中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Magnetostratigraphic investigations on an Emeishan basalt section in western Guizhou province, China

文献类型:期刊论文

作者Huang, K; Opdyke, ND
刊名EARTH AND PLANETARY SCIENCE LETTERS
出版日期1998-11-01
卷号163期号:1-4页码:1-14
关键词magnetostratigraphy basalts Guizhou China Yangtze platform
ISSN号0012-821X
文献子类Article
英文摘要A magnetostratigraphic investigation has been conducted on a late Permian Emeishan basalt section at Duge in western Guizhou province, China. The characteristic remanent magnetization (ChRM) directions resolved at high temperatures from the basalts pass the fold test with dual polarity and define a normal magnetozone of five sixths of the total thickness in the lower part and a reversed magnetozone of one sixth of the thickness in the top part of the section. The ChRM directions from the basalt clasts of pyroclastic rocks fail the conglomerate test, but the direction and polarity of the ChRM of the clasts from the upper reversed zone are consistent with those of the basaltic lavas in the reversed zone and the normal directions also dominate the ChRM of the clasts taken from the lower normal zone. This suggests that either the original remanence of the clasts was reset by cementing basaltic lavas or the ChRM of the basalts was acquired late but not beyond a field reversal. The magnetostratigraphic pattern (N-R) observed at Duge is as simple as that observed from some major continental flood basalt provinces in the world, where very few magnetic polarity zones were observed from volcanic sequences of great thickness; the emplacement of the Emeishan basalts in western Guizhou is estimated to be less than two million years. The normal polarity magnetozone observed indicates that the extrusion of the Emeishan basalts in western Guizhou postdates the Permo-Carboniferous reversed superchron (PCRS). The apparent shortness of the reversed magnetozone explains why far fewer reverse directions than normal ones have been so far reported from the Emeishan basalts. (C) 1998 Elsevier Science B.V. All rights reserved.
WOS关键词SOUTHWEST CHINA ; FLOOD BASALTS ; PALEOMAGNETISM ; REMAGNETIZATION ; ROCKS
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000077181400001
出版者ELSEVIER SCIENCE BV
源URL[http://ir.iggcas.ac.cn/handle/132A11/74998]  
专题中国科学院地质与地球物理研究所
通讯作者Huang, K
作者单位1.Univ Florida, Dept Geol, Gainesville, FL 32611 USA
2.Chinese Acad Sci, Inst Geophys, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Huang, K,Opdyke, ND. Magnetostratigraphic investigations on an Emeishan basalt section in western Guizhou province, China[J]. EARTH AND PLANETARY SCIENCE LETTERS,1998,163(1-4):1-14.
APA Huang, K,&Opdyke, ND.(1998).Magnetostratigraphic investigations on an Emeishan basalt section in western Guizhou province, China.EARTH AND PLANETARY SCIENCE LETTERS,163(1-4),1-14.
MLA Huang, K,et al."Magnetostratigraphic investigations on an Emeishan basalt section in western Guizhou province, China".EARTH AND PLANETARY SCIENCE LETTERS 163.1-4(1998):1-14.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。