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《Guizhou Geology》 1987-04
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Fluid Inclusion in Carbonatites Mineral and Petroleum Exploration in Guizhou

Yang Hui-Ming ( Dianqiangui Petroleum Exploration Bureau )  
The type, character, temperature and existing form of fluid inclusion in car bonatite are described in this paper.Based on the relationship between fluid inclusion and petroleum exploration, three situations can be classified as follows. l. A great amount liquid and pure liquid inclusions present and the pure gas inclusions can not be seen in rocks; 2. Only the gas and pure gas inclusions occur: 3. The liquid inclusions predominate in rocks.And they symbolized a good, bad, and middle petroleum exploration prospect in Guizhou respectively. According to the temperature of fluid [inclusion, there are three situations about inclusions, 1. Temperature of inclusions is lower than 140C or 170C, which present in post Ordovician strata in the east part of Guizhou; 2.Temperature 200C, in permian strata in North and South Guizhou; 3. Temperature 140C-150C, in Permian strata of Middle Guizhou. They also reflect the good, bad and middle petroleum prospect in Guizhou correspondingly. The ratio, CH4/(CO2+H2O ) =0.015-0.03, in the gas phase of fluid inclusion from Wenan Sinian System, is higer than that from some well-known oil and gas formation and therefore the petroleum can not be found in Sinian strata of this area. This result will be of significance for other area.
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