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DOI | 10.1126/science.1078115 |
Seismic images of crust and upper mantle beneath Tibet: Evidence for Eurasian plate subduction | |
Kind R.; Yuan X.; Saul J.; Nelson D.; Sobolev S.V.; Mechie J.; Zhao W.; Kosarev G.; Ni J.; Achauer U.; Jiang M. | |
发表日期 | 2002 |
ISSN | 0036-8075 |
起始页码 | 1219 |
结束页码 | 1221 |
卷号 | 298期号:5596 |
英文摘要 | Seismic data from central Tibet have been combined to image the subsurface structure and understand the evolution of the collision of India and Eurasia. The 410- and 660-kilometer mantle discontinuities are sharply defined, implying a lack of a subducting slab beneath the plateau. The discontinuities appear slightly deeper beneath northern Tibet, implying that the average temperature of the mantle above the transition zone is about 300°C hotter in the north than in the south. There is a prominent south-dipping converter in the uppermost mantle beneath northern Tibet that might represent the top of the Eurasian mantle lithosphere underthrusting the northern margin of the plateau. |
英文关键词 | Geographical regions; Image analysis; Lithology; Seismic prospecting; Mantle discontinuities; Subsurface structures; Tectonics; continental collision; crust; Eurasian plate; seismic data; subduction; tectonic evolution; upper mantle; article; atmosphere; China; compression; earthquake; environmental temperature; evolution; measurement; priority journal; shear stress; China |
语种 | 英语 |
来源期刊 | Science
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/244323 |
作者单位 | GeoForschungsZentrum Potsdam, 14473 Potsdam, Germany |
推荐引用方式 GB/T 7714 | Kind R.,Yuan X.,Saul J.,et al. Seismic images of crust and upper mantle beneath Tibet: Evidence for Eurasian plate subduction[J],2002,298(5596). |
APA | Kind R..,Yuan X..,Saul J..,Nelson D..,Sobolev S.V..,...&Jiang M..(2002).Seismic images of crust and upper mantle beneath Tibet: Evidence for Eurasian plate subduction.Science,298(5596). |
MLA | Kind R.,et al."Seismic images of crust and upper mantle beneath Tibet: Evidence for Eurasian plate subduction".Science 298.5596(2002). |
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