陆相盆地沉积作用与构造作用的关系

陶晓风; 刘登忠; 朱利东

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陆相盆地沉积作用与构造作用的关系

陶晓风, 刘登忠, 朱利东

文章导航 > 沉积学报 > 2001 > 19(3): 410-414

陶晓风, 刘登忠, 朱利东. 陆相盆地沉积作用与构造作用的关系[J]. 沉积学报, 2001, 19(3): 410-414.

引用本文:

陶晓风, 刘登忠, 朱利东. 陆相盆地沉积作用与构造作用的关系[J]. 沉积学报, 2001, 19(3): 410-414.

TAO Xiao feng, LIU Deng zhong, ZHU Li dong. Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process[J]. Acta Sedimentologica Sinica, 2001, 19(3): 410-414.

Citation:

TAO Xiao feng, LIU Deng zhong, ZHU Li dong. Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process[J]. Acta Sedimentologica Sinica, 2001, 19(3): 410-414.

陶晓风, 刘登忠, 朱利东. 陆相盆地沉积作用与构造作用的关系[J]. 沉积学报, 2001, 19(3): 410-414.

引用本文:

陶晓风, 刘登忠, 朱利东. 陆相盆地沉积作用与构造作用的关系[J]. 沉积学报, 2001, 19(3): 410-414.

TAO Xiao feng, LIU Deng zhong, ZHU Li dong. Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process[J]. Acta Sedimentologica Sinica, 2001, 19(3): 410-414.

Citation:

TAO Xiao feng, LIU Deng zhong, ZHU Li dong. Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process[J]. Acta Sedimentologica Sinica, 2001, 19(3): 410-414.

陆相盆地沉积作用与构造作用的关系

成都理工学院地质学系,成都 610059

详细信息

作者简介:
陶晓风,男,1958年出生,副教授,构造地质学专业

中图分类号: P512.2

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文章访问数: 623
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Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process

Chengdu Institute of Technology,Chengdu 610059

摘要

摘要: 构造作用与沉积作用两者之间的联系性和统一性正受到人们重视。陆相盆地沉积作用受构造作用的控制极为明显。沉积演化就是构造演化的反映,陆相盆地沉积作用直接反映了构造活动的特征。陆相盆地沉积作用最主要的特征是相变快和幕式沉积作用。按构造动力学背景,可将陆相盆地分为三大类型:张性盆地、压性盆地和剪性盆地。这三类盆地在沉积作用上有很大差异。
- 陆相盆地 /
- 盆地类型 /
- 构造背景 /
- 盆地充填
Abstract: A good deal of attention has been paid to the relation and unity of the tectonic process and sedimentation．It is very obvious that the sedimentary process of the terrestrial basin is controlled by tectogenesis．The sedimentary evolution of the basin is the reflection of the tectonic evolution．The sedimentary process of the terrestrial basin has unique characteristics．(1)The scope of the terrestrial basin is mainly controlled by the fault zones．(2)The regional tectonic cycle obviously controls the sedimentary sequence boundary of the terrestrial basin．The periodicity of tectogenesis causes the periodic change of the sedimentary sequence．(3)The sedimentary model of the terrestrial basin is obviously controlled by the tectonic framework．(4)There are many surprising sedimentary events in sedimentary formation of the terrestrial basin．(5)Owing to the influence of the tectonics,the deformation frequently occurs in the sedimentary deposit．(6)Because the sediments of the terrestrial basin have the short-distance transport,the sediments．have the low mature index．(7)There are more sedimentary centres,more matter-sources,narrow sedimentary facies-zone and the quick facies change in the terrestrial basin． According to the background of the tectonic dynamics．the terrestrial basin can be divided into the extension basin．the compression basin and the shear basin．The three basins differ gready in the sedimentary characteristics．The extension basin is usually directed at rift basin the border of the extension basin is mainly the normal fault or growth fault．The plane shape of the extension is zone-shape．The sedimentary deposit of the extension basin has not strong deformation．the thickness of the sediment on the downthrow wall is greater than that the sediment on the upcast wall．The periodic change of the tectogenesis cause the enlarging or the contract the extension basin． The compression basin is usually directed at the terrestrial foreland basin．The shape of the compression basin is usually dustpan shape．The sedimentary deposit of the compression basin has usually the strong deformation．The sedimentary center of the compression basin moves to the foreland．The evolution of the compression basin has relation to the evolution of theorogenic belt．The developing process of the compression basin is a contract process．The shear basin is usually directed at the strike-slip basin．The plane shape of the shear basin is usually rhombus．The plane constitution is usually a string of beads．The evolution of the shear basin is controlled by the master fault,The developing process of the shear basin is an enlarging process．The sedimentary center of the shear basin moves to the strike of the master fault．
- terrestrial basin /
- basin type /
- tectonic backgTound /
- filling characteristics

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参考文献(1)

[1]	1.1:5万兔蛾幅、顺荡井幅、弥沙井幅区域地质调查报告 1999 2.刘登忠;朱利东;陶晓风陆相红层填图方法 1999 3.夏祖葆红层问题 1990(10) 4.廖瑞君;刘邦秀;邹爱建陆相红盆地构造一岩性一岩相填图方法新进展 1998(12) 5.李思田断陷盆地分析与煤聚集规律 1988 6.夏文臣;金友渔沉积盆地的成因地层分析 1988 7.刘登忠;陶晓风;朱利东滇西兰坪盆地盆山耦合 1999 8.许效松中国西部大型盆地分析及地球动力学 1997

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陆相盆地沉积作用与构造作用的关系

成都理工学院地质学系,成都 610059

作者简介:
陶晓风,男,1958年出生,副教授,构造地质学专业

收稿日期: 2000-01-11
修回日期: 2000-08-17
刊出日期: 2001-09-10

中图分类号: P512.2

关键词:

摘要: 构造作用与沉积作用两者之间的联系性和统一性正受到人们重视。陆相盆地沉积作用受构造作用的控制极为明显。沉积演化就是构造演化的反映,陆相盆地沉积作用直接反映了构造活动的特征。陆相盆地沉积作用最主要的特征是相变快和幕式沉积作用。按构造动力学背景,可将陆相盆地分为三大类型:张性盆地、压性盆地和剪性盆地。这三类盆地在沉积作用上有很大差异。

English Abstract

Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process

Chengdu Institute of Technology,Chengdu 610059

Received Date: 2000-01-11
Rev Recd Date: 2000-08-17
Publish Date: 2001-09-10

Keywords:

Abstract: A good deal of attention has been paid to the relation and unity of the tectonic process and sedimentation．It is very obvious that the sedimentary process of the terrestrial basin is controlled by tectogenesis．The sedimentary evolution of the basin is the reflection of the tectonic evolution．The sedimentary process of the terrestrial basin has unique characteristics．(1)The scope of the terrestrial basin is mainly controlled by the fault zones．(2)The regional tectonic cycle obviously controls the sedimentary sequence boundary of the terrestrial basin．The periodicity of tectogenesis causes the periodic change of the sedimentary sequence．(3)The sedimentary model of the terrestrial basin is obviously controlled by the tectonic framework．(4)There are many surprising sedimentary events in sedimentary formation of the terrestrial basin．(5)Owing to the influence of the tectonics,the deformation frequently occurs in the sedimentary deposit．(6)Because the sediments of the terrestrial basin have the short-distance transport,the sediments．have the low mature index．(7)There are more sedimentary centres,more matter-sources,narrow sedimentary facies-zone and the quick facies change in the terrestrial basin． According to the background of the tectonic dynamics．the terrestrial basin can be divided into the extension basin．the compression basin and the shear basin．The three basins differ gready in the sedimentary characteristics．The extension basin is usually directed at rift basin the border of the extension basin is mainly the normal fault or growth fault．The plane shape of the extension is zone-shape．The sedimentary deposit of the extension basin has not strong deformation．the thickness of the sediment on the downthrow wall is greater than that the sediment on the upcast wall．The periodic change of the tectogenesis cause the enlarging or the contract the extension basin． The compression basin is usually directed at the terrestrial foreland basin．The shape of the compression basin is usually dustpan shape．The sedimentary deposit of the compression basin has usually the strong deformation．The sedimentary center of the compression basin moves to the foreland．The evolution of the compression basin has relation to the evolution of theorogenic belt．The developing process of the compression basin is a contract process．The shear basin is usually directed at the strike-slip basin．The plane shape of the shear basin is usually rhombus．The plane constitution is usually a string of beads．The evolution of the shear basin is controlled by the master fault,The developing process of the shear basin is an enlarging process．The sedimentary center of the shear basin moves to the strike of the master fault．

陶晓风, 刘登忠, 朱利东. 陆相盆地沉积作用与构造作用的关系[J]. 沉积学报, 2001, 19(3): 410-414.

引用本文:

陶晓风, 刘登忠, 朱利东. 陆相盆地沉积作用与构造作用的关系[J]. 沉积学报, 2001, 19(3): 410-414.

TAO Xiao feng, LIU Deng zhong, ZHU Li dong. Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process[J]. Acta Sedimentologica Sinica, 2001, 19(3): 410-414.

Citation:

TAO Xiao feng, LIU Deng zhong, ZHU Li dong. Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process[J]. Acta Sedimentologica Sinica, 2001, 19(3): 410-414.

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陆相盆地沉积作用与构造作用的关系

作者简介:
陶晓风,男,1958年出生,副教授,构造地质学专业

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Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process

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陆相盆地沉积作用与构造作用的关系

成都理工学院地质学系,成都 610059

作者简介:
陶晓风,男,1958年出生,副教授,构造地质学专业

English Abstract

Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process

Chengdu Institute of Technology,Chengdu 610059

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陆相盆地沉积作用与构造作用的关系

作者简介: 陶晓风,男,1958年出生,副教授,构造地质学专业

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Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process

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出版历程

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陆相盆地沉积作用与构造作用的关系

成都理工学院地质学系,成都 610059

作者简介: 陶晓风,男,1958年出生,副教授,构造地质学专业

English Abstract

Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process

Chengdu Institute of Technology,Chengdu 610059

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期刊在线

联系我们

作者简介:
陶晓风,男,1958年出生,副教授,构造地质学专业

作者简介:
陶晓风,男,1958年出生,副教授,构造地质学专业