IMHE OpenIR  > 山地灾害与地表过程重点实验室
Alternative TitleMagnetostratigraphy of Borehole SZ04 in the Yangtze River Delta and Its Implications
张平; 李向前; 潘明宝; 宗开红; 苗巧银; 李永祥; 欧健; 冯文立; 季文婷 刘维明
Corresponding Author张平
Source Publication沉积学报
Abstract文章对位于长江三角洲南翼平原区西部的SZ04孔进行了详细的磁性地层学研究。结合绝对测年,并与标准极性柱对比认为269.2 m岩芯清楚的记录了布容(Brunhes)、松山(Matuyama)、高斯(Gauss)极性带,及贾拉米洛(Jaramillo)、奥尔都维(Olduvai)等亚极性带和布莱克(Black)地磁漂移,其中B/M、M/G界限深度分别为100 m和155 m;SZ04孔底部碎屑沉积物形成的年龄大于5.23 Ma。研究发现,钻孔沉积物磁化率、岩石地层特征在特殊的时代界限附近有明显变化可进行区域对比。分析表明,第四纪以来长江三角洲地区一直存在持续的构造沉降,且沉降中心持续往南东方向移动,构造沉降运动的发生和发展存在三个重要的期次分别为2.58 Ma,0.78 Ma和0.125 Ma。
Other AbstractThis study aims to establish a high resolution paleomagnetic age scale of Borehole SZ04 (269.2 m in length) which was drilled from the western part of plain region on the south flank of the Yangtze River Delta. Combining with the absolute age and compared with the standard polarity column, the results show that the 269.2 m core consists of three polarity events including Brunhes, Matuyama and Gauss and three subpolarity events including Black, Jaramillo and Olduvai. The B/M and the M/G boundary are found at the depth of 100 m and 155 m, respectively; Clastic deposit at the bottom of Borehole SZ04 was formed at about 5.23 Ma. Analysis of the dating results indicates that obvious changes of the sediments magnetic susceptibility and lithostratigraphy characteristic are existed near each particular boundaries, which can be correlated with in a large region. Therefore, it is concluded that crust subsidence in this region was continuously occurred since Quaternary, accompanied with the subsidence center moving to the south and the crust subsidence activities were concentrated and intensified in three important time phase at about 2.58 Ma, 0.78 Ma and 0.125 Ma.
Keyword长江三角洲 Sz04孔 磁性地层 极性带
Subject Area第四纪地质学
Indexed ByCSCD
Citation statistics
Cited Times:6[CSCD]   [CSCD Record]
Document Type期刊论文
Corresponding Author张平
Recommended Citation
GB/T 7714
张平,李向前,潘明宝,等. 长江三角洲SZ04孔磁性地层研究及其意义[J]. 沉积学报,2013,31(6):1041-1049.
APA 张平.,李向前.,潘明宝.,宗开红.,苗巧银.,...&季文婷 刘维明.(2013).长江三角洲SZ04孔磁性地层研究及其意义.沉积学报,31(6),1041-1049.
MLA 张平,et al."长江三角洲SZ04孔磁性地层研究及其意义".沉积学报 31.6(2013):1041-1049.
Files in This Item:
File Name/Size DocType Version Access License
长江三角洲SZ04孔磁性地层研究.pdf(1066KB) 开放获取CC BY-NC-SAView Application Full Text
Related Services
Recommend this item
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[张平]'s Articles
[李向前]'s Articles
[潘明宝]'s Articles
Baidu academic
Similar articles in Baidu academic
[张平]'s Articles
[李向前]'s Articles
[潘明宝]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[张平]'s Articles
[李向前]'s Articles
[潘明宝]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: 长江三角洲SZ04孔磁性地层研究.pdf
Format: Adobe PDF
This file does not support browsing at this time
All comments (0)
No comment.

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