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

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

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

计量

文章访问数: 520
HTML全文浏览量: 3
PDF下载量: 440
被引次数: 0

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

HTML全文

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

[1]	李娟, 陈雷, 胡月, 计玉冰, 卢畅, 董建华, 谭秀成. 滇黔北昭通地区晚奥陶世-早志留世黑色页岩地球化学特征及其地质意义【碳酸盐岩与富有机岩形成环境专辑】 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.038
[2]	张茜, 张海全, 王剑, 门玉澎, 余谦, 周业鑫, 曹竣锋, 赵安坤. 康滇古陆两侧五峰组－龙马溪组黑色泥岩沉积演化差异【“华南古大陆演化及其资源环境效应”专辑】 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.039
[3]	朱红涛, 徐长贵, 李森, 杜晓峰. 陆相盆地限制性沉积体系 . 沉积学报, 2023, 41(6): 1903-1916. doi: 10.14027/j.issn.1000-0550.2022.137
[4]	张治波, 徐颖, 苗艳菊, 王文锋, 赵迪斐, 陈丹玲. 昌都盆地古近系贡觉组物源及其沉积环境 . 沉积学报, 2022, 40(6): 1561-1581. doi: 10.14027/j.issn.1000-0550.2022.094
[5]	潘世乐, 蒋赟, 康健, 陈波, 张顺存, 孙国强. 柴北缘冷湖七号下干柴沟组上段古气候及物源分析 . 沉积学报, 2021, 39(5): 1292-1304. doi: 10.14027/j.issn.1000-0550.2021.013
[6]	范海经, 邓虎成, 伏美燕, 刘四兵, 余翰泽, 李依林. 四川盆地下寒武统筇竹寺组沉积特征及其对构造的响应 . 沉积学报, 2021, 39(4): 1004-1019. doi: 10.14027/j.issn.1000-0550.2020.041
[7]	侯阳红, 康志宏, 赵晨君, 余旭东, 王恩博. 下扬子地区下寒武统幕府山组黑色岩系地球化学特征及其地质意义 . 沉积学报, 2020, 38(4): 886-897. doi: 10.14027/j.issn.1000-0550.2019.076
[8]	李相博, 刘化清, 潘树新, 王菁. 中国湖相沉积物重力流研究的过去、现在与未来 . 沉积学报, 2019, 37(5): 904-921. doi: 10.14027/j.issn.1000-0550.2018.193
[9]	陈超, 潘志龙, 修迪, 魏文通, 张金龙, 张欢, 王硕, 常致凯, 王仁霞. 北山地区红柳园组沉积时代、沉积环境及源区构造背景分析 . 沉积学报, 2017, 35(3): 470-479. doi: 10.14027/j.cnki.cjxb.2017.03.005
[10]	. 贺兰山地区中奥陶统樱桃沟组物源及构造背景分析 . 沉积学报, 2014, 32(2): 205-217.
[11]	李娟于炳松郭峰. 黔北地区下寒武统底部黑色页岩沉积环境条件与源区构造背景分析 . 沉积学报, 2013, 31(1): 20-31.
[12]	李运振. 中国近海新生代盆地沉积环境演变分析 . 沉积学报, 2010, 28(6): 1066-1075.
[13]	赵小明. 青海南部治多—杂多地区石炭纪—三叠纪砂岩地球化学特征与构造背景探讨 . 沉积学报, 2008, 26(1): 11-20.
[14]	王伟涛. 黑龙江省绥滨坳陷下白垩统碎屑岩源区分析及其构造意义 . 沉积学报, 2007, 25(2): 201-206.
[15]	周江羽, 王江海, 尹安, Spurlin M S, Horton B K. 青藏东北缘早第三纪盆地充填的沉积型式及构造背景——以囊谦和下拉秀盆地为例 . 沉积学报, 2002, 20(1): 85-91.
[16]	郑荣才, 彭军, 吴朝容. 陆相盆地基准面旋回的级次划分和研究意义 . 沉积学报, 2001, 19(2): 249-255.
[17]	方维萱, 芦继英. 陕西银硐子-大西沟菱铁银多金属矿床热水沉积岩相特征及成因 . 沉积学报, 2000, 18(3): 431-438.
[18]	张强, 邵震杰. 走滑环境中陆相盆地充填层序特征以云南先锋盆地为例 . 沉积学报, 1997, 15(4): 30-37.
[19]	程日辉, 刘招君, 王东坡. 陆相盆地充填层序的类型——以辽西地区中生代盆地为例 . 沉积学报, 1997, 15(3): 166-170.
[20]	陈功. 外生铀矿床成矿铀质来源与资源评价若干问题 . 沉积学报, 1987, 5(3): 59-65.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 520
HTML全文浏览量: 3
PDF下载量: 440
被引次数: 0

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.

全文HTML

参考文献 (1)

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

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

计量

Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process

计量

目录

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

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

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

计量

出版历程

Relationship between Sedimentary Process in Terrestrial Basin and Tectonic Process

计量

出版历程

目录

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

全文HTML

目录

友情链接

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