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- W2359365759 abstract "Measures as thin-section analysis,clay mineral X-ray diffraction,vitrinite reflection and physical pro-perty analysis of oil layer,combined with the results of a regional petroleum geological study,were applied to the research of the relationship between authigenic minerals and secondary porosity of the deep clastic reservoirs in the 3rd and 4th members of the Paleogene Shahejie Formation in Jiyang Depression.The result shows that,for the 3rd member,the secondary porosity of the depth interval within 3 150-3 600 m are related to the dissolution of acid-soluble components such as carbonate minerals,while that within 4 250-4 500 m are formed by dissolution of alkali-soluble components.In contrast,for the 4th member,the secondary porosity of the depth intervals within 3 350-3 600,3 950-4 200 and 4 500-4 900 m are formed mainly by dissolution of acid-soluble minerals,and those within 5 600-5 700 m are connected with dissolution of alkali-soluble components.For the depth interval of 4 400-4 700 m in Chezhen sag,the low content of kaolinite and high content of ledikite coincide well with high secondary porosity.For the deep layers in northern Dongying sag and Bonan sag,high content of chlorite coincide relatively well with high secondary porosity and present a mutual waning and waxing relationship with the ledikite content.For the depth interval of 3 500-4 800 m in the Bonan sag,there is an abnormal clay mineral transforming zone,and high I/S ratios coincide relatively well with an abrupt increasing of chlorite and high secondary porosity." @default.
- W2359365759 created "2016-06-24" @default.
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- W2359365759 date "2010-01-01" @default.
- W2359365759 modified "2023-09-26" @default.
- W2359365759 title "Relationship between authigenic minerals and porosity in the deep Paleogene formations of the Jiyang Depression" @default.
- W2359365759 hasPublicationYear "2010" @default.
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