GIEC OpenIR  > 中国科学院广州能源研究所
珠江口盆地白云凹陷北坡上新世一第四纪陆架边缘沉积体系特征
Alternative TitlePLIOCENE-QUATERNARY SHELF-EDGE DEPOSITIONAL SYSTEMS ON THE NORTHERN SLOPE OF BAIYUN SAG, THE PEARL RIVER MOUTH BASIN
孙美静1; 彭学超1; 聂鑫1; 刘杰2
2015
Source Publication海洋地质前沿
Issue8Pages:41-46
AbstractBased on the high resolution multi-channel seismic data, drilling cores and well logs data, the Pliocene-Quaternary isochronous stratigraphic framework is established for the northern slope of the Baiyun Sag. Typical depositional systems are recognized on
Other Abstract运用珠江口盆地新采集的高分辨率多道地震资料,结合前人在本区的钻井、岩心、测井曲线及地震的综合资料,建立了白云凹陷北坡上新世一第四纪的等时地层格架,在此基础上分析了陆架边缘典型沉积体系,并初步探讨了其控制因素。研究表明,上新世一第四纪地层内识别出T0(海底)、T1(1.8Ma)和T2(5.3Ma)3个三级层序界面,划分出A、B2个三级层序。研究区地震相主要有席状平行一亚平行地震相、帚状前积地震相、透镜状前积地震相、谷状充填地震相,不同的地震相及其组合代表特定的沉积体系。地震相特征分析表明,研究区上新世一第四
Keyword珠江口盆地 白云凹陷 上新世一第四纪 陆架边缘 沉积体系
Funding Organization中国地质调查局项目(1212011220115);中国地质大学构造与油气资源教育部重点实验室开放基金(TPR-2014-14)
Document Type期刊论文
Identifierhttp://ir.giec.ac.cn/handle/344007/16125
Collection中国科学院广州能源研究所
Affiliation1.国土资源部海底矿产资源重点实验室,广州海洋地质调查局,广州510075
2.中国科学院天然气水合物重点实验室,中国科学院广州能源研究所,广州510640
Recommended Citation
GB/T 7714
孙美静,彭学超,聂鑫,等. 珠江口盆地白云凹陷北坡上新世一第四纪陆架边缘沉积体系特征[J]. 海洋地质前沿,2015(8):41-46.
APA 孙美静,彭学超,聂鑫,&刘杰.(2015).珠江口盆地白云凹陷北坡上新世一第四纪陆架边缘沉积体系特征.海洋地质前沿(8),41-46.
MLA 孙美静,et al."珠江口盆地白云凹陷北坡上新世一第四纪陆架边缘沉积体系特征".海洋地质前沿 .8(2015):41-46.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[孙美静]'s Articles
[彭学超]'s Articles
[聂鑫]'s Articles
Baidu academic
Similar articles in Baidu academic
[孙美静]'s Articles
[彭学超]'s Articles
[聂鑫]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[孙美静]'s Articles
[彭学超]'s Articles
[聂鑫]'s Articles
Terms of Use
No data!
Social Bookmark/Share
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.