Clay seals of oil and gas deposits by V I Osipov; V N Sokolov; V V Eremeev

By V I Osipov; V N Sokolov; V V Eremeev

content material: Pt. I. Formation of Clay Seal homes: Theoretical basics --
Ch. 1. Composition of Clay Sediments and Their constitution Formation in Sedimentogenesis --
Ch. 2. Lithogenesis of Clay Sediments --
Ch. three. Formation of the homes of Clay Seals in Lithogenesis --
Pt. II. attribute of the Facies sorts of Clay Seals --
Ch. four. Depositional Environments of Clay Seal Formation --
Ch. five. Facies research of Clay Seals in Oil- and Gas-Bearing Basins --
Ch. 6. The Composition of the Facies sorts of Clay Seals and Its switch with intensity --
Ch. 7. constitution and homes of the Facies varieties of Clay Seals --
Pt. III. Modeling of the swap within the Clay Seal homes in Lithogenesis

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This is evidenced by the circular form of the orientation rose (see Fig. 9%) [23]. In comparison with the quantitative analysis results obtained for the honeycomb microstructure of young clay sediments (see Fig. 13), the matrix microstructure shows a noticeable decrease in the content of large micropores (more than 10 ␮m). At the same time, the number of small micropores (1–10 ␮m) increases, though their average equivalent diameter becomes a little less than in the honeycomb microstructure. 1–1 ␮m) in the matrix microstructure shows a little increase, obviously at the expense of destroyed large and small micropores that have passed to this category.

Silt grains (3) are usually isometric and their surface is covered by clay «coats» (Fig. 2, a). The grain size ranges from 5 to 15 ␮m. 3 ␮m (Fig. 3). 8% of the total porosity (total porosity of the sample is 39%). 2) (see Fig. 2, a). 3 ␮m. They have an isometric or anisometric form. Large isometric micropores (5) (Fig. 3). The intramicroaggregate porosity represented by interparticle (2) and interultramicroaggregate (3) pores (Fig. 2, b) is of subordinate importance in the matrix microstructure.

G. Kossovskaya et al. B. M. V. V. Orlova [79], and many others. E. Fersman [74]. B. V. D. S. Fife et al. [83]. Other scientists began to use the term epigenesis in describing the postdiagenetic transformations in rocks [84–86]. As the term «epigenesis» is used in the ore geology in another sense, the first of the terms has become preferably used. Later, at the boundary between catagenesis and metamorphism, one more stage has been differentiated and given the name of metagenesis [75]. M. B. Vassoevich [76] proposed to use the term «metagenesis» instead of «metamorphism».

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