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DOI10.1126/science.1082777
Seismic imaging of the downwelling Indian lithosphere beneath central Tibet
Tilmann F.; Ni J.; Hearn T.; Ma Y.S.; Rapine R.; Kind R.; Mechie J.; Saul J.; Haines S.; Klemperer S.; Brown L.; Pananont P.; Ross A.; Nelson K.D.; Guo J.; Zhao W.
发表日期2003
ISSN0036-8075
起始页码1424
结束页码1427
卷号300期号:5624
英文摘要A tomographic image of the upper mantle beneath central Tibet from INDEPTH data has revealed a subvertical high-velocity zone from ∼100- to ∼400-kilometers depth, located approximately south of the Bangong-Nujiang Suture. We interpret this zone to be downwelling Indian mantle lithosphere. This additional lithosphere would account for the total amount of shortening in the Himalayas and Tibet. A consequence of this downwelling would be a deficit of asthenosphere, which should be balanced by an upwelling counterflow, and thus could explain the presence of warm mantle beneath north-central Tibet.
英文关键词Approximation theory; Image analysis; Tomography; Seismic imaging; Seismology; crustal structure; lithospheric structure; mantle structure; seismic velocity; tomography; article; atmosphere; China; image analysis; imaging system; India; measurement; priority journal; tomography; velocity; 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/245756
作者单位Department of Physics, New Mexico State University, Las Cruces, NM 88003, United States; New Mexico State Univ., Las Cruces, NM, United States; Stanford Univ., Stanford, CA, United States; Cornell Univ., Ithaca, NY, United States; Syracuse Univ., Syracuse, NY, United States; Department of Earth Sciences, Cambridge University, Cambridge CB3 0EZ, United Kingdom
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GB/T 7714
Tilmann F.,Ni J.,Hearn T.,et al. Seismic imaging of the downwelling Indian lithosphere beneath central Tibet[J],2003,300(5624).
APA Tilmann F..,Ni J..,Hearn T..,Ma Y.S..,Rapine R..,...&Zhao W..(2003).Seismic imaging of the downwelling Indian lithosphere beneath central Tibet.Science,300(5624).
MLA Tilmann F.,et al."Seismic imaging of the downwelling Indian lithosphere beneath central Tibet".Science 300.5624(2003).
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