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Preliminary Application of the Dolomite-Calcite Oxygen Isotope Thermometer in Studying the Origin of Dolomite in Feixianguan Formation, Northeast Sichuan Province, China
详细信息   
摘要

    

Based on the textural classification and oxygen isotope analyses, the temperatures of different types of dolomite samples from Feixianguan Formation of Northeast Sichuan Province are calculated by the dolomite-calcite oxygen isotope thermometer. Most of the calculated temperatures range over from 40 to 140 . The calculated temperatures of crystalline dolomite and dolomite cement have a relatively high temperature range and the calculated temperatures of oolitic dolomite and micrite dolomite have a relatively low temperature range. These results are consistent with the fluid-inclusion homogenization temperatures and formation environment of dolomite.

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