珠江口盆地21Ma和13.8Ma陆架边缘三角洲对比

doi:10.11743/ogg20140512

石油与天然气地质 ›› 2014, Vol. 35 ›› Issue (5): 670-678.doi: 10.11743/ogg20140512

珠江口盆地21Ma和13.8Ma陆架边缘三角洲对比

易雪斐¹, 张昌民², 李少华², 杜家元^2,3, 罗明³, 李向阳⁴

1. 非常规油气湖北省协同创新中心, 湖北武汉 430100;
2. 长江大学油气资源与勘探技术教育部重点实验室, 湖北武汉 430100;
3. 中海石油(中国)有限公司深圳分公司, 广东广州 510240;
4. 河南省核工业地质局, 河南信阳 464000

收稿日期:2013-09-28 修回日期:2014-08-18 出版日期:2014-10-08 发布日期:2014-10-17
通讯作者: 张昌民（1963- ），男，博士生导师，沉积学和开发地质。
第一作者简介:易雪斐（1986- ），女，博士，沉积学和层序地层学。E-mail：xuefeiyi1986@163.com。
基金项目:
国家“十二五”重大专项（2011ZX05023-002）。

Comparison between shelf-margin delta of 21 Ma and 13.8 Ma in Pearl River Mouth Basin

Yi Xuefei¹, Zhang Changmin², Li Shaohua², Du Jiayuan^2,3, Luo Ming³, Li Xiangyang⁴

1. Hubei Cooperative Innovation Center of Unconventional Oil and Gas, Wuhan, Hubei 430100, China;
2. Key Laboratory of Oil and Gas Resources and Exploration, Yangtze University, Wuhan, Hubei 430100, China;
3. Shenzhen Branch of CNOOC Ltd., Guangzhou, Guangdong 510240, China;
4. Nuclear Industry Geological Survey of Henan Province, Xinyang, Henan 464000, China

Received:2013-09-28 Revised:2014-08-18 Online:2014-10-08 Published:2014-10-17

摘要/Abstract

摘要：

陆架边缘三角洲是三角洲动态分类中一种比较重要的三角洲类型，已经成为科学研究和勘探开发的热点。根据驱动因素，可将陆架边缘三角洲分为物源供给驱动型和可容纳空间驱动型两类。珠江口盆地距今21 Ma和13.8 Ma时期具备发育陆架边缘三角洲的地质条件。通过对录井、测井曲线和地震资料的综合分析，从地形、相对海平面变化和沉积物供给三方面对21 Ma和13.8 Ma进行对比，对陆架边缘三角洲形成条件进行了分析，认为21 Ma时期为物源供给驱动型，而13.8 Ma时期为可容纳空间驱动型。虽然层序SQ2和SQ9在地形、相对海平面变化和沉积物供给三方面都存在较大差异，但它们都为典型的Ⅰ型层序，发育低位扇体、陆架边缘三角洲和三角洲前缘的滑塌体，均为稳定的陆架边缘三角洲。

关键词: 物源供给驱动型, 可容纳空间驱动型, 坡折, 陆架边缘三角洲, 珠江口盆地

Abstract:

Shelf-margin delta,an important type in the dynamic classification of delta,has become the focus of science researches and hot spot in oil & gas exploration.According to the driving factors,shelf-margin delta can be categorized into two types,namely sediment supply-driving delta and accommodation-driving delta.The Pearl River Mouth Basin had favorable geological condition for shelf-margin delta development at 21 Ma and 13.8 Ma.Shelf-margin deltas(21 Ma and 13.8 Ma)are analyzed in respects of topography,relative sea-level change and sediment supply through integration of well logging,logging curves and seismic data.The forming condition analysis shows that the delta at 21 Ma is of sediment supply-dri-ving type,while the delta at 13.8 Ma is of accommodation-driving type.Although SQ2 and SQ9 are obviously different in respects of topography,relative sea-level change and sediment supply,they both are type I sequences,and have well-developed lowstand fans,shelf-margin delta and delta-front slumping deposits,which belonging to stable shelf-margin deltas.

Key words: sediment supply-driving type, accommodation-driving type, slope break, shelf-margin delta, Pearl River Mouth Basin

中图分类号:

TE121.3

易雪斐,张昌民,李少华,等. 珠江口盆地21Ma和13.8Ma陆架边缘三角洲对比[J]. 石油与天然气地质, 2014, 35(5): 670-678. doi: 10.11743/ogg20140512 Yi Xuefei,Zhang Changmin,Li Shaohua,et al. Comparison between shelf-margin delta of 21 Ma and 13.8 Ma in Pearl River Mouth Basin[J]. Oil & Gas Geology, 2014, 35(5): 670-678. doi: 10.11743/ogg20140512

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珠江口盆地21Ma和13.8Ma陆架边缘三角洲对比

Comparison between shelf-margin delta of 21 Ma and 13.8 Ma in Pearl River Mouth Basin

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