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DOI | 10.1126/science.1010580 |
Detection of widespread fluids in the Tibetan crust by magnetotelluric studies | |
Wei W.; Unsworth M.; Jones A.; Booker J.; Tan H.; Nelson D.; Chen L.; Li S.; Solon K.; Bedrosian P.; Jin S.; Deng M.; Ledo J.; Kay D.; Roberts B. | |
发表日期 | 2001 |
ISSN | 0036-8075 |
起始页码 | 716 |
结束页码 | 718 |
卷号 | 292期号:5517 |
英文摘要 | Magnetotelluric exploration has shown that the middle and lower crust is anomalously conductive across most of the north-to-south width of the Tibetan plateau. The integrated conductivity (conductance) of the Tibetan crust ranges from 3000 to greater than 20,000 siemens. In contrast, stable continental regions typically exhibit conductances from 20 to 1000 siemens, averaging 100 siemens. Such pervasively high conductance suggests that partial melt and/or aqueous fluids are widespread within the Tibetan crust. In southern Tibet, the high-conductivity layer is at a depth of 15 to 20 kilometers and is probably due to partial melt and aqueous fluids in the crust. In northern Tibet, the conductive layer is at 30 to 40 kilometers and is due to partial melting. Zones of fluid may represent weaker areas that could accommodate deformation and lower crustal flow. |
英文关键词 | Electric conductance; Fluids; Geomagnetism; Magnetotelluric exploration; Geology; crustal structure; magnetotelluric method; partial melting; aqueous solution; article; conductance; geology; liquid; magnetism; melting point; priority journal; China |
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/245995 |
作者单位 | Institute of Geophysical Research, University of Alberta, Edmonton, Alta. T6G 2JI, Canada |
推荐引用方式 GB/T 7714 | Wei W.,Unsworth M.,Jones A.,et al. Detection of widespread fluids in the Tibetan crust by magnetotelluric studies[J],2001,292(5517). |
APA | Wei W..,Unsworth M..,Jones A..,Booker J..,Tan H..,...&Roberts B..(2001).Detection of widespread fluids in the Tibetan crust by magnetotelluric studies.Science,292(5517). |
MLA | Wei W.,et al."Detection of widespread fluids in the Tibetan crust by magnetotelluric studies".Science 292.5517(2001). |
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