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Article Navigation >  Acta Sedimentologica Sinica  > 1997  >  15(S1): 46-50

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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Influence on Clay Mineral Distributions by Tectonic Backgrounds and Movements

  • Institute of Hangzhou Petroleum Geology,Hangzhou 310023

  • 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.
  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-062024-072024-082024-092024-102024-112024-122025-012025-022025-032025-042025-0500.511.522.5
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    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 2.1 %其他: 2.1 %其他: 2.1 %其他: 2.1 %China: 0.9 %China: 0.9 %United States: 3.0 %United States: 3.0 %上海: 0.4 %上海: 0.4 %兰州: 0.4 %兰州: 0.4 %凉山: 0.4 %凉山: 0.4 %北京: 16.3 %北京: 16.3 %台州: 0.4 %台州: 0.4 %呼和浩特: 0.9 %呼和浩特: 0.9 %哥伦布: 0.4 %哥伦布: 0.4 %天津: 1.7 %天津: 1.7 %张家口: 1.7 %张家口: 1.7 %成都: 0.9 %成都: 0.9 %扬州: 0.4 %扬州: 0.4 %晋中: 0.4 %晋中: 0.4 %杭州: 1.7 %杭州: 1.7 %格兰特县: 0.4 %格兰特县: 0.4 %武汉: 0.4 %武汉: 0.4 %深圳: 0.4 %深圳: 0.4 %漯河: 0.9 %漯河: 0.9 %牡丹江: 0.4 %牡丹江: 0.4 %芒廷维尤: 10.3 %芒廷维尤: 10.3 %芝加哥: 3.0 %芝加哥: 3.0 %苏州: 0.9 %苏州: 0.9 %荆州: 0.4 %荆州: 0.4 %西宁: 46.4 %西宁: 46.4 %贵阳: 0.4 %贵阳: 0.4 %长沙: 0.4 %长沙: 0.4 %阳泉: 0.4 %阳泉: 0.4 %青岛: 0.4 %青岛: 0.4 %首尔: 0.4 %首尔: 0.4 %其他其他ChinaUnited States上海兰州凉山北京台州呼和浩特哥伦布天津张家口成都扬州晋中杭州格兰特县武汉深圳漯河牡丹江芒廷维尤芝加哥苏州荆州西宁贵阳长沙阳泉青岛首尔
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  • Received:  1997-04-12

Influence on Clay Mineral Distributions by Tectonic Backgrounds and Movements

  • Institute of Hangzhou Petroleum Geology,Hangzhou 310023
  • Received Date: 1997-04-12

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.
shu

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