准噶尔地块二叠纪岩脉的古地磁研究

全文: PDF(389 KB)
输出: BibTeX | EndNote (RIS)

摘要

作者通过对准噶尔地块的岩脉采样的古地磁研究以及大量地质资料,确认了准噶尔地块在早二叠世位于北纬35°,与塔里木地块、哈萨克斯坦地块及西伯利亚基本上在同一纬度带中,作为劳亚大陆的一个组成部分,作者并对该区自早二叠世以来的构造变动作了分析.

	服务

	把本文推荐给朋友
	加入引用管理器
	E-mail Alert
	RSS
	作者相关文章

Abstract：

On the basis of paleomagnetic study of samples collected from dykes inJunggar massif and large quantities of geological data, it is confirmed thatJunggar massif was located 35° north latitude in Early Permian, lying basically in the same latitude zone as Tarim massif, Kazakhstan massif and Siberia andserving as a component part of Laurasis continent. The authors have also madean analysis of tectonism in this area since Early Permian.

出版日期: 1991-06-24

引用本文:

李永安, 李强, 张慧, 李燕平, R. Sharps, M. McWilliams. 准噶尔地块二叠纪岩脉的古地磁研究[J]. 物探与化探, 1991, 15(3): 182-187.
Li Yongan, Li Qiang, Zhang Huai, Li Yanping, R. Sharps, M. McWilliams. PALEOMAGNETIC STUDY OF PERMIAN DYKES INJUNGGAR MASSIF. Geophysical and Geochemical Exploration, 1991, 15(3): 182-187.

链接本文:

https://www.wutanyuhuatan.com/CN/ 或 https://www.wutanyuhuatan.com/CN/Y1991/V15/I3/182

［1］新疆地矿局,1985,中国新疆维吾尔自治区地质图及说明书,地质出版社.
［2］李燕平、李永安、张正坤、翟永健、李强、高振家、R, Shares, M. McWilliams, 1989,中国塔里木地块的视极移曲线,地质学报,第63卷,第3期.
［3］胡雨帆,1985,试论中国西部地区二叠纪植物区系特征,中国区域地质,第12辑.
［4］白云虹、程国良、孙春格、孙宇航、李永安、董玉杰、孙东江,1985,新疆塔里木地台晚古生代占地磁极移曲线及其地质构造含义,地震地质,第7卷,第1期.
［5］晋慧娟、李八慈,198S,博格达山西南麓晚古生代风暴岩一半深海块体搬运沉积物及其形成的构造背景,沉积学报,增刊.
［6］李育慈、晋慧娟,1989,准噶尔盆地西北缘石炭纪深水沉积与油气关系的探讨,沉积学报,增刊.
［7］新疆地矿局地质矿产研究所,1988,新疆古地理图集,新疆人民出版社.
［8］ G. Tilton, S. Kwon, H. Colwnan and X. Xiao, :!986, Tsotoeic studies from the West Junggar Mts., NW China (abstract),Geol. Sos. Ant. Abstr. Progr. 773.
［9］ A. N. Khramov, G. N. Petroea and D. M. Pechersky, 1981, Paleotnagnetism of the soutet Uaion, Am.Geophys. Union. Geodyn. Ser. 2;
［10］ P. McPadden, R. Merrill and M. McFlhinny, 1988, Dipole/quaclrupole family modeling of Paleosecular variation, J. Geophys. Res. 93.