塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征

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塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征

高志前

文章导航 > 沉积学报 > 2006 > 24(1): 19-27

高志前. 塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征[J]. 沉积学报, 2006, 24(1): 19-27.

引用本文:

高志前. 塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征[J]. 沉积学报, 2006, 24(1): 19-27.

GAO Zhiqian. The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin[J]. Acta Sedimentologica Sinica, 2006, 24(1): 19-27.

Citation:

GAO Zhiqian. The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin[J]. Acta Sedimentologica Sinica, 2006, 24(1): 19-27.

高志前. 塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征[J]. 沉积学报, 2006, 24(1): 19-27.

引用本文:

高志前. 塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征[J]. 沉积学报, 2006, 24(1): 19-27.

GAO Zhiqian. The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin[J]. Acta Sedimentologica Sinica, 2006, 24(1): 19-27.

Citation:

GAO Zhiqian. The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin[J]. Acta Sedimentologica Sinica, 2006, 24(1): 19-27.

塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征

高志前

中国地质大学(北京)能源学院北京 100083

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高志前

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The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin

GAO Zhiqian

School of Energy Resources, China University of Geosciences, Beijing 100083

More Information

Corresponding author: GAO Zhiqian

摘要

摘要: 从寒武纪到奥陶纪，塔里木盆地经历了早、中寒武世缓坡型碳酸盐岩台地，晚寒武世—早中奥陶世弱镶边斜坡型碳酸盐岩台地，晚奥陶世早期孤立型碳酸盐岩台地和晚奥陶世中晚期淹没型碳酸盐岩台地四种不同台地结构型式的演变。不同类型的碳酸盐岩台地在其剖面结构、台地边缘特征、沉积相构成等方面有着显著差异，它控制了不同区域沉积相类型和特征，并决定了烃源岩、储集岩和区域盖层的发育条件和展布规律。通过地震、钻井层序地层分析，总结出了不同类型的碳酸盐岩台地结构的层序—沉积相模式。在碳酸盐岩台地演变过程中，塔里木盆地发育二期坡折带：寒武纪—早中奥陶世形成第一期坡折带，沿着库南1井—满参1井—塔东2井一线分布，呈向西凸伸的弧形带；晚奥陶世发育第二期坡折带，由库南1井—满参1井—塔中1井—塘参1井延伸，呈向东凸伸的弧形带。坡折带的迁移变化，反映着台地样式的转变。
- 塔里木盆地 /
- 寒武—奥陶系 /
- 台地结构 /
- 沉积演化 /
- 层序—沉积相模式
Abstract: Tarim basin underwent the ramp carbonate platform of earlymiddle Cambrian, rimmed shelf carbonate platform of late Cambrianearly middle Ordovician, isolated carbonate platform in the early period of late Ordovician, and drowned carbonate platform in the middlelate period of late Ordovician. The different carbonate platform has distinct diversities in the section structure, platform edge feature and facies constitution, and controls the types and features of facies in the different regions and the upgrowth condition and the distribution rule of source rock, reservoir and caps. Through the sequence stratigraphy study of the seismic and loggings, 4 types of carbonate platform structure have been established and 5 sequencefacies models been summarized. During carbonate platform evolvement, two periods of platform slope are developed: The first platform slope is formed in Cambrianearly middle Ordovician, controlled by Well Kunan 1, WellMancan 1, WellTadong 2 route, represents arc belt toward the west. The second platform slope is formed in the late Ordovician, constrained by Well Kunan 1, WellMancan 1, WellTazhong 1 and WellTangcan 1, represents arc belt toward the east. The shifting and variation of the slope reveals the change of carbonate platform types.
- Tarim basin /
- CambrianOrdovician /
- platform structure /
- depositional evolvement /
- sequencefacies model

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[1]	朱永进, 沈安江, 刘玲利, 陈永权, 俞广. 塔里木盆地晚震旦世—中寒武世构造沉积充填过程及油气勘探地位 . 沉积学报, 2020, 38(2): 398-410. doi: 10.14027/j.issn.1000-0550.2019.045
[2]	朱永进, 倪新锋, 刘玲利, 乔占峰, 陈永权, 郑剑锋. 裂后沉降期碳酸盐岩缓坡沉积响应及成储特征——以塔里木盆地下寒武统肖尔布拉克组为例 . 沉积学报, 2019, 37(5): 1044-1057. doi: 10.14027/j.issn.1000-0550.2019.006
[3]	邓世彪, 关平, 李保华, 刘沛显, 陈永权. 塔里木盆地下寒武统台缘带沉积结构特征及其形成过程 . 沉积学报, 2018, 36(4): 706-721. doi: 10.14027/j.issn.1000-0550.2018.059
[4]	杨伟利, 王毅, 张众琛, 梁晨, 李京昌. 塔里木盆地顺南地区中-下奥陶统正演沉积数值模拟 . 沉积学报, 2017, 35(1): 117-123. doi: 10.14027/j.cnki.cjxb.2017.01.012
[5]	韩杰, 吴萧, 潘文庆, 江杰, 张敏. 塔里木盆地西北缘巴楚—乌什露头区奥陶系沉积相特征 . 沉积学报, 2015, 33(4): 764-772. doi: 10.14027/j.cnki.cjxb.2015.04.015
[6]	. 塔里木盆地奥陶系碳酸盐岩颗粒滩沉积组合及展布特征 . 沉积学报, 2014, 32(3): 418-428.
[7]	屈海洲, 王振宇, 张正红, 张云峰, 于红枫, 郑剑. 塔中地区晚奥陶世镶边台地沉积演化 . 沉积学报, 2014, 32(5): 823-831.
[8]	. 塔里木盆地北部三叠系“二元”层序结构特征及演化模式 . 沉积学报, 2014, 32(2): 325-333.
[9]	. 塔里木盆地奥陶纪碳酸盐岩台地的层序结构演化及其对盆地过程的响应 . 沉积学报, 2013, 31(05): 907-919.
[10]	. 塔里木盆地西北缘乌恰地区晚白垩世—渐新世微相分析及沉积演化 . 沉积学报, 2012, 30(3): 501-510.
[11]	倪新锋. 塔里木盆地英买力—哈拉哈塘地区奥陶系碳酸盐岩岩溶型储层特征及成因 . 沉积学报, 2011, 29(3): 465-474.
[12]	陈景山. 塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布 . 沉积学报, 2007, 25(6): 858-868.
[13]	杨帆, 贾进华. 塔里木盆地乌什凹陷白垩系冲积扇—扇三角洲沉积相及有利储盖组合 . 沉积学报, 2006, (5): 681-689.
[14]	. 塔里木盆地乌什凹陷白垩系冲积扇—扇三角洲沉积相及有利储盖组合 . 沉积学报, 2006, 24(05): 681-689.
[15]	谭秀成王振宇李凌孙崇浩陈景山曹剑. 库车前陆盆地第三系沉积相配置及演化研究 . 沉积学报, 2006, 24(06): 790-797.
[16]	卫平生, 李天顺, 李安春, 王建功. 巴彦浩特盆地石炭系沉积相及沉积演化 . 沉积学报, 2005, 23(2): 240-247.
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[20]	王毅, 纪友亮, 熊继辉, 田海芹. 塔里木盆地上泥盆统与石炭系层序地层分析 . 沉积学报, 1998, 16(2): 74-81.

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塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征

高志前

中国地质大学(北京)能源学院北京 100083

通讯作者: 高志前

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2006-02-10

关键词:

摘要: 从寒武纪到奥陶纪，塔里木盆地经历了早、中寒武世缓坡型碳酸盐岩台地，晚寒武世—早中奥陶世弱镶边斜坡型碳酸盐岩台地，晚奥陶世早期孤立型碳酸盐岩台地和晚奥陶世中晚期淹没型碳酸盐岩台地四种不同台地结构型式的演变。不同类型的碳酸盐岩台地在其剖面结构、台地边缘特征、沉积相构成等方面有着显著差异，它控制了不同区域沉积相类型和特征，并决定了烃源岩、储集岩和区域盖层的发育条件和展布规律。通过地震、钻井层序地层分析，总结出了不同类型的碳酸盐岩台地结构的层序—沉积相模式。在碳酸盐岩台地演变过程中，塔里木盆地发育二期坡折带：寒武纪—早中奥陶世形成第一期坡折带，沿着库南1井—满参1井—塔东2井一线分布，呈向西凸伸的弧形带；晚奥陶世发育第二期坡折带，由库南1井—满参1井—塔中1井—塘参1井延伸，呈向东凸伸的弧形带。坡折带的迁移变化，反映着台地样式的转变。

English Abstract

The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin

GAO Zhiqian

School of Energy Resources, China University of Geosciences, Beijing 100083

Corresponding author: GAO Zhiqian

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2006-02-10

Keywords:

Abstract: Tarim basin underwent the ramp carbonate platform of earlymiddle Cambrian, rimmed shelf carbonate platform of late Cambrianearly middle Ordovician, isolated carbonate platform in the early period of late Ordovician, and drowned carbonate platform in the middlelate period of late Ordovician. The different carbonate platform has distinct diversities in the section structure, platform edge feature and facies constitution, and controls the types and features of facies in the different regions and the upgrowth condition and the distribution rule of source rock, reservoir and caps. Through the sequence stratigraphy study of the seismic and loggings, 4 types of carbonate platform structure have been established and 5 sequencefacies models been summarized. During carbonate platform evolvement, two periods of platform slope are developed: The first platform slope is formed in Cambrianearly middle Ordovician, controlled by Well Kunan 1, WellMancan 1, WellTadong 2 route, represents arc belt toward the west. The second platform slope is formed in the late Ordovician, constrained by Well Kunan 1, WellMancan 1, WellTazhong 1 and WellTangcan 1, represents arc belt toward the east. The shifting and variation of the slope reveals the change of carbonate platform types.

高志前. 塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征[J]. 沉积学报, 2006, 24(1): 19-27.

引用本文:

高志前. 塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征[J]. 沉积学报, 2006, 24(1): 19-27.

GAO Zhiqian. The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin[J]. Acta Sedimentologica Sinica, 2006, 24(1): 19-27.

Citation:

GAO Zhiqian. The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin[J]. Acta Sedimentologica Sinica, 2006, 24(1): 19-27.

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塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征

通讯作者:
高志前

计量

The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin

Corresponding author: GAO Zhiqian

计量

目录

塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征

中国地质大学(北京)能源学院北京 100083

通讯作者: 高志前

English Abstract

The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin

School of Energy Resources, China University of Geosciences, Beijing 100083

Corresponding author: GAO Zhiqian

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塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征

通讯作者: 高志前

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The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin

Corresponding author: GAO Zhiqian

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出版历程

目录

塔里木盆地寒武—奥陶系碳酸盐岩台地样式及其沉积响应特征

中国地质大学(北京)能源学院 北京 100083

通讯作者: 高志前

English Abstract

The Structural Types and Depositional Characteristics of Carbonate Platform in the CambrianOrdovician of Tarim Basin

School of Energy Resources, China University of Geosciences, Beijing 100083

Corresponding author: GAO Zhiqian

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期刊在线

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通讯作者:
高志前

中国地质大学(北京)能源学院北京 100083