我国东部三个中新生代含油盆地和拗(凹)陷泥岩压实特征

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ON THE COMPACTION CHARATERISTICS OF MUDSTONES IN THE MESO-CENOZOIC PETROLIFEROUS BASINS OR DEPRESSIONS OF THE EAST CHINA

摘要: 作者根据泥岩孔隙度、泥岩粘土矿物和泥岩孔隙流体压力,将我国东部三水、泌阳和黄骅三个中新生代含油气盆地和拗(凹)陷的泥岩压实划分为四个阶段,根据所划分的阶段总结了三个盆地和拗(凹)陷泥岩压实异同和原因。
- 泥岩压实 /
- 压实阶段 /
- 压实特征 /
- 压实差异
Abstract: Based on the properties of the porosity, clay mineral and the pore fluid pressure of the mud-stones, the durations for the mudstone compactions of the Meso-Cenozoic of Shanshui petroliferous Basin,and the Miyang and the Huanghua depressions can be divided into four stages respectively. In this paper,it summarizes the differences and similarities,as well as the genesis among the basin and the depressions on the basis mentioned above.

[1]	张博全等.石油实验地质,1985;7(4):284-293
[2]	张博全等.地球科学,1990;15(1):37-46
[3]	真柄钦次著,陈荷立泽压实与流体运移,1981
[4]	Ricke Ⅲ H H,Chilingnyian GV,徐怀大译.泥质沉积物的压实,1984
[5]	李绍光等.石油学报,1982;(3):13-21