百色盆地那读组层序分析与生储盖组合

彭军; 郑荣才; 陈景山

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百色盆地那读组层序分析与生储盖组合

彭军, 郑荣才, 陈景山

文章导航 > 沉积学报 > 2002 > 20(1): 106-111

彭军, 郑荣才, 陈景山. 百色盆地那读组层序分析与生储盖组合[J]. 沉积学报, 2002, 20(1): 106-111.

引用本文:

彭军, 郑荣才, 陈景山. 百色盆地那读组层序分析与生储盖组合[J]. 沉积学报, 2002, 20(1): 106-111.

PENG Jun, ZHENG Rong-cai, CHEN Jing-shan. Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin[J]. Acta Sedimentologica Sinica, 2002, 20(1): 106-111.

Citation:

PENG Jun, ZHENG Rong-cai, CHEN Jing-shan. Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin[J]. Acta Sedimentologica Sinica, 2002, 20(1): 106-111.

彭军, 郑荣才, 陈景山. 百色盆地那读组层序分析与生储盖组合[J]. 沉积学报, 2002, 20(1): 106-111.

引用本文:

彭军, 郑荣才, 陈景山. 百色盆地那读组层序分析与生储盖组合[J]. 沉积学报, 2002, 20(1): 106-111.

PENG Jun, ZHENG Rong-cai, CHEN Jing-shan. Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin[J]. Acta Sedimentologica Sinica, 2002, 20(1): 106-111.

Citation:

PENG Jun, ZHENG Rong-cai, CHEN Jing-shan. Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin[J]. Acta Sedimentologica Sinica, 2002, 20(1): 106-111.

百色盆地那读组层序分析与生储盖组合

1 油气藏地质及开发工程国家重点实验室,西南石油学院,四川南充,637001;
2 油气藏地质及开发工程国家重点实验室,成都理工学院,成都,610059

详细信息

作者简介:
彭军男 1968年出生博士后(副教授) 沉积学与层序地层学

中图分类号: P539.2

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文章访问数: 387
HTML全文浏览量: 1
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Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin

1 State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum Institute, Nanchong Sichuan 637001;
2 State Key Laboratory of oil and gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 6l0059

摘要

摘要: 通过野外露头、钻井岩心、测井曲线和地震资料的综合分析,在识别出 4类不同成因类型和规模的层序界面基础上,将百色盆地那读组划分为 1个超长期、5个长期和 16个中期基准面旋回层序。并详细地讨论了层序与生储盖组合的关系,指出生储盖组合特征与长期基准面旋回关系最为密切,有利储层发育位置主要出现在长期基准面上升半旋回的早中期和下降半旋回的中晚期,转换面附近则是烃源岩和盖层的发育位置;各长期旋回层序的生储盖组合具不同特征,明显受基准面升降幅度、频率及其所影响的相组合、可容纳空间和A/S值变化控制;按生储盖组合在垂向和纵向上的配置关系,可划分为上生下储、下生上储、侧向运移等 3种基本组合类型。
- 基准面旋回 /
- 层序界面 /
- 层序分析 /
- 生储盖组合 /
- 那读组 /
- 百色盆地
Abstract: Through the comprehensive analysis of out crop, rock cores, well loggings and seismic data, one super-long-term, five long-term and sixteen middle-term base-level cycle sequences are distinguished in Nadu Formation of Baise basin. In this paper, the relationship between the source-reservoir-cap associations and the base-level cycle sequences of Nadu Formation are discussed in detail, and some knowledge is acquired as follows: (1) long-term base-level cycles bear close relation to source-reservoir-cap rock associtations,the main reservoir sand bodies develop in the early-middle stage of the uprising periods and middle-late stage of subsiding periods of the long-term base-level cycle, and the main hydrocarbon source rocks and favourable regional cap rocks develop at the turning position from uprising to subsiding of the long-term base-level cylce; (2) the characteristics of source-reservoir-cap rock associations developed in each long-term base-level cycle are distinctly different and controlled by the frequency, amplitude of the rising and falling of the base-level, facies association, accommodation and A/S ratio; (3) according to the spatial relationship of source rocks, reservoir rocks and cap rocks in the vertical or horizontal section of the formation, three types of basic associations can be divided. The first associations is usually of the type with source rocks in the upper and reservoirs below, the second one with source rocks below and reservoirs in the upper, and the third one with source rocks in other district.
- base-level cycle /
- sequence interface /
- sequence analysis /
- source-reservoir-cap rock association /
- Nadu Formation /
- Baise basin

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参考文献(7)

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[3]	王洪亮,邓宏文.地层基准面原理在湖相储层预测中的应用[J].石油与天然气地质,1997,18(2):96～102
[4]	郑荣才.四川盆地下侏罗统大安寨段高分辨率层序地层学[J].沉积学报,1998,16(2):42～49
[5]	郑荣才,吴朝容.西部凹陷深层沙河街组生储盖组合的层序分析[J].成都理工学院学报,1999,26(4):348～356
[6]	吴朝容,郑荣才.辽河油田西部洼陷沙河街组高分辨率层序地层学特征[J].成都理工学院学报,1999,26(4):375～381
[7]	柳梅青,陈亦军,郑荣才.川西新场气田蓬莱镇组陆相地层高分辨率层序地层学研究[J].沉积学报,2000,18(1):50～56

[1]	李跃, 李军辉, 王子赫, 李美芳, 娄洪, 王琦, 孙海雷. 陆相断陷湖盆基准面旋回对沉积砂体的控制——以海拉尔盆地贝尔凹陷贝西地区为例 . 沉积学报, 2019, 37(4): 858-867. doi: 10.14027/j.issn.1000-0550.2018.179
[2]	钟原, 刘宏, 谭秀成, 连承波, 廖纪佳, 刘明洁, 胡广, 曹剑. 富砂地层格架高分辨率层序地层学研究及储层甜点预测——以四川盆地合川地区须家河组为例 . 沉积学报, 2016, 34(4): 758-774. doi: 10.14027/j.cnki.cjxb.2016.04.016
[3]	杨延强, 吴胜和, 岳大力, 兰献娇, 李艳杰, 沈云奇. 长期基准面旋回内河口坝构型的演化规律——以胜坨油田坨7断块沙二段下油组为例 . 沉积学报, 2015, 33(2): 326-336. doi: 10.14027/j.cnki.cjxb.2015.02.012
[4]	. 鄂尔多斯盆地奥陶系层序地层格架 . 沉积学报, 2014, 32(1): 44-60.
[5]	. 地层记录中旋回层序界面的识别方法及原理 . 沉积学报, 2012, 30(6): 991-998.
[6]	张世广. 高分辨率层序地层学在储层宏观非均质性研究中的应用——以松辽盆地朝阳沟油田朝1—朝气3区块扶余油层为例 . 沉积学报, 2009, 27(3): 458-469.
[7]	刘新颖. 印尼Sunda盆地裂陷期层序地层与沉积充填特征 . 沉积学报, 2009, 27(2): 280-288.
[8]	袁红旗. 海拉尔盆地查干诺尔凹陷下白垩统层序地层学研究 . 沉积学报, 2008, 26(2): 241-248.
[9]	辛仁臣. 湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例 . 沉积学报, 2008, 26(1): 77-85.
[10]	唐民安. 大牛地气田下石盒子组基准面旋回与储层流动单元的层次性 . 沉积学报, 2007, 25(1): 39-47.
[11]	罗忠. 层序界面对砂岩成岩作用及储层质量的影响——以鄂尔多斯盆地延河露头上三叠统延长组为例 . 沉积学报, 2007, 25(6): 903-914.
[12]	梁积伟. 鄂尔多斯盆地东北部山西组高分辨层序地层学研究 . 沉积学报, 2006, 24(2): 251-258.
[13]	操应长, 姜在兴, 夏斌, 杨伟利, 张家震. 声波时差测井资料识别层序地层单元界面的方法、原理及实例 . 沉积学报, 2003, 21(2): 318-323.
[14]	赵俊兴, 陈洪德, 向芳. 鄂尔多斯盆地中部延安地区中侏罗统延安组高分辨率层序地层研究 . 沉积学报, 2003, 21(2): 307-312.
[15]	郑荣才, 彭军, 彭光明, 盘昌林, 高红灿. 高分辨率层序分析在油藏开发工程中的应用——以百色盆地仑35块那二段油藏为例 . 沉积学报, 2003, 21(4): 654-662.
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百色盆地那读组层序分析与生储盖组合

1 油气藏地质及开发工程国家重点实验室,西南石油学院,四川南充,637001;

2 油气藏地质及开发工程国家重点实验室,成都理工学院,成都,610059

作者简介:
彭军男 1968年出生博士后(副教授) 沉积学与层序地层学

收稿日期: 2001-07-04

中图分类号: P539.2

关键词:

那读组 /

摘要: 通过野外露头、钻井岩心、测井曲线和地震资料的综合分析,在识别出 4类不同成因类型和规模的层序界面基础上,将百色盆地那读组划分为 1个超长期、5个长期和 16个中期基准面旋回层序。并详细地讨论了层序与生储盖组合的关系,指出生储盖组合特征与长期基准面旋回关系最为密切,有利储层发育位置主要出现在长期基准面上升半旋回的早中期和下降半旋回的中晚期,转换面附近则是烃源岩和盖层的发育位置;各长期旋回层序的生储盖组合具不同特征,明显受基准面升降幅度、频率及其所影响的相组合、可容纳空间和A/S值变化控制;按生储盖组合在垂向和纵向上的配置关系,可划分为上生下储、下生上储、侧向运移等 3种基本组合类型。

English Abstract

Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin

1 State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum Institute, Nanchong Sichuan 637001;

2 State Key Laboratory of oil and gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 6l0059

Received Date: 2001-07-04

Keywords:

Abstract: Through the comprehensive analysis of out crop, rock cores, well loggings and seismic data, one super-long-term, five long-term and sixteen middle-term base-level cycle sequences are distinguished in Nadu Formation of Baise basin. In this paper, the relationship between the source-reservoir-cap associations and the base-level cycle sequences of Nadu Formation are discussed in detail, and some knowledge is acquired as follows: (1) long-term base-level cycles bear close relation to source-reservoir-cap rock associtations,the main reservoir sand bodies develop in the early-middle stage of the uprising periods and middle-late stage of subsiding periods of the long-term base-level cycle, and the main hydrocarbon source rocks and favourable regional cap rocks develop at the turning position from uprising to subsiding of the long-term base-level cylce; (2) the characteristics of source-reservoir-cap rock associations developed in each long-term base-level cycle are distinctly different and controlled by the frequency, amplitude of the rising and falling of the base-level, facies association, accommodation and A/S ratio; (3) according to the spatial relationship of source rocks, reservoir rocks and cap rocks in the vertical or horizontal section of the formation, three types of basic associations can be divided. The first associations is usually of the type with source rocks in the upper and reservoirs below, the second one with source rocks below and reservoirs in the upper, and the third one with source rocks in other district.

彭军, 郑荣才, 陈景山. 百色盆地那读组层序分析与生储盖组合[J]. 沉积学报, 2002, 20(1): 106-111.

引用本文:

彭军, 郑荣才, 陈景山. 百色盆地那读组层序分析与生储盖组合[J]. 沉积学报, 2002, 20(1): 106-111.

PENG Jun, ZHENG Rong-cai, CHEN Jing-shan. Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin[J]. Acta Sedimentologica Sinica, 2002, 20(1): 106-111.

Citation:

PENG Jun, ZHENG Rong-cai, CHEN Jing-shan. Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin[J]. Acta Sedimentologica Sinica, 2002, 20(1): 106-111.

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百色盆地那读组层序分析与生储盖组合

作者简介:
彭军男 1968年出生博士后(副教授) 沉积学与层序地层学

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Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin

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目录

百色盆地那读组层序分析与生储盖组合

1 油气藏地质及开发工程国家重点实验室,西南石油学院,四川南充,637001;

2 油气藏地质及开发工程国家重点实验室,成都理工学院,成都,610059

作者简介:
彭军男 1968年出生博士后(副教授) 沉积学与层序地层学

English Abstract

Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin

1 State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum Institute, Nanchong Sichuan 637001;

2 State Key Laboratory of oil and gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 6l0059

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百色盆地那读组层序分析与生储盖组合

作者简介: 彭军 男 1968年出生 博士 后(副教授) 沉积学与层序地层学

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Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin

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百色盆地那读组层序分析与生储盖组合

1 油气藏地质及开发工程国家重点实验室,西南石油学院,四川南充,637001; 2 油气藏地质及开发工程国家重点实验室,成都理工学院,成都,610059

作者简介: 彭军 男 1968年出生 博士 后(副教授) 沉积学与层序地层学

English Abstract

Sequence Analysis and Source-Reservoir-Cap Rock Associations of Nadu Formation in Baise Basin

1 State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum Institute, Nanchong Sichuan 637001; 2 State Key Laboratory of oil and gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 6l0059

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
彭军男 1968年出生博士后(副教授) 沉积学与层序地层学

1 油气藏地质及开发工程国家重点实验室,西南石油学院,四川南充,637001;

2 油气藏地质及开发工程国家重点实验室,成都理工学院,成都,610059

作者简介:
彭军男 1968年出生博士后(副教授) 沉积学与层序地层学

1 State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum Institute, Nanchong Sichuan 637001;

2 State Key Laboratory of oil and gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 6l0059