YUE Fusheng; ZHANG Jinglian and DU Letian
, 2003, 30(4): 640-0.
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It is known that after the buried, thermal evolution, hydrocarbon generation of organic matter, kaolinite's transfer to montmorillonite, montmorillonite's transfer to illite, which coupled with hydrocarbon generation and migration. Investigation of the Paleogene sediments in Jiyang Depression of Sheng1i Oilfield showed that the transfer from montmorillonite, kaolinite into illite, montmorillonite into potash feldspar, sericite, illite is the result of K+ metasomatism of deeper hydrothemol fluids, which associate with the generation of secondary quartz, and is the silicon release of K+ metasomatism. In the Jiyang Depression there are some evidences of deeper hydrothermal fluids: gypsum-salt generation, Paleogene reef and dolomization, anomalous high gold in crude oils, mantle-derived CO2 gas pool and 3He isotopic anomaly, high temperature of quartz fluid inclusions, basalt magma effusive eruption, and so on. Recognition of illitation, dolomization, gypsum-salt formation will bring about revolutionary effect on petroleum exploration in future.