南堡凹陷东营组层序地层格架与沉积体系

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南堡凹陷东营组层序地层格架与沉积体系

管红

文章导航 > 沉积学报 > 2008 > 26(5): 730-736

管红. 南堡凹陷东营组层序地层格架与沉积体系[J]. 沉积学报, 2008, 26(5): 730-736.

引用本文:

管红. 南堡凹陷东营组层序地层格架与沉积体系[J]. 沉积学报, 2008, 26(5): 730-736.

GUAN Hong. Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin[J]. Acta Sedimentologica Sinica, 2008, 26(5): 730-736.

Citation:

GUAN Hong. Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin[J]. Acta Sedimentologica Sinica, 2008, 26(5): 730-736.

管红. 南堡凹陷东营组层序地层格架与沉积体系[J]. 沉积学报, 2008, 26(5): 730-736.

引用本文:

管红. 南堡凹陷东营组层序地层格架与沉积体系[J]. 沉积学报, 2008, 26(5): 730-736.

GUAN Hong. Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin[J]. Acta Sedimentologica Sinica, 2008, 26(5): 730-736.

Citation:

GUAN Hong. Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin[J]. Acta Sedimentologica Sinica, 2008, 26(5): 730-736.

南堡凹陷东营组层序地层格架与沉积体系

管红

中国石油大学(北京)资源与信息学院北京 102249

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Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin

GUAN Hong

China University of Petroleum, Beijing 102249

More Information

Corresponding author: GUAN Hong

摘要

摘要: 通过对地震、岩心、钻、测井资料综合分析，将东营组划分为1个二级层序、3个三级层序。并根据初次湖泛面和最大湖泛面特征将每个层序进一步划分为低位域、湖侵域和高位域等三个体系域。层序格架和展布受凹陷结构和断裂活动影响，高柳断层以北地区东营组沉积厚度薄，且后期剥蚀严重。南部滩海地区的各层序完整，厚度相对稳定。在层序格架内分析了南堡凹陷东营组的沉积体系，东北部陡坡带以发育水下扇、扇三角洲为主，西北部和南部缓坡带发育三角洲、扇三角洲和辫状河三角洲。层序界面、准层序（组）叠加样式以及沉积体系空间展布均受到构造活动的控制，强构造活动期形成退积式叠加模式，而弱构造活动期对应进积式叠加模式。对层序发育和油气成藏条件分析认为层序1低位域的扇三角洲砂体和层序2中的浊积砂体为寻找岩性油气藏的有利部位。
- 层序地层格架 /
- 体系域 /
- 控制因素 /
- 沉积体系 /
- 东营组 /
- 南堡凹陷
Abstract: Comprehensively using the drilling, logging and seismic data, based on the boundary characteristics of the sequence systems tract, sequences of Ed Formation in Paleogene in the area of Nanpu sag were classified. Ed Formations were divided into three sedimentary sequences. By tracing MFS and FFS, lowstand, transgressive and highstand system tracts was ascertained. The basin palaeogeography and fault activity have influenced on framework and distributions of the sequence. On the area of hangingwall of Gaoliu fault, Ed Formation was thin and eroded hardly, especially in Liuzan region. The centre of sequence thickness was located on Linque subsag, thickness is more than 2500m.While on the land, average sequence thickness is 1800m. Depositional systems were analysis on sequence stratigraphic framework. On the slope region in the northeast, alluvial fan and fandelta were mainly depositional systems. And braided riverdelta, fan delta and delta were distributed in the northwest and south slope. Tectonic activities were critical controlling factors on sequence system boundary; stack mode and distribution of deposition system. Strong active fault make retrogradation mode, and inertia fault make progradation. The favorable lithological traps are located mainly on fandelta in the lowstand system tracts of sequence1 and on turbidite fan in the sequence 2.
- sequence framework /
- systems tract /
- controlling factor /
- sedimentary system /
- Ed /
- Nanpu Sag

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[1]	赵鑫, 卢政环, 廖飞燕, 时阳, 郭浩, 肖露, 赖锦, 李美俊, 龚承林. 福山凹陷流沙港组储层品质控制因素与优质储层预测 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2023.085
[2]	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
[3]	李跃, 蒙启安, 李军辉, 王琦, 邹越, 娄洪. 贝尔凹陷南屯组物源特征及其对沉积体系的控制 . 沉积学报, 2018, 36(4): 756-767. doi: 10.14027/j.issn.1000-0550.2018.050
[4]	宋爽, 朱筱敏, 于福生, 葛家旺, 史亚会, 贺敬聪, 袁立忠, 刘军. 珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系 . 沉积学报, 2016, 34(2): 222-235. doi: 10.14027/j.cnki.cjxb.2016.02.002
[5]	李欢, 杨香华, 朱红涛, 周心怀, 李建平. 渤中西环古近系东营组物源转换与沉积充填响应 . 沉积学报, 2015, 33(1): 36-48. doi: 10.14027/j.cnki.cjxb.2015.01.004
[6]	刘永福, 赵建华, 范秋海, 林畅松, 叶茂林, 范倩倩, 张荣茜. 塔北隆起中部白垩系卡普沙良群层序地层格架及沉积体系研究 . 沉积学报, 2014, 32(6): 1113-1122.
[7]	. 梨树断陷营城组层序地层格架与沉积相特征 . 沉积学报, 2014, 32(3): 576-585.
[8]	操应长. 东营凹陷西部沙四上亚段滩坝砂体有效储层的物性下限及控制因素 . 沉积学报, 2009, 27(2): 230-237.
[9]	杨俊生. 苏丹Muglad盆地Fula坳陷白垩系Abu Gabra组层序地层及沉积体系 . 沉积学报, 2008, 26(6): 994-1004.
[10]	肖〓毅. 辽河清水洼陷东营组高分辨率层序格架下沉积演化特征及有利区带预测 . 沉积学报, 2008, 26(6): 1014-1020.
[11]	郭彦如刘化清李相博完颜容郑希民. 大型坳陷湖盆层序地层格架的研究方法体系 ———以鄂尔多斯盆地中生界延长组为例 . 沉积学报, 2008, 26(3): 384-391.
[12]	黄传炎. 板桥凹陷断裂陡坡带沙一段层序样式和沉积体系特征及其成藏模式研究 . 沉积学报, 2007, 25(3): 386-391.
[13]	张翔. 塔里木盆地下志留统塔塔埃尔塔格组沉积体系及沉积模式 . 沉积学报, 2006, 24(3): 370-377.
[14]	魏国齐, 陈更生, 杨威, 杨雨, 胡明毅, 张林, 吴世祥, 金惠, 沈珏红. 川北下三叠统飞仙关组“槽台”沉积体系及演化 . 沉积学报, 2004, 22(2): 254-260.
[15]	刘景彦, 陈志勇, 林畅松, 吴志轩. 东海丽水西次凹古新统明月峰组层序—体系域分析及沉积体系展布 . 沉积学报, 2004, 22(3): 380-386.
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[18]	许淑梅, 翟世奎, 李三忠, 周立宏. 歧口凹陷滩海区下第三系层序地层分析及沉积体系研究 . 沉积学报, 2001, 19(3): 363-367.
[19]	郑荣才, 刘文均, 李祥辉, 王洪峰, 陈源仁. 龙门山平驿铺组沉积体系及旋回层序研究^① . 沉积学报, 1997, 15(3): 1-7.
[20]	王多云, 陈应泰, 徐洪生. 受周期性湖平面升降控制的冲积扇—扇三角洲沉积体系——柴达木盆地阿尔金山前西段干柴沟组 . 沉积学报, 1991, 9(4): 43-48.

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南堡凹陷东营组层序地层格架与沉积体系

管红

中国石油大学(北京)资源与信息学院北京 102249

通讯作者: 管红

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2008-10-10

关键词:

体系域 /

东营组 /

摘要: 通过对地震、岩心、钻、测井资料综合分析，将东营组划分为1个二级层序、3个三级层序。并根据初次湖泛面和最大湖泛面特征将每个层序进一步划分为低位域、湖侵域和高位域等三个体系域。层序格架和展布受凹陷结构和断裂活动影响，高柳断层以北地区东营组沉积厚度薄，且后期剥蚀严重。南部滩海地区的各层序完整，厚度相对稳定。在层序格架内分析了南堡凹陷东营组的沉积体系，东北部陡坡带以发育水下扇、扇三角洲为主，西北部和南部缓坡带发育三角洲、扇三角洲和辫状河三角洲。层序界面、准层序（组）叠加样式以及沉积体系空间展布均受到构造活动的控制，强构造活动期形成退积式叠加模式，而弱构造活动期对应进积式叠加模式。对层序发育和油气成藏条件分析认为层序1低位域的扇三角洲砂体和层序2中的浊积砂体为寻找岩性油气藏的有利部位。

English Abstract

Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin

GUAN Hong

China University of Petroleum, Beijing 102249

Corresponding author: GUAN Hong

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2008-10-10

Keywords:

Abstract: Comprehensively using the drilling, logging and seismic data, based on the boundary characteristics of the sequence systems tract, sequences of Ed Formation in Paleogene in the area of Nanpu sag were classified. Ed Formations were divided into three sedimentary sequences. By tracing MFS and FFS, lowstand, transgressive and highstand system tracts was ascertained. The basin palaeogeography and fault activity have influenced on framework and distributions of the sequence. On the area of hangingwall of Gaoliu fault, Ed Formation was thin and eroded hardly, especially in Liuzan region. The centre of sequence thickness was located on Linque subsag, thickness is more than 2500m.While on the land, average sequence thickness is 1800m. Depositional systems were analysis on sequence stratigraphic framework. On the slope region in the northeast, alluvial fan and fandelta were mainly depositional systems. And braided riverdelta, fan delta and delta were distributed in the northwest and south slope. Tectonic activities were critical controlling factors on sequence system boundary; stack mode and distribution of deposition system. Strong active fault make retrogradation mode, and inertia fault make progradation. The favorable lithological traps are located mainly on fandelta in the lowstand system tracts of sequence1 and on turbidite fan in the sequence 2.

管红. 南堡凹陷东营组层序地层格架与沉积体系[J]. 沉积学报, 2008, 26(5): 730-736.

引用本文:

管红. 南堡凹陷东营组层序地层格架与沉积体系[J]. 沉积学报, 2008, 26(5): 730-736.

GUAN Hong. Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin[J]. Acta Sedimentologica Sinica, 2008, 26(5): 730-736.

Citation:

GUAN Hong. Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin[J]. Acta Sedimentologica Sinica, 2008, 26(5): 730-736.

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南堡凹陷东营组层序地层格架与沉积体系

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管红

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Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin

Corresponding author: GUAN Hong

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南堡凹陷东营组层序地层格架与沉积体系

中国石油大学(北京)资源与信息学院北京 102249

通讯作者: 管红

English Abstract

Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin

China University of Petroleum, Beijing 102249

Corresponding author: GUAN Hong

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南堡凹陷东营组层序地层格架与沉积体系

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Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin

Corresponding author: GUAN Hong

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南堡凹陷东营组层序地层格架与沉积体系

中国石油大学(北京)资源与信息学院 北京 102249

通讯作者: 管红

English Abstract

Sequence Framework and Sedimentary Facies of Ed Formation  in Paleogene, Nanpu Sag, Bohai Bay Basin

China University of Petroleum, Beijing 102249

Corresponding author: GUAN Hong

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管红

中国石油大学(北京)资源与信息学院北京 102249