东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨

陈发亮; 朱晖; 李绪涛; 苗翠芝

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

东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨

陈发亮, 朱晖, 李绪涛, 苗翠芝

文章导航 > 沉积学报 > 2000 > 18(3): 384-388,394

陈发亮, 朱晖, 李绪涛, 苗翠芝. 东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨[J]. 沉积学报, 2000, 18(3): 384-388,394.

引用本文:

陈发亮, 朱晖, 李绪涛, 苗翠芝. 东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨[J]. 沉积学报, 2000, 18(3): 384-388,394.

CHEN Fa liang, ZHU Hui, LI Xu tao, MIAO Cui zhi. Partition of Sequence Strata and Discussion aboutSalt- rock Resource in Shahejie Formation of Eogene, Dongpu Depression[J]. Acta Sedimentologica Sinica, 2000, 18(3): 384-388,394.

Citation:

CHEN Fa liang, ZHU Hui, LI Xu tao, MIAO Cui zhi. Partition of Sequence Strata and Discussion aboutSalt- rock Resource in Shahejie Formation of Eogene, Dongpu Depression[J]. Acta Sedimentologica Sinica, 2000, 18(3): 384-388,394.

陈发亮, 朱晖, 李绪涛, 苗翠芝. 东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨[J]. 沉积学报, 2000, 18(3): 384-388,394.

引用本文:

陈发亮, 朱晖, 李绪涛, 苗翠芝. 东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨[J]. 沉积学报, 2000, 18(3): 384-388,394.

Citation:

东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨

1 中原油田地质调查处河南濮阳 457001;
2 中原油田勘探开发科学研究院河南濮阳 457001

详细信息

作者简介:
陈发亮,男,1973年生,工程师,石油地质

中图分类号: P539.2,P588

计量

文章访问数: 896
HTML全文浏览量: 48
PDF下载量: 495
被引次数: 0

Partition of Sequence Strata and Discussion aboutSalt- rock Resource in Shahejie Formation of Eogene, Dongpu Depression

1 Survey Institute of Geology, Zhongyuan Petroleum Exploration Bureau, Puyang Henan 457001;
2 Institute of Exploration and Development Zhongyuan Oilfield,Puyang Henan 457001

摘要

摘要: 应用层序地层学理论,通过对地质、地化、古生物、钻井和测井资料进行综合分析,再现了东濮凹陷下第三系沙河街组地层沉积岩相古地理,并再次探讨了该地区分布广泛、厚度巨大的盐膏地层的成因及盐的来源问题,认为东濮凹陷大量的盐膏层属于一种潮湿气候条件下受深大断裂控制的深水成盐模式,这种模式由于大量盐膏层与生油岩同期形成并与大量沉积砂体相匹配故极有利于形成生储盖配置良好的岩性地层油气藏。
- 层序地层 /
- 体系域 /
- 盐膏成因 /
- 下第三系 /
- 东濮凹陷
Abstract: Dongpu depression is located in the southwest of Bohai Bay basin. The area is about 5300 square kilometers. The south is wide and the north is narrow. Lanliao fault controls its development and evolvement. On the basis of sequence stratigraphic theory, the author analyzed of the geologic, seimic, geochemical, paleobiological, drilling and logging data. There are two sequences (Sequence I and Sequence II) and eight systems tracts(one sequence includes LST, TST, HST and FSST) has been identified in Shahejie and Dongying formation. They are all have clear characteristics in seimic, geologic, core and logging dada. In continental basin, the influence of the three factors of tectonization, weather and sediments on sequence is different from that in marine basin, the weather is more important than that in marine sequence. After the synthetical analysis of sedimentary facies markers, the author has made the sedimentary lithofacies paleogeographic reconstruction of Shahejie formation of Eogene in Dongpu depression. In this paper the author also re-discussed the resource and the formation of salt-rock, which distributed widely and has a large thickness. The characteristics of chemical components, paleobiota, lithology and distribution of the salt-rock are different from the normal evaporite. It is not come from the evaporation of sea water. Combined the paleotectogenesis and the paleoclimate, the result of the study indicates that the salt-rock is originate from the hot bittern in deep earth and formed under a deep-water environment with a moist climate in Dongpu depression. The formed model is due to an event abruptly. Development of salt-rock is related to tectonization of Lanliao fault but not the climate. The salt-rock is located in TST or HST and developed with source rock. It is advantageous to source rock by preventing it from oxygen. It can also provide heat and pressure for source rock to change into oil or gas. The salt-rock is tighter than mudstone as seal-rock. Because of so many salt-rock formed with source rock and sand body, It is more propitious to form litho-reservoir which has a good matching relationship among source、reservoir and seal rock.
- sequence strata /
- systems tract /
- salt-rock resource /
- Eogene /
- Dongpu depression

HTML全文

参考文献(4)

[1]	陆荣生,赵春元,陈树文等.中国石油地质志(卷7,中原油田)[M] .北京：石油工业出版社,1993.35～43
[2]	姜在兴,李华启编著.层序地层学原理及应用[M] .北京：石油工业出版社,1996.57～68
[3]	C.K.威尔格斯[美] 等编.徐怀大等译,层序地层学原理一海平面变化综合分析[C] .北京：石油工业出版社,1993 49～54
[4]	Dag Nummedal, Principles and Applications of Siliciclastic SequenceStratigraphy Beijing China[R] . 1993.35～42

[1]	赖锦, 王贵文, 柴毓, 冉冶, 郑新华, 信毅, 周磊, 吴庆宽. 库车坳陷白垩系巴什基奇克组成岩层序地层特征 . 沉积学报, 2015, 33(2): 394-407. doi: 10.14027/j.cnki.cjxb.2015.02.019
[2]	吴贤涛, 张国成. 东濮凹陷古近系沙河街组边缘海—浅海相识别与油气储层 . 沉积学报, 2015, 33(2): 364-375. doi: 10.14027/j.cnki.cjxb.2015.02.016
[3]	. 渤海湾盆地东濮凹陷膏盐岩与油气的关系 . 沉积学报, 2014, 32(1): 126-137.
[4]	. 东濮凹陷古近系沙河街组三段河口湾沉积亚相之沉积学与痕迹学识别与油气储层 . 沉积学报, 2014, 32(4): 744-753.
[5]	冯有良. 辽河西部凹陷古近系层序地层与地层岩性油气藏预测 . 沉积学报, 2009, 27(1): 57-63.
[6]	管红. 南堡凹陷东营组层序地层格架与沉积体系 . 沉积学报, 2008, 26(5): 730-736.
[7]	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.
[8]	陈明, 许效松, 万方, 楼雄鹰, 汪正江, 傅恒. 塔里木盆地柯坪地区中下奥陶统碳酸盐岩露头层序地层学研究 . 沉积学报, 2004, 22(1): 110-116.
[9]	罗小平, 沈忠民, 彭渤莹, 王又杰, 林壬子. 东濮凹陷白庙地区天然气及凝析油地球化学特征及成因 . 沉积学报, 2004, 22(S1): 50-55.
[10]	张喜林, 朱筱敏, 钟大康, 梁兵, 曹冰, 贺向阳. 苏北盆地高邮凹陷第三系—上白垩统层序地层格架特征 . 沉积学报, 2004, 22(3): 393-399.
[11]	张德武, 冯有良, 邱以钢, 闵伟, 郭玉新, 赵乐强, 向立宏. 东营凹陷下第三系层序地层研究与隐蔽油气藏预测 . 沉积学报, 2004, 22(1): 67-72.
[12]	尹太举, 张昌民, 李中超, 毛立华, 尹艳树, 邓宏文. 濮城油田沙三中6-10砂组高分辨率层序地层研究 . 沉积学报, 2003, 21(4): 663-669.
[13]	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.
[14]	赵全民, 杨道庆, 江继刚, 彭江, 徐士忠. 舞阳、襄城凹陷下第三系盐湖相有机地球化学与沉积环境研究 . 沉积学报, 2003, 21(2): 334-339.
[15]	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.
[16]	国景星, 戴启德, 徐炜. 沾化凹陷东部长堤地区下第三系沉积体系研究 . 沉积学报, 2001, 19(3): 368-374.
[17]	张枝焕, 胡文瑄, 曾溅辉, 于炳松, 陆现彩, 贾红育. 东营凹陷下第三系流体—岩石相互作用研究 . 沉积学报, 2000, 18(4): 560-566.
[18]	吴智勇, 郭建华, 吴东胜, 何宏. 东濮断陷湖盆下第三系沙二段的冲积扇沉积 . 沉积学报, 1999, 17(3): 449-453.
[19]	傅强. 成岩作用对储层孔隙的影响——以辽河盆地荣37块气田下第三系为例 . 沉积学报, 1998, 16(3): 92-96.
[20]	胡受权. 泌阳断陷双河—赵凹地区下第三系核三上段陆相层序发育的可容空间机制 . 沉积学报, 1998, 16(3): 102-108.

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: 896
HTML全文浏览量: 48
PDF下载量: 495
被引次数: 0

东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨

1 中原油田地质调查处河南濮阳 457001;

2 中原油田勘探开发科学研究院河南濮阳 457001

作者简介:
陈发亮,男,1973年生,工程师,石油地质

收稿日期: 1999-01-17
修回日期: 2000-04-05
刊出日期: 2000-09-10

中图分类号: P539.2,P588

关键词:

体系域 /

摘要: 应用层序地层学理论,通过对地质、地化、古生物、钻井和测井资料进行综合分析,再现了东濮凹陷下第三系沙河街组地层沉积岩相古地理,并再次探讨了该地区分布广泛、厚度巨大的盐膏地层的成因及盐的来源问题,认为东濮凹陷大量的盐膏层属于一种潮湿气候条件下受深大断裂控制的深水成盐模式,这种模式由于大量盐膏层与生油岩同期形成并与大量沉积砂体相匹配故极有利于形成生储盖配置良好的岩性地层油气藏。

English Abstract

Partition of Sequence Strata and Discussion aboutSalt- rock Resource in Shahejie Formation of Eogene, Dongpu Depression

1 Survey Institute of Geology, Zhongyuan Petroleum Exploration Bureau, Puyang Henan 457001;

2 Institute of Exploration and Development Zhongyuan Oilfield,Puyang Henan 457001

Received Date: 1999-01-17
Rev Recd Date: 2000-04-05
Publish Date: 2000-09-10

Keywords:

Abstract: Dongpu depression is located in the southwest of Bohai Bay basin. The area is about 5300 square kilometers. The south is wide and the north is narrow. Lanliao fault controls its development and evolvement. On the basis of sequence stratigraphic theory, the author analyzed of the geologic, seimic, geochemical, paleobiological, drilling and logging data. There are two sequences (Sequence I and Sequence II) and eight systems tracts(one sequence includes LST, TST, HST and FSST) has been identified in Shahejie and Dongying formation. They are all have clear characteristics in seimic, geologic, core and logging dada. In continental basin, the influence of the three factors of tectonization, weather and sediments on sequence is different from that in marine basin, the weather is more important than that in marine sequence. After the synthetical analysis of sedimentary facies markers, the author has made the sedimentary lithofacies paleogeographic reconstruction of Shahejie formation of Eogene in Dongpu depression. In this paper the author also re-discussed the resource and the formation of salt-rock, which distributed widely and has a large thickness. The characteristics of chemical components, paleobiota, lithology and distribution of the salt-rock are different from the normal evaporite. It is not come from the evaporation of sea water. Combined the paleotectogenesis and the paleoclimate, the result of the study indicates that the salt-rock is originate from the hot bittern in deep earth and formed under a deep-water environment with a moist climate in Dongpu depression. The formed model is due to an event abruptly. Development of salt-rock is related to tectonization of Lanliao fault but not the climate. The salt-rock is located in TST or HST and developed with source rock. It is advantageous to source rock by preventing it from oxygen. It can also provide heat and pressure for source rock to change into oil or gas. The salt-rock is tighter than mudstone as seal-rock. Because of so many salt-rock formed with source rock and sand body, It is more propitious to form litho-reservoir which has a good matching relationship among source、reservoir and seal rock.

陈发亮, 朱晖, 李绪涛, 苗翠芝. 东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨[J]. 沉积学报, 2000, 18(3): 384-388,394.

引用本文:

陈发亮, 朱晖, 李绪涛, 苗翠芝. 东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨[J]. 沉积学报, 2000, 18(3): 384-388,394.

Citation:

全文HTML

参考文献 (4)

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

留言板

东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨

作者简介:
陈发亮,男,1973年生,工程师,石油地质

计量

Partition of Sequence Strata and Discussion aboutSalt- rock Resource in Shahejie Formation of Eogene, Dongpu Depression

计量

目录

东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨

1 中原油田地质调查处河南濮阳 457001;

2 中原油田勘探开发科学研究院河南濮阳 457001

作者简介:
陈发亮,男,1973年生,工程师,石油地质

English Abstract

Partition of Sequence Strata and Discussion aboutSalt- rock Resource in Shahejie Formation of Eogene, Dongpu Depression

1 Survey Institute of Geology, Zhongyuan Petroleum Exploration Bureau, Puyang Henan 457001;

2 Institute of Exploration and Development Zhongyuan Oilfield,Puyang Henan 457001

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨

作者简介: 陈发亮,男,1973年生,工程师,石油地质

计量

出版历程

Partition of Sequence Strata and Discussion aboutSalt- rock Resource in Shahejie Formation of Eogene, Dongpu Depression

计量

出版历程

目录

东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨

1 中原油田地质调查处 河南濮阳 457001; 2 中原油田勘探开发科学研究院 河南濮阳 457001

作者简介: 陈发亮,男,1973年生,工程师,石油地质

English Abstract

Partition of Sequence Strata and Discussion aboutSalt- rock Resource in Shahejie Formation of Eogene, Dongpu Depression

1 Survey Institute of Geology, Zhongyuan Petroleum Exploration Bureau, Puyang Henan 457001; 2 Institute of Exploration and Development Zhongyuan Oilfield,Puyang Henan 457001

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
陈发亮,男,1973年生,工程师,石油地质

1 中原油田地质调查处河南濮阳 457001;

2 中原油田勘探开发科学研究院河南濮阳 457001

作者简介:
陈发亮,男,1973年生,工程师,石油地质

1 Survey Institute of Geology, Zhongyuan Petroleum Exploration Bureau, Puyang Henan 457001;

2 Institute of Exploration and Development Zhongyuan Oilfield,Puyang Henan 457001