库车前陆盆地白垩系层序地层样式及控制因素分析

严德天 王 华 王家豪 王清晨

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

库车前陆盆地白垩系层序地层样式及控制因素分析

严德天王华王家豪王清晨

中国科学院地质与地球物理研究所北京 100101

详细信息

中图分类号: P539.2

计量

文章访问数: 718
HTML全文浏览量: 13
PDF下载量: 399
被引次数: 0

Analysis of the Cretaceous Sequence-stratigraphic Pattern and Controlling Factors in Kuna Foreland Basin

YAN De-tian

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101

摘要

摘要: 白垩系库车坳陷是在南天山强烈逆冲导致的挠曲沉降背景下发育的前陆盆地。综合地震、钻井和露头资料对白垩系进行了层序地层划分,共分出2个区域性的沉积旋回或构造层序、8个三级层序;区内各层序及其内部体系域总体呈现东西向展布、南北向分异的特点;建立了两种层序地层学框架模式:卡普沙良群构造层序具有典型前陆盆地挤压深陷特征,沉积构成反映了从前陆逆冲挠曲沉降到回弹上隆的演化过程;巴什基齐克组构造层序具有宽缓、伸展的特点,层序地层框架模式及内部地层构成样式有其独特性。白垩系前陆盆地的层序地层格架和沉积体系域的配置受到前陆构造作用的控制,而气候及湖平面变化则主要影响层序地层格架内的沉积相类型。
- 库车前陆盆地 /
- 层序地层样式 /
- 控制因素 /
- 白垩系
Abstract: The cretaceous Kuqa depression is a foreland basin generated by flexural subsidence resulting from the southward thrusting of the southern Tianshan Mountains. This paper has divided Cretaceous sequence stratigraphy of Kuqa foreland basin into two tectonic sequences and eight 3rd order sequences based on outcrops, well loggings and seismographic profiles. The sequences and system tracts in the Kuqa foreland basin spread from east to west as a whole and vary obviously from south to north. Two different models of sequence stratigraphic framework were established through studying the internal composition of sequence strata and boundary of individual sequences. In the kapushaliangqun group, this basin appeared as a strong compressive piedmont alluvial-hungry basin, a typical foreland basin. The development of sequence is attributed to the foreland tectonic process from flexural subsidence caused by thrust loading to rebounded uplift due to the erosion and stress release. In contrast, the basin shows smooth and expansive features in the bashijiqike age，and it has a unique model of sequence stratigraphy framework and special internal stratigraphic composition. The sequence framework and depositional pattern of the Cretaceous foreland basin were predominantly determined by the foreland tectonism and the changes of climate mainly impacted on sedimentary facies within sequence frameworks.
- Kuqa foreland basin /
- sequence-stratigraphic pattern /
- controlling factors /
- cretaceous

HTML全文

参考文献(0)

[1]	于乐丹, 彭军, 许天宇, 韩浩东, 杨一茗. 陆相断陷咸化湖盆细粒沉积地层有机质富集特征及控制因素分析 . 沉积学报, 2024, 42(2): 701-722. doi: 10.14027/j.issn.1000-0550.2022.096
[2]	王金艺, 金振奎, 王昕尧, 任奕霖, 程浩, 焦盼盼. 陆相细粒岩储层质量的控制因素 . 沉积学报, 2023, 41(2): 646-659. doi: 10.14027/j.issn.1000-0550.2021.092
[3]	操应长, 燕苗苗, 葸克来, 吴松涛, 朱宁, 朱如凯. 玛湖凹陷夏子街地区三叠系百口泉组砂砾岩储层特征及控制因素 . 沉积学报, 2019, 37(5): 945-956. doi: 10.14027/j.issn.1000-0550.2019.002
[4]	曾庆鲁, 张荣虎, 王力宝, 赵继龙, 佘敏. 库车坳陷白垩系深层致密砂岩储层溶蚀作用实验模拟研究 . 沉积学报, 2018, 36(5): 946-956. doi: 10.14027/j.issn.1000-0550.2018.079
[5]	郭颖, 王粤川, 韦阿娟, 吴昊明, 叶涛, 高坤顺, 曾金昌. 潜山内幕火山岩储层特征及控制因素——以渤海海域秦皇岛30A地区白垩系为例 . 沉积学报, 2017, 35(2): 343-357. doi: 10.14027/j.cnki.cjxb.2017.02.012
[6]	郭沫贞, 徐洋, 寿建峰, 刘占国, 韩守华. 准噶尔盆地西北缘二叠系碎屑岩次生孔隙发育控制因素 . 沉积学报, 2017, 35(2): 330-342. doi: 10.14027/j.cnki.cjxb.2017.02.011
[7]	张金友. 陆相坳陷盆地烃源岩内致密砂岩储层含油性主控因素——以松辽盆地北部中央坳陷区齐家凹陷高台子油层为例 . 沉积学报, 2016, 34(5): 991-1002. doi: 10.14027/j.cnki.cjxb.2016.05.018
[8]	王颖, 王晓州, 廖计华, 朱石磊, 蔡露露. 巴西桑托斯盆地白垩系湖相藻叠层石礁特征及主控因素分析 . 沉积学报, 2016, 34(5): 819-829. doi: 10.14027/j.cnki.cjxb.2016.05.002
[9]	斯春松, 刘占国, 寿建峰, 李积永, 宫清顺, 张庆丰, 王鹏, 王波. 柴达木盆地昆北地区路乐河组砂砾岩有效储层发育主控因素及分布规律 . 沉积学报, 2014, 32(5): 966-972.
[10]	刘畅, 张琴, 谢寅符, 乔李井宇, 孙杰夫, 梅啸寒. 厄瓜多尔Oriente盆地东北部区块白垩系层序地层格架及发育模式 . 沉积学报, 2014, 32(6): 1123-1131.
[11]	. 库车前陆盆地上侏罗统—下白垩统砾岩特征与构造演化关系 . 沉积学报, 2013, 31(6): 980-993.
[12]	王峰. 鄂尔多斯盆地北部上古生界盒8储层特征及控制因素分析 . 沉积学报, 2009, 27(2): 238-245.
[13]	朱志敏. 阜新盆地白垩系沙海组煤层气系统 . 沉积学报, 2008, 26(3): 426-434.
[14]	. 库车坳陷北部白垩系沉积速率分析 . 沉积学报, 2006, 24(05): 641-649.
[15]	严德天, 王华, 王家豪, 王清晨. 库车前陆盆地白垩系层序地层样式及控制因素分析 . 沉积学报, 2006, (6): 841-848.
[16]	郭彦如. 银额盆地查干断陷闭流湖盆层序的控制因素与形成机理 . 沉积学报, 2004, 22(2): 295-301.
[17]	杨剑萍, 许正豪, 姜在兴, 操应长, 陈发亮. 山东惠民凹陷中央隆起带古近系沙河街组层序地层特征及控制因素研究 . 沉积学报, 2003, 21(4): 670-674.
[18]	朱筱敏, 王贵文, 李滨阳, 马立驰, 孙月平, 雷安贵, 程建平. 开鲁盆地陆西凹陷下白垩统层序地层学和油气评价 . 沉积学报, 2002, 20(4): 531-536.
[19]	金振奎, 邹元荣, 蒋春雷, 由伟丰. 大港探区奥陶系岩溶储层发育分布控制因素 . 沉积学报, 2001, 19(4): 530-535.
[20]	王随继, 任明达, 黄杏珍, 李建青, 赵东升. 柴达木盆地第三系粘土矿物横向分布规律及控制因素研究 . 沉积学报, 1997, 15(3): 153-157,165.

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: 718
HTML全文浏览量: 13
PDF下载量: 399
被引次数: 0

库车前陆盆地白垩系层序地层样式及控制因素分析

中国科学院地质与地球物理研究所北京 100101

收稿日期: 2006-01-21

修回日期: 2006-03-27

刊出日期: 2006-12-10

中图分类号: P539.2

关键词:

摘要: 白垩系库车坳陷是在南天山强烈逆冲导致的挠曲沉降背景下发育的前陆盆地。综合地震、钻井和露头资料对白垩系进行了层序地层划分,共分出2个区域性的沉积旋回或构造层序、8个三级层序;区内各层序及其内部体系域总体呈现东西向展布、南北向分异的特点;建立了两种层序地层学框架模式:卡普沙良群构造层序具有典型前陆盆地挤压深陷特征,沉积构成反映了从前陆逆冲挠曲沉降到回弹上隆的演化过程;巴什基齐克组构造层序具有宽缓、伸展的特点,层序地层框架模式及内部地层构成样式有其独特性。白垩系前陆盆地的层序地层格架和沉积体系域的配置受到前陆构造作用的控制,而气候及湖平面变化则主要影响层序地层格架内的沉积相类型。

Analysis of the Cretaceous Sequence-stratigraphic Pattern and Controlling Factors in Kuna Foreland Basin

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101

Received Date: 2006-01-21

Rev Recd Date: 2006-03-27

Publish Date: 2006-12-10

Keywords:

Abstract: The cretaceous Kuqa depression is a foreland basin generated by flexural subsidence resulting from the southward thrusting of the southern Tianshan Mountains. This paper has divided Cretaceous sequence stratigraphy of Kuqa foreland basin into two tectonic sequences and eight 3rd order sequences based on outcrops, well loggings and seismographic profiles. The sequences and system tracts in the Kuqa foreland basin spread from east to west as a whole and vary obviously from south to north. Two different models of sequence stratigraphic framework were established through studying the internal composition of sequence strata and boundary of individual sequences. In the kapushaliangqun group, this basin appeared as a strong compressive piedmont alluvial-hungry basin, a typical foreland basin. The development of sequence is attributed to the foreland tectonic process from flexural subsidence caused by thrust loading to rebounded uplift due to the erosion and stress release. In contrast, the basin shows smooth and expansive features in the bashijiqike age，and it has a unique model of sequence stratigraphy framework and special internal stratigraphic composition. The sequence framework and depositional pattern of the Cretaceous foreland basin were predominantly determined by the foreland tectonism and the changes of climate mainly impacted on sedimentary facies within sequence frameworks.

留言板

库车前陆盆地白垩系层序地层样式及控制因素分析

计量

Analysis of the Cretaceous Sequence-stratigraphic Pattern and Controlling Factors in Kuna Foreland Basin

计量

目录

库车前陆盆地白垩系层序地层样式及控制因素分析

中国科学院地质与地球物理研究所北京 100101

English Abstract

Analysis of the Cretaceous Sequence-stratigraphic Pattern and Controlling Factors in Kuna Foreland Basin

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

库车前陆盆地白垩系层序地层样式及控制因素分析

计量

出版历程

Analysis of the Cretaceous Sequence-stratigraphic Pattern and Controlling Factors in Kuna Foreland Basin

计量

出版历程

目录

库车前陆盆地白垩系层序地层样式及控制因素分析

中国科学院地质与地球物理研究所 北京 100101

English Abstract

Analysis of the Cretaceous Sequence-stratigraphic Pattern and Controlling Factors in Kuna Foreland Basin

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101

全文HTML

目录

友情链接

期刊在线

联系我们

中国科学院地质与地球物理研究所北京 100101