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Characteristics of Fluid Inclusions of the Shitouzhai Permian Reef-Type Paleo-Oil Reservoir, Guizhou, South China

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摘要


    

The Shitouzhai Permian paleo-oil reservoir in Guizhou province is a typical example of numerous Upper Paleozoic reef-type paleo-oil reservoirs in the Yunnan, Guizhou and Guangxi regions. The homogenization temperatures of saline aqueous inclusions coexisting with the hydrocarbon inclusions in the three stage calcites are 77lue="84" UnitName="℃">84 , 91lue="103" UnitName="℃">103 and 103lue="155" UnitName="℃">155 , respectively. It is suggested that the hydrocarbon charge of the Shitouzhai reservoir began during the middle Indosinian and reached to a peak during the late Indosinian to the early Yanshannian. The destruction of the reservoir occurred from the middle to late Yanshannian.
    

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