四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制

黄继祥; 曾伟; 张高信; 冉宏

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

四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制

黄继祥, 曾伟, 张高信, 冉宏

文章导航 > 沉积学报 > 1995 > 13(S1): 109-117

黄继祥, 曾伟, 张高信, 冉宏. 四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制[J]. 沉积学报, 1995, 13(S1): 109-117.

引用本文:

黄继祥, 曾伟, 张高信, 冉宏. 四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制[J]. 沉积学报, 1995, 13(S1): 109-117.

Huang Jixiang, Zeng Wei, Zhang Gaoxing, Ran Hong. The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 109-117.

Citation:

Huang Jixiang, Zeng Wei, Zhang Gaoxing, Ran Hong. The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 109-117.

黄继祥, 曾伟, 张高信, 冉宏. 四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制[J]. 沉积学报, 1995, 13(S1): 109-117.

引用本文:

黄继祥, 曾伟, 张高信, 冉宏. 四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制[J]. 沉积学报, 1995, 13(S1): 109-117.

Citation:

Huang Jixiang, Zeng Wei, Zhang Gaoxing, Ran Hong. The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 109-117.

四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制

1 西南石油学院勘探系南充 637001;
2 四川石油川东开发公司重庆 630021

基金项目: 八五国家攻关项目

计量

文章访问数: 378
HTML全文浏览量: 6
PDF下载量: 394
被引次数: 0

The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin

1 Department Exploration of South West Petroleum Insititute, Nanchong 637001;
2 Eastern Development Company of Sichuan Petroleum Bureau, Chongqing 630021

摘要

摘要: 四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育，受海平面相对升降的控制。提出了浅海滩和变浅暴露滩的新分类，分析了滩微相的古地理和层位分布规律，建立了滩的组成模型，总结了滩发育的三种相序模式。变浅暴露滩有有利的生、储和盖组合，发育的孔隙层段，早期形成的沉积－成岩圈闭，控制了各种圈闭中裂缝－孔隙型气藏的形成。上述思想提供了与滩有关的气藏勘探的新思路。
- 四川盆地 /
- 三叠系 /
- 嘉陵江组 /
- 滩 /
- 微相 /
- 气藏
Abstract: The 2-section of Jialingjang Group of Triassic in the eastern part of Sichuan Basin is an important gas bearing position. The Development of bank-micro factes have played an important pole in controlling the gas pool of fracture-pore type in traps.The banks are POint-bank on the platform in upper yangtze epicontinental sea. The new classificantion of shallow-sea bank and shallow exposed banks has been suggested on the basis of the evolution model of depositional environments which were controlled by relative sea-level changes. The similarities and difference of two types of banks have been compared. There were four bank development periods in the multicycle sedements of 2-section of Jialingjiang Group.The distribution of banks in two bank-development periods, for example, the 2-subsection of 2-section, have been mapped. The composition and devolopment model of point-bank at the Tishan anticline has been analysed. It clearly points out that the lithic factes in the core of bank have big thickness and good continuity in the multi-bank development periods. There are three types of factes sequences models:(1) the banks developed with sea-level up and disappeared with sea-level down; (2) the banks developed with sea-level down and disappeared to expose ; and (3) the banks developed with sea-level up and disappeared with sea-level up.Finally, the authors state how the shallow exposed bank control the formation of gas-pool. It has been recognind: ①the bank-microfacies complexs are beneficial for complexs of oil-producing, reservoir and seal formations, ②the shallow exposed bank is the microfacies zone of the pore-layers devolopment, ③ the sediment-diagenetic trap formed in bank-microfacies zone is beneficial for early accumulation of oil and gas pools @the development of pore-layers and accumulation of oil and gas in early sediment-diagenetic traps are the base of present gas -pool of fracture-pore type in various traps.
- Sichuan basin /
- Triassic /
- Jialingjiang Group /
- bank /
- microfactes /
- gas-pool

HTML全文

参考文献(1)

[1]	1.l曾允孚、夏文杰主编，1986，沉积岩石学，北京:地质出版社。 2. Scholle , P. A.，Bebout, D. G.，and Moore, C. H.，1983, eds, Carbonate Depositional Environments, A. A. P. G.Memoir 33. 3.王英华主编，1991，中下扬子地区海相碳酸盐岩成岩作用研究，北京:科学技术出版社。 4.方少仙、黄继祥等，1989，中国南方泥盆、石炭纪岩相古地理及含油气性研究，《沉积相研究文集》编委会主编，《含油气盆地沉积相与油气分布》，北京:石油工业出版社。

[1]	王昕尧, 金振奎, 朱毅秀, 胡宗全, 刘光祥, 赵国伟, 李硕, 史书婷. 四川盆地自流井组陆相页岩石英成因研究 . 沉积学报, 2022, 40(4): 1010-1018. doi: 10.14027/j.issn.1000-0550.2021.053
[2]	芦飞凡, 谭秀成, 王利超, 唐青松, 肖笛, 董少峰, 苏成鹏, 潘政屹. 川中地区中二叠统栖霞组滩控岩溶型白云岩储层特征及主控因素 . 沉积学报, 2021, 39(2): 456-469. doi: 10.14027/j.issn.1000-0550.2020.020
[3]	孙海涛, 钟大康, 王威, 王爱, 杨烁, 杜红权, 唐自成, 周志恒. 四川盆地马路背地区上三叠统须家河组致密砂岩储层成因分析 . 沉积学报, 2021, 39(5): 1057-1067. doi: 10.14027/j.issn.1000-0550.2020.121
[4]	苏中堂, 佘伟, 罗静兰, 马国伟, 张帅. 鄂尔多斯盆地奥陶系马五₅亚段沉积微相与古地理演化 . 沉积学报, 2021, 39(6): 1344-1356. doi: 10.14027/j.issn.1000-0550.2020.101
[5]	徐文礼, 文华国, 刘均, 马智超, 孙权威, 蔡家兰, 陈守春, 韩建, 蒋欢, 荣浩然. 川东下三叠统嘉陵江组层序—岩相古地理特征 . 沉积学报, 2021, 39(6): 1478-1490. doi: 10.14027/j.issn.1000-0550.2021.105
[6]	黎霆, 李平平, 诸丹诚, 杨明磊, 李海平, 李涛, 邹华耀. 蜀南地区嘉陵江组颗粒滩储层发育机理 . 沉积学报, 2021, 39(2): 470-481. doi: 10.14027/j.issn.1000-0550.2020.015
[7]	金民东, 谭秀成, 李毕松, 朱祥, 曾伟, 连承波. 四川盆地震旦系灯影组白云岩成因 . 沉积学报, 2019, 37(3): 443-454. doi: 10.14027/j.issn.1000-0550.2018.148
[8]	宋世骏, 柳益群, 郑庆华, 周鼎武, 付瑜. 鄂尔多斯盆地三叠系延长组黑色岩系成因探讨——以铜川地区长7₃段为例 . 沉积学报, 2019, 37(6): 1117-1128. doi: 10.14027/j.issn.1000-0550.2019.053
[9]	任娜娜, 韩波, 张军涛, 冯菊芳, 王晓涛, 朱爽, 马强, 田海芹, 何治亮. 海水进退、滩坪出没、云化岩溶等与碳酸盐岩储层关系研究——以上扬子地台龙王庙组为例 . 沉积学报, 2018, 36(6): 1190-1205. doi: 10.14027/j.issn.1000-0550.2018.068
[10]	张顺存, 黄立良, 冯右伦, 邹阳, 鲁新川, 郭晖. 准噶尔盆地玛北地区三叠系百口泉组储层成岩相特征 . 沉积学报, 2018, 36(2): 354-365. doi: 10.14027/j.issn.1000-0550.2018.030
[11]	邹妞妞, 史基安, 张大权, 马崇尧, 张顺存, 鲁新川. 准噶尔盆地西北缘玛北地区百口泉组扇三角洲沉积模式 . 沉积学报, 2015, 33(3): 607-615. doi: 10.14027/j.cnki.cjxb.2015.03.019
[12]	. 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.
[13]	. 四川盆地东南部早三叠世地震事件沉积及其地质意义 . 沉积学报, 2012, 30(3): 477-489.
[14]	谭秀成. 陆表海碳酸盐岩台地沉积期微地貌恢复方法研究——以四川盆地磨溪气田嘉二2亚段A层为例 . 沉积学报, 2011, 29(3): 486-494.
[15]	胡明毅. 四川盆地嘉陵江组层序—岩相古地理特征和储层预测 . 沉积学报, 2010, 28(6): 1145-1152.
[16]	王一刚. 四川盆地三叠系飞仙关组气藏储层成岩作用研究拾零 . 沉积学报, 2007, 25(6): 831-839.
[17]	王琪, 禚喜准, 陈国俊, 史基安, 王多云. 鄂尔多斯盆地盐池—姬源地区三叠系长4+5砂岩成岩演化特征与优质储层分布 . 沉积学报, 2005, 23(3): 397-405.
[18]	杨家静, 王一刚, 王兰生, 文应初, 刘划一, 周国源. 四川盆地东部长兴组——飞仙关组气藏地球化学特征及气源探讨 . 沉积学报, 2002, 20(2): 349-353.
[19]	马永生, 李启明, 关德师. 鄂尔多斯盆地中部气田奥陶系马五_1－4碳酸盐岩微相特征与储层不均质性研究 . 沉积学报, 1996, 14(1): 22-32.
[20]	隗合明. 四川渠县三叠系膏盐的同生、成岩、后生及表生变化 . 沉积学报, 1987, 5(4): 56-65.

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: 378
HTML全文浏览量: 6
PDF下载量: 394
被引次数: 0

四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制

1 西南石油学院勘探系南充 637001;

2 四川石油川东开发公司重庆 630021

基金项目: 八五国家攻关项目

收稿日期: 1994-05-10
刊出日期: 1995-12-10

关键词:

四川盆地 /

三叠系 /

嘉陵江组 /

滩 /

微相 /

气藏

摘要: 四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育，受海平面相对升降的控制。提出了浅海滩和变浅暴露滩的新分类，分析了滩微相的古地理和层位分布规律，建立了滩的组成模型，总结了滩发育的三种相序模式。变浅暴露滩有有利的生、储和盖组合，发育的孔隙层段，早期形成的沉积－成岩圈闭，控制了各种圈闭中裂缝－孔隙型气藏的形成。上述思想提供了与滩有关的气藏勘探的新思路。

English Abstract

The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin

1 Department Exploration of South West Petroleum Insititute, Nanchong 637001;

2 Eastern Development Company of Sichuan Petroleum Bureau, Chongqing 630021

Received Date: 1994-05-10
Publish Date: 1995-12-10

Keywords:

Abstract: The 2-section of Jialingjang Group of Triassic in the eastern part of Sichuan Basin is an important gas bearing position. The Development of bank-micro factes have played an important pole in controlling the gas pool of fracture-pore type in traps.The banks are POint-bank on the platform in upper yangtze epicontinental sea. The new classificantion of shallow-sea bank and shallow exposed banks has been suggested on the basis of the evolution model of depositional environments which were controlled by relative sea-level changes. The similarities and difference of two types of banks have been compared. There were four bank development periods in the multicycle sedements of 2-section of Jialingjiang Group.The distribution of banks in two bank-development periods, for example, the 2-subsection of 2-section, have been mapped. The composition and devolopment model of point-bank at the Tishan anticline has been analysed. It clearly points out that the lithic factes in the core of bank have big thickness and good continuity in the multi-bank development periods. There are three types of factes sequences models:(1) the banks developed with sea-level up and disappeared with sea-level down; (2) the banks developed with sea-level down and disappeared to expose ; and (3) the banks developed with sea-level up and disappeared with sea-level up.Finally, the authors state how the shallow exposed bank control the formation of gas-pool. It has been recognind: ①the bank-microfacies complexs are beneficial for complexs of oil-producing, reservoir and seal formations, ②the shallow exposed bank is the microfacies zone of the pore-layers devolopment, ③ the sediment-diagenetic trap formed in bank-microfacies zone is beneficial for early accumulation of oil and gas pools @the development of pore-layers and accumulation of oil and gas in early sediment-diagenetic traps are the base of present gas -pool of fracture-pore type in various traps.

黄继祥, 曾伟, 张高信, 冉宏. 四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制[J]. 沉积学报, 1995, 13(S1): 109-117.

引用本文:

黄继祥, 曾伟, 张高信, 冉宏. 四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制[J]. 沉积学报, 1995, 13(S1): 109-117.

Citation:

Huang Jixiang, Zeng Wei, Zhang Gaoxing, Ran Hong. The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 109-117.

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

四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制

计量

The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin

计量

目录

四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制

1 西南石油学院勘探系南充 637001;

2 四川石油川东开发公司重庆 630021

English Abstract

The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin

1 Department Exploration of South West Petroleum Insititute, Nanchong 637001;

2 Eastern Development Company of Sichuan Petroleum Bureau, Chongqing 630021

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制

计量

出版历程

The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin

计量

出版历程

目录

四川盆地川东地区三叠系嘉陵江组第二段滩微相的发育分布及对气藏形成的控制

1 西南石油学院勘探系 南充 637001; 2 四川石油川东开发公司 重庆 630021

English Abstract

The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin

1 Department Exploration of South West Petroleum Insititute, Nanchong 637001; 2 Eastern Development Company of Sichuan Petroleum Bureau, Chongqing 630021

全文HTML

目录

友情链接

期刊在线

联系我们

1 西南石油学院勘探系南充 637001;

2 四川石油川东开发公司重庆 630021

1 Department Exploration of South West Petroleum Insititute, Nanchong 637001;

2 Eastern Development Company of Sichuan Petroleum Bureau, Chongqing 630021