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DOI10.1126/science.283.5406.1306
Seismic evidence for a detached indian lithospheric mantle beneath tibet
Kosarev C.; Kind R.; Sobolev S.V.; Yuan X.; Hanka W.; Oreshin S.
发表日期1999
ISSN0036-8075
起始页码1306
结束页码1309
卷号283期号:5406
英文摘要P-to-S converted teleseismic waves recorded by temporary broadband networks across Tibet show a north-dipping interface that begins 50 kilometers north of the Zangbo suture at the depth of the Moho (80 kilometers) and extends to a depth of 200 kilometers beneath the Bangong suture. Under northern Tibet a segmented south-dipping structure was imaged. These observations suggest a different form of detachment of the Indian and Asian lithospheric mantles caused by differences in their composition and buoyancy.
英文关键词lithospheric structure; seismic wave; article; Asia; earthquake; geography; geology; India; natural science; priority journal; China; Moho
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/244396
作者单位Inst. of the Physics of the Earth, Russian Academy of Sciences, B. Gruzinskaya 10, 128810 Moscow, Russian Federation; GeoForschungsZentrum Potsdam, Telegrafenberg, 14473 Potsdam, Germany; Freie Universität Berlin, Geophysik, Malteser Strasse 74-100, 12249 Berlin, Germany
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Kosarev C.,Kind R.,Sobolev S.V.,et al. Seismic evidence for a detached indian lithospheric mantle beneath tibet[J],1999,283(5406).
APA Kosarev C.,Kind R.,Sobolev S.V.,Yuan X.,Hanka W.,&Oreshin S..(1999).Seismic evidence for a detached indian lithospheric mantle beneath tibet.Science,283(5406).
MLA Kosarev C.,et al."Seismic evidence for a detached indian lithospheric mantle beneath tibet".Science 283.5406(1999).
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