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- W2359090870 abstract "A large volume of basalts was distributed in oil source rocks of Funing formation in Minqiao area of Jinhu depression.The basalts and source rocks are interbedded together forming a kind of assemblage of basalt and source rock. A series of measurements were conducted on trace elements for both the basalts and the source rocks.The results show that the basalts were altered by organic acids and carbonic acid generated from its surround source rocks during their burial history and the trace elements were migrated from the basalts to the source rocks.In fact,the basalt alteration is process of element activation,mineral corrosion and material transportation in the basalts by the acids from source rocks.Then the trace elements are migrated and deposited in the source rocks. At the early alteration,original gas pores and shrink fractures of the basalts were enlarged,and late,the pores and fractures were further enlarged and connected to each other to produce good reservoir spaces for oil and gas accumulation.Meanwhile,the source rocks around the basalts were abnormally rich in the trace metal elements.The interaction between basalt and source rocks is an important mechanism for the basalt corrosion and the reservoir space formation,and for catalysis of organic matter into hydrocarbons by the trace elements in the source rocks." @default.
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- W2359090870 date "2006-01-01" @default.
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- W2359090870 title "Migration of trace elements from basalts to oil source rocks and its geological significance in Minqiao area of Jinhu depression" @default.
- W2359090870 hasPublicationYear "2006" @default.
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