珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系

宋爽; 朱筱敏; 于福生; 葛家旺; 史亚会; 贺敬聪; 袁立忠; 刘军

doi:10.14027/j.cnki.cjxb.2016.02.002

ISSN 1000-0550 CN 62-1038/P

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珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系

宋爽, 朱筱敏, 于福生, 葛家旺, 史亚会, 贺敬聪, 袁立忠, 刘军

文章导航 > 沉积学报 > 2016 > 34(2): 222-235

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[J]. 沉积学报, 2016, 34(2): 222-235. doi: 10.14027/j.cnki.cjxb.2016.02.002

引用本文:

SONG Shuang, ZHU XiaoMin, YU FuSheng, GE JiaWang, SHI YaHui, HE JingCong, YUAN LiZhong, LIU Jun. Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2016, 34(2): 222-235. doi: 10.14027/j.cnki.cjxb.2016.02.002

Citation:

SONG Shuang, ZHU XiaoMin, YU FuSheng, GE JiaWang, SHI YaHui, HE JingCong, YUAN LiZhong, LIU Jun. Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2016, 34(2): 222-235. doi: 10.14027/j.cnki.cjxb.2016.02.002

引用本文:

Citation:

SONG Shuang, ZHU XiaoMin, YU FuSheng, GE JiaWang, SHI YaHui, HE JingCong, YUAN LiZhong, LIU Jun. Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2016, 34(2): 222-235. doi: 10.14027/j.cnki.cjxb.2016.02.002

珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系

doi: 10.14027/j.cnki.cjxb.2016.02.002

宋爽^1,2,
朱筱敏^1,2,,
于福生^1,2,
葛家旺²,
史亚会²,
贺敬聪²,
袁立忠³,
刘军³

1.
中国石油大学(北京)油气与资源探测国家重点实验室北京 102249;
2.
中国石油大学(北京)地球科学学院北京 102249;
3.
中海石油(中国)深圳分公司广州 510240

基金项目: 国家油气重大专项课题(2011ZX05025-005,2011ZX05001-002);国家自然科学基金项目(41272133)

详细信息

作者简介:
宋爽女 1990年出生硕士研究生层序地层学及岩相古地理 E-mail:1023songshuang@163.com

通讯作者:
朱筱敏男教授 E-mail:xmzhu@cup.edu.cn

中图分类号: P512.2;P542

计量

文章访问数: 530
HTML全文浏览量: 7
PDF下载量: 798
被引次数: 0

Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin

1.
College of Geosciences, China University of Petroleum, Beijing 102249, China;
2.
State Key Laboratory of Petroleum Resource and Prospecting(China University of Petroleum), Beijing 102249, China;
3.
Shengzhen Institute of CNOOC Limited, Guangzhou, China 510240

Funds: National Major Projects of Oil and Gas, No.2011ZX05025-005, 2011ZX05001-002;National Natural Science Foundation of China, No.41272133

摘要

摘要: 长昌-鹤山凹陷为珠江口盆地珠四坳陷NE-SW走向的凹陷,是珠江口盆地继白云、荔湾深水区油气突破之后的又一个深水战略性勘探区块,目前无钻井,属于勘探新区,因此基础地质研究尤为重要。通过断层解释和地层厚度分析,认为文昌组和恩平组分别对应早期强裂陷阶段和晚期弱裂陷阶段,并识别多种不同级别和类型的构造变换带。以经典层序地层学理论为指导,通过对全区二维地震资料追踪闭合,将长昌-鹤山凹陷文昌组-恩平组划分为2个二级层序和7个三级层序。在三级层序格架内,根据地震相特征结合经典的地震相-沉积相转换关系,重建了研究区沉积充填演化过程。通过平面断层组合分析认为,研究区发育两个级别(Ⅰ级和Ⅱ级)、六种类型(同向未叠覆型、同向叠覆型、同向平行型、同向共线型、对向叠覆型和背向叠覆型)构造变换带。断陷活动的强弱控制着层序和沉积体系的发育,构造变换带、坡折带类型控制着砂体的分布与规模。针对研究区是深水勘探新区,可通过该思路从构造与沉积耦合度高的区域进行有利区带的预测,为低勘探程度深水研究区的油气勘探提供了科学依据。
- 层序地层格架 /
- 沉积体系 /
- 构造变换带 /
- 长昌&mdash /
- 鹤山凹陷 /
- 珠江口盆地
Abstract: Changchang-Heshan depression, located in southwest Zhu-IV subbasin of Pearl River Mouth Basin, extends in NE-SW direction. It is an important strategic exploration block after oil and gas exploration breakthrough in Baiyun and Liwan depression in deep water area. Changchang-Heshan depression is a new area to oil and gas exploration and has no wells, so the basic geological research is particularly important. Based on fault interpretation and formation thickness analysis, rift stages and structural characteristics were studied in detail. Wenchang and Enping Formation experienced two successive tectonic stages, which respectively corresponded to intensive rift stage and weak rift stage. A variety of different levels and types of structural transfer zones were identified at the same time. Guided by the theory of classic sequence stratigraphy, Wenchang and Enping Formation were divided into two second-order sequences and seven third-order sequences based on the two-dimensional seismic data. According to the characteristics of the seismic reflection, transfer the classic seismic facies to sedimentary facies within the sequence framework, and then rebuilt the process of sedimentary system evolution in the study area. Classified two levels(Ⅰ and Ⅱ) and six types of structural transfer zones(syntropy non-overlapping, syntropy non-overlapping, syntropy parallel, syntropy collineation, opposite overlapping and back to back overlapping). The degree of the fault activity controlled the sequence evolution and sedimentation system. Furthermore, structural transfer zone and slope break controlled the distribution and scale of sand bodies. The study area is a new region for oil and gas exploration, this method is focused on the close relation between tectonism and sedimentation. Finally, it offers reliable evidence for favourable region exploration and supports a solid scientific evidence for the low degree oil and gas exploration in deep water area.
- sequence stratigraphic framework /
- sedimentary system /
- transfer zone /
- Changchang-Heshan depression /
- Pearl River Mouth Basin /

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[1]	梁杰, 刘杰, 牛胜利, 林秋金, 朱君雪, 刘徐敏. 珠江口盆地惠州25转换带文昌组五段早期低位体系域源—渠—汇耦合关系及勘探潜力探讨 . 沉积学报, 2022, 40(6): 1451-1460. doi: 10.14027/j.issn.1000-0550.2022.016
[2]	舒梁锋, 张向涛, 张忠涛, 张丽丽, 雷胜兰, 高中亮, 韩霄, 于飒. 珠江口盆地白云南洼珠海组陆架边缘三角洲沉积体系演化 . 沉积学报, 2022, 40(3): 825-837. doi: 10.14027/j.issn.1000-0550.2021.146
[3]	刘杰, 苏明, 乔少华, 沙志彬, 吴能友, 杨睿. 珠江口盆地白云凹陷陆坡限制型海底峡谷群成因机制探讨 . 沉积学报, 2016, 34(5): 940-950. doi: 10.14027/j.cnki.cjxb.2016.05.013
[4]	王永凤, 李冬, 王英民, 徐强. 珠江口盆地重要不整合界面与珠江沉积体系演化分析 . 沉积学报, 2015, 33(3): 587-594. doi: 10.14027/j.cnki.cjxb.2015.03.017
[5]	吴其林, 但志伟, 肖为, 曾驿, 周小康, 侯志平. 珠江口盆地H区块碳酸盐岩储层地震沉积学应用研究 . 沉积学报, 2015, 33(4): 828-835. doi: 10.14027/j.cnki.cjxb.2015.04.021
[6]	刘畅, 张琴, 谢寅符, 乔李井宇, 孙杰夫, 梅啸寒. 厄瓜多尔Oriente盆地东北部区块白垩系层序地层格架及发育模式 . 沉积学报, 2014, 32(6): 1123-1131.
[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]	李成海, 王家豪, 柳保军, 苏奥, 徐东浩, 罗泉源, 刘姗, 牟川. 珠江口盆地白云凹陷古近系沉积相类型 . 沉积学报, 2014, 32(6): 1162-1170.
[9]	. 珠江口盆地番禺天然气区东南缘坡折带韩江组中段沉积层序与岩性地层圈闭研究 . 沉积学报, 2013, 31(6): 1081-1087.
[10]	李云. 珠江口盆地荔湾31气田珠江组深水扇沉积相分析 . 沉积学报, 2011, 29(4): 665-676.
[11]	付兆辉. 渤海湾盆地埕北凹陷古近系沉积体系分析与油气成藏 . 沉积学报, 2009, 27(1): 26-31.
[12]	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.
[13]	邵磊. 珠江口盆地的沉积充填与珠江的形成演变 . 沉积学报, 2008, 26(2): 179-158.
[14]	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.
[15]	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.
[16]	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.
[17]	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.
[18]	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.
[19]	屈红军, 李文厚, 苗建宇, 张小莉, 庞军刚. 东濮凹陷濮卫环洼带沙三段沉积体系及储层发育规律 . 沉积学报, 2003, 21(4): 601-606.
[20]	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.

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珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系

doi: 10.14027/j.cnki.cjxb.2016.02.002

1. 中国石油大学(北京)油气与资源探测国家重点实验室北京 102249;

2. 中国石油大学(北京)地球科学学院北京 102249;

3. 中海石油(中国)深圳分公司广州 510240

基金项目: 国家油气重大专项课题(2011ZX05025-005,2011ZX05001-002);国家自然科学基金项目(41272133)

作者简介:
宋爽女 1990年出生硕士研究生层序地层学及岩相古地理 E-mail:1023songshuang@163.com

通讯作者: 朱筱敏男教授 E-mail:xmzhu@cup.edu.cn

收稿日期: 2015-04-21
修回日期: 2015-06-12
刊出日期: 2016-04-10

中图分类号: P512.2;P542

关键词:

长昌— /

摘要: 长昌-鹤山凹陷为珠江口盆地珠四坳陷NE-SW走向的凹陷,是珠江口盆地继白云、荔湾深水区油气突破之后的又一个深水战略性勘探区块,目前无钻井,属于勘探新区,因此基础地质研究尤为重要。通过断层解释和地层厚度分析,认为文昌组和恩平组分别对应早期强裂陷阶段和晚期弱裂陷阶段,并识别多种不同级别和类型的构造变换带。以经典层序地层学理论为指导,通过对全区二维地震资料追踪闭合,将长昌-鹤山凹陷文昌组-恩平组划分为2个二级层序和7个三级层序。在三级层序格架内,根据地震相特征结合经典的地震相-沉积相转换关系,重建了研究区沉积充填演化过程。通过平面断层组合分析认为,研究区发育两个级别(Ⅰ级和Ⅱ级)、六种类型(同向未叠覆型、同向叠覆型、同向平行型、同向共线型、对向叠覆型和背向叠覆型)构造变换带。断陷活动的强弱控制着层序和沉积体系的发育,构造变换带、坡折带类型控制着砂体的分布与规模。针对研究区是深水勘探新区,可通过该思路从构造与沉积耦合度高的区域进行有利区带的预测,为低勘探程度深水研究区的油气勘探提供了科学依据。

English Abstract

Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin

1. College of Geosciences, China University of Petroleum, Beijing 102249, China;

2. State Key Laboratory of Petroleum Resource and Prospecting(China University of Petroleum), Beijing 102249, China;

3. Shengzhen Institute of CNOOC Limited, Guangzhou, China 510240

Funds: National Major Projects of Oil and Gas, No.2011ZX05025-005, 2011ZX05001-002;National Natural Science Foundation of China, No.41272133

Received Date: 2015-04-21
Rev Recd Date: 2015-06-12
Publish Date: 2016-04-10

Keywords:

Abstract: Changchang-Heshan depression, located in southwest Zhu-IV subbasin of Pearl River Mouth Basin, extends in NE-SW direction. It is an important strategic exploration block after oil and gas exploration breakthrough in Baiyun and Liwan depression in deep water area. Changchang-Heshan depression is a new area to oil and gas exploration and has no wells, so the basic geological research is particularly important. Based on fault interpretation and formation thickness analysis, rift stages and structural characteristics were studied in detail. Wenchang and Enping Formation experienced two successive tectonic stages, which respectively corresponded to intensive rift stage and weak rift stage. A variety of different levels and types of structural transfer zones were identified at the same time. Guided by the theory of classic sequence stratigraphy, Wenchang and Enping Formation were divided into two second-order sequences and seven third-order sequences based on the two-dimensional seismic data. According to the characteristics of the seismic reflection, transfer the classic seismic facies to sedimentary facies within the sequence framework, and then rebuilt the process of sedimentary system evolution in the study area. Classified two levels(Ⅰ and Ⅱ) and six types of structural transfer zones(syntropy non-overlapping, syntropy non-overlapping, syntropy parallel, syntropy collineation, opposite overlapping and back to back overlapping). The degree of the fault activity controlled the sequence evolution and sedimentation system. Furthermore, structural transfer zone and slope break controlled the distribution and scale of sand bodies. The study area is a new region for oil and gas exploration, this method is focused on the close relation between tectonism and sedimentation. Finally, it offers reliable evidence for favourable region exploration and supports a solid scientific evidence for the low degree oil and gas exploration in deep water area.

引用本文:

Citation:

SONG Shuang, ZHU XiaoMin, YU FuSheng, GE JiaWang, SHI YaHui, HE JingCong, YUAN LiZhong, LIU Jun. Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2016, 34(2): 222-235. doi: 10.14027/j.cnki.cjxb.2016.02.002

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珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系

doi: 10.14027/j.cnki.cjxb.2016.02.002

作者简介:
宋爽女 1990年出生硕士研究生层序地层学及岩相古地理 E-mail:1023songshuang@163.com

通讯作者:
朱筱敏男教授 E-mail:xmzhu@cup.edu.cn

计量

Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin

计量

目录

珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系

doi: 10.14027/j.cnki.cjxb.2016.02.002

1. 中国石油大学(北京)油气与资源探测国家重点实验室北京 102249;

2. 中国石油大学(北京)地球科学学院北京 102249;

3. 中海石油(中国)深圳分公司广州 510240

作者简介:
宋爽女 1990年出生硕士研究生层序地层学及岩相古地理 E-mail:1023songshuang@163.com

通讯作者: 朱筱敏男教授 E-mail:xmzhu@cup.edu.cn

English Abstract

Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin

1. College of Geosciences, China University of Petroleum, Beijing 102249, China;

2. State Key Laboratory of Petroleum Resource and Prospecting(China University of Petroleum), Beijing 102249, China;

3. Shengzhen Institute of CNOOC Limited, Guangzhou, China 510240

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珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系

doi: 10.14027/j.cnki.cjxb.2016.02.002

作者简介: 宋爽 女 1990年出生 硕士研究生 层序地层学及岩相古地理 E-mail:1023songshuang@163.com

通讯作者: 朱筱敏 男 教授 E-mail:xmzhu@cup.edu.cn

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出版历程

Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin

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出版历程

目录

珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系

doi: 10.14027/j.cnki.cjxb.2016.02.002

1. 中国石油大学(北京)油气与资源探测国家重点实验室 北京 102249; 2. 中国石油大学(北京)地球科学学院 北京 102249; 3. 中海石油(中国)深圳分公司 广州 510240

作者简介: 宋爽 女 1990年出生 硕士研究生 层序地层学及岩相古地理 E-mail:1023songshuang@163.com

通讯作者: 朱筱敏 男 教授 E-mail:xmzhu@cup.edu.cn

English Abstract

Sedimentary System Evolution and its Response to Tectonic Movement in Changchang-Heshan Depression, Deep Water Area of Pearl River Mouth Basin

1. College of Geosciences, China University of Petroleum, Beijing 102249, China; 2. State Key Laboratory of Petroleum Resource and Prospecting(China University of Petroleum), Beijing 102249, China; 3. Shengzhen Institute of CNOOC Limited, Guangzhou, China 510240

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联系我们

作者简介:
宋爽女 1990年出生硕士研究生层序地层学及岩相古地理 E-mail:1023songshuang@163.com

通讯作者:
朱筱敏男教授 E-mail:xmzhu@cup.edu.cn

1. 中国石油大学(北京)油气与资源探测国家重点实验室北京 102249;

2. 中国石油大学(北京)地球科学学院北京 102249;

3. 中海石油(中国)深圳分公司广州 510240

作者简介:
宋爽女 1990年出生硕士研究生层序地层学及岩相古地理 E-mail:1023songshuang@163.com

通讯作者: 朱筱敏男教授 E-mail:xmzhu@cup.edu.cn

1. College of Geosciences, China University of Petroleum, Beijing 102249, China;

2. State Key Laboratory of Petroleum Resource and Prospecting(China University of Petroleum), Beijing 102249, China;

3. Shengzhen Institute of CNOOC Limited, Guangzhou, China 510240