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《Journal of Jianghan Petroleum Institute》 1992-04
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The Characteristics and Orgin of Ordovician Dolomite in Tazhong Area, Tarim Basin

Zhai Yonghong Wang Zezhong Wang Zhengyun Wang Fangping(Dept of Petroleum Geology, JPI)  
With the study of petrology, mineralogy and geochemistry of the Ordovician massive dolomite in Tazhong area of Tarim basin, associated with tectonic evolution in this area, it is concluded that the dolomite has formed by dorag dolomitization in three different stages. The mixing pattern of mixed water includes that the sea water is mixed by fresh water in the exposure of depositional grain banks, that the relict sea water in the sediment is mixed by fresh water in the regressive exposures, that the relict fresh water is mixed by sea water in the progressive bury. The later two stytes of mixing process are of a little difference from the traditional one. The angular gravel of breccia dolomite which has the same origin as the massive dolomite, replaced by Iow temperature hydrothermal, has a higher trace element value of Fe~(2+), Mn~(2+), Sr~(2+), Ba~(2+). The order of the dolomite decreased whereas the value of d_(104) increased。
【CateGory Index】: P581
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