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Wang Xingxin, Wang Shaoyi. Influence on Clay Mineral Distributions by Tectonic Backgrounds and Movements[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 46-50.
Citation: Wang Xingxin, Wang Shaoyi. Influence on Clay Mineral Distributions by Tectonic Backgrounds and Movements[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 46-50.

Influence on Clay Mineral Distributions by Tectonic Backgrounds and Movements

  • Received Date: 1997-04-12
  • The paper discusses the clay mineral distribution and evolution of argillaceous rock in sedimentary basins from view of tectonicgeology. It's considered that tectonic backgrounds and movements are the basical factors controlling clay minerals of argillaceousrocks in sedimentary basins. This explains more reasonably the differences of clay mineral compositional characteristics of argilla-ceous rocks between petroleum basins in the east and west China. Furthermore, it explains a special kind of clay mineral assem-blage generally existed in western Tertiary argillaccous rocks, in which the clay minerals are mainly composed of illite and chloritebut the diagenetic grade is very low.
  • [1] Kish H.J.,J. Metamorphic Geol.,1990, 8:31-46.
    [2] Dorsey R. J.,et al.,Geology,1988, 10:944-947.
    [3] Sassi F. P.,Scolari A.,Mineral. and Petrol.,1974. 45:143-1452
    [4] Sassi F. P.,Kraumer H. G.,Schweiz. Mineral. Petrogr Mitt.. 1976, 56:427-434.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Received:  1997-04-12

Influence on Clay Mineral Distributions by Tectonic Backgrounds and Movements

Abstract: The paper discusses the clay mineral distribution and evolution of argillaceous rock in sedimentary basins from view of tectonicgeology. It's considered that tectonic backgrounds and movements are the basical factors controlling clay minerals of argillaceousrocks in sedimentary basins. This explains more reasonably the differences of clay mineral compositional characteristics of argilla-ceous rocks between petroleum basins in the east and west China. Furthermore, it explains a special kind of clay mineral assem-blage generally existed in western Tertiary argillaccous rocks, in which the clay minerals are mainly composed of illite and chloritebut the diagenetic grade is very low.

Wang Xingxin, Wang Shaoyi. Influence on Clay Mineral Distributions by Tectonic Backgrounds and Movements[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 46-50.
Citation: Wang Xingxin, Wang Shaoyi. Influence on Clay Mineral Distributions by Tectonic Backgrounds and Movements[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 46-50.
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