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《Journal of Jianghan Petroleum Institute》 1991-02
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The Origin of Xiaqiulitaga Group Dolomite in Keping Area, Tarim Basin

Hu Mingyi(Jianghan Petroleum Institute) Jia Zhenyuan(China University of Geosciences)  
The origin of Xiaqiulitaga group dolomite in Keping area, Tarim Basin, Xinjiang is discussed in this paper according to the textures of dolomite, geochemical analysis of elements, x-ray diffraction and inclusion thermometry. It is concluded that different dolomites formed in different environments have different models of dolomitization. Algal dolomite and mud crystalline dolomite in tidal flat or lagoon, consisting for its greater part of mud crystalline dolomite and with a high ordering degree(equal to 0.84), contain a large amount of trace elements(Sr, Ba more than 100 ppm and B more than 1ppm). These facts show that Algal dolomite and mud crystalline dolomite were formed by Coorong dolomitization. Grain dolomite in shoal, consisting of mud crystalline and coarsely crystalline dolomite and with a poor ordering degree (about 0.56 to 0.76), was formed by meteoric-marine mixing dolomitization. Crystalline dolomite in tidal flat, consisting of different forms and sizes of dolomite and with the ordering degree as high as 0.88 to 0.95, was formed by deep burial dolomitization.
【CateGory Index】: P618.1
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