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- W2391480664 abstract "The biggest oolitic gas field has been found at Feixianguan Formation in northeast Sichuan Basin,which belongs to the dynamic system of other source, high press and vertical migration. The natural gas is the dry gas with high content of H_(2)S, and mainly comes from the cracking of foregone pool. The high content of H_(2)S in gas component is contributed to the thermochemical sulfate reduction. The gas accumulation is controlled by palaeohigh. The natural gas distributes under the territorial caprock of gypsum and salinastone at Leikoupo Formation of Middle Triassic, and accumulates in the encirclement controlled by fault. Of all pool forming conditions, encirclement and oolitic reservoir are the two major factors. The provision capability of oolitic reservoir has been greatly improved by dolomitization and corrosion of organic acid and sulfur acid. These oolitic gas reservoirs contain two kinds of forming models, namely, lithology-structure and structure. It belongs to the type of late hydrocarbon accumulation for pool forming that undergo the process of the petroleum accumulation at late Indo-Chinese epoch-Yanshan movement, and adjustment at Himalayan movement. The oolitic reservoir has a good exploration foreground due to the wide distribution and the huge resource potenial." @default.
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- W2391480664 date "2005-01-01" @default.
- W2391480664 modified "2023-09-26" @default.
- W2391480664 title "Features of gas accumulation and exploration foreground in oolitic reservoir of Feixianguan Formation in Sichuan Basin" @default.
- W2391480664 hasPublicationYear "2005" @default.
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