 2. State Key Laboratory of Organic Ge;Carbon isotope composition of buried plant tissues in Ngoring shallow frozen lacustrine sediments[J];GEOCHIMICA;2000-05
10 Cai Chunfang; Mei Bowen (Jianghan Petroleum Institute. Jingsha, Hubei 434102)Li Wei(Research Institute of Petroleum Exploration and Development, Beijing 100083);THE HYDROGEOCHEMISTRY OF OIL-FIELDS IN TARIM BASIN[J];GEOCHIMICA;1996-06
China Proceedings of conference Full-text Database 1 Hits
1 Liu Chenglin(Institute of Mineral Deposits, CAGS, Beijing)Wang Milly (Geological Society of China , Beijing);Evolution of Quaternary Depositional Environments and Forming of Potash Deposits in Lop Lake,Xinjiang, China[A];[C];1999
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