气候变化领域集成服务门户(CCPortal): Electrically conductive crust in southern Tibet from INDEPTH magnetotelluric surveying

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DOI	10.1126/science.274.5293.1694
	Electrically conductive crust in southern Tibet from INDEPTH magnetotelluric surveying
	Chen L.; Booker J.R.; Jones A.G.; Wu N.; Unsworth M.J.; Wei W.; Tan H.
发表日期	1996
ISSN	0036-8075
起始页码	1694
结束页码	1696
卷号	274 期号:5293
英文摘要	The crust north of the Himalaya is generally electrically conductive below depths of 10 to 20 km. This conductive zone approaches the surface beneath the Kangmar dome (dipping north) and extends beneath the Zangbo suture. A profile crossing the northern Yadong-Gulu rift shows that the high conductivity region extends outside the rift, and its top within the rift coincides with a bright spot horizon imaged on the INDEPTH CMP (common midpoint) profiles. The high conductivity of the middle crust is atypical of stable continental regions and suggests that there is a regionally interconnected fluid phase in the crust of the region.
英文关键词	article; china; diagnostic procedure; electrical conductivity parameters; electricity; electromagnetic field; geographic distribution; geology; image analysis; priority journal
语种	英语
来源期刊	Science
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/243294
作者单位	China University of Geosciences, Beijing, China; School of Geophysics, University of Washington, Seattle, WA 98195, United States; Geological Survey of Canada, 1 Observatory Crescent, Ottawa, Ont. K1A 0Y3, Canada
推荐引用方式 GB/T 7714	Chen L.,Booker J.R.,Jones A.G.,et al. Electrically conductive crust in southern Tibet from INDEPTH magnetotelluric surveying[J],1996,274(5293).
APA	Chen L..,Booker J.R..,Jones A.G..,Wu N..,Unsworth M.J..,...&Tan H..(1996).Electrically conductive crust in southern Tibet from INDEPTH magnetotelluric surveying.Science,274(5293).
MLA	Chen L.,et al."Electrically conductive crust in southern Tibet from INDEPTH magnetotelluric surveying".Science 274.5293(1996).