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《Geological Science and Technology Information》 2009-03
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Element Geochemistry Characteristics of Karstic Cave Deposit in Tahe Oilfield and Its Environmental Significance

LIU Xian-feng a,b,c,CAI Zhong-xian b,c (a.Graduate School;b.Faculty of Earth Resources;c.Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education,China University of Geosciences,Wuhan 430074,China)  
Tahe Oilfield lies in southwest margin of Akekur Salient in north Tarim basin.Meteoric water karstification because of intensive uplift during Caledonian-Hercynian period,extensive transgression in early Carboniferous and large scale magma and volcano events in Permian would influence the Ordovician carbonate formation.Based on the features of geology evolvement,a study is made of arenaceous and pelitic karstic cave deposit on its trace elements such as Ga,Rb,etc,and REE characteristics in the main Tahe Oilfield.The results indicate that most samples show characteristic of fresh water corrosion,while samples of the four wells such as T615 reveal the influence of seawater.It can be inferred that the seawater-fresh water mixing corrosion is not intense in this area,and that the characteristics of element geochemistry of karstic filling indicate the overlay on the earlier fresh water corrosion.The analysis refelcts that positive europium anomaly of some samples may be relative to the hydrothermal fluids in Permian.Also the analysis of the carbon and oxygen isotopes suggests the occurrence of freshwater-seawater mixed corrosion and magma hydrothermal fluid corrosion in the oilfield except for fresh water corrosion.
【Fund】: 国家重点基础研究发展规划“973”项目(2005CB422105)
【CateGory Index】: P618.13
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