FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2025603156> ?p ?o ?g. }

• W2025603156 endingPage "168" @default.
• W2025603156 startingPage "157" @default.
• W2025603156 abstract "Subduction of the Indian lithosphere under Eurasia plays an important role in the tectonic evolution of the Tibetan plateau and surrounding regions. To improve our knowledge of pertinent mantle structures through tomographic imaging we combine P -wave arrival time data from temporary arrays in Tibet and stations of the Chinese Seismograph Network with reprocessed data from the International Seismological Centre. The new images reveal considerable spatial variations in mantle structure along the collision zone , and the horizontal distance over which presumed (continental) Indian lithosphere slides northward beneath the plateau decreases from west (where it underlies the Himalayas and the entire plateau) to east (where no indication is found for present-day underthrusting beyond the Himalayan Block and Indus–Tsangpo suture). P- wavespeed appears low in the shallow mantle beneath much of central and eastern Tibet. These observations suggest that Indian lithosphere underlies only the southwestern part of the plateau and that the central and northeastern part is underlain by lithosphere of Asian origin. The (continental) parts of the Indian plate that currently underthrust or subduct below the plateau appear generally detached from the (oceanic) slab fragments that subducted longer ago and that have been detected deeper in the mantle, except perhaps in the central part of the collision zone (80–90°E). This suggests that ongoing India–Eurasia collision must increasingly be driven by other forces, such as subduction of the Indian plate further west and east (e.g. beneath Indochina). Our images reveal structures associated with eastward subduction along the Burmese arc southeast of the eastern Himalayan syntaxis. The Tengchong volcanic complex in southwest China is marked by slow wave propagation to ~ 150 km depth, suggesting a causal link to subduction along the Burmese arc; the low velocities beneath the Red River fault region extend to greater depth and may be related to upper mantle processes further southeast." @default.
• W2025603156 created "2016-06-24" @default.
• W2025603156 creator A5010507750 @default.
• W2025603156 creator A5044199252 @default.
• W2025603156 creator A5069334991 @default.
• W2025603156 creator A5075725903 @default.
• W2025603156 date "2008-09-01" @default.
• W2025603156 modified "2023-09-30" @default.
• W2025603156 title "Subduction of the Indian lithosphere beneath the Tibetan Plateau and Burma" @default.
• W2025603156 cites W1493790006 @default.
• W2025603156 cites W1964042891 @default.
• W2025603156 cites W1964838527 @default.
• W2025603156 cites W1968327637 @default.
• W2025603156 cites W1974467019 @default.
• W2025603156 cites W1976967272 @default.
• W2025603156 cites W1977966931 @default.
• W2025603156 cites W1983049944 @default.
• W2025603156 cites W1989704882 @default.
• W2025603156 cites W1997859575 @default.
• W2025603156 cites W2002325302 @default.
• W2025603156 cites W2010635835 @default.
• W2025603156 cites W2012512380 @default.
• W2025603156 cites W2014462897 @default.
• W2025603156 cites W2020805787 @default.
• W2025603156 cites W2027934726 @default.
• W2025603156 cites W2031946574 @default.
• W2025603156 cites W2033800529 @default.
• W2025603156 cites W2036590770 @default.
• W2025603156 cites W2041498088 @default.
• W2025603156 cites W2041774199 @default.
• W2025603156 cites W2045569627 @default.
• W2025603156 cites W2056925848 @default.
• W2025603156 cites W2058269792 @default.
• W2025603156 cites W2063269424 @default.
• W2025603156 cites W2064361878 @default.
• W2025603156 cites W2064829413 @default.
• W2025603156 cites W2076823546 @default.
• W2025603156 cites W2084176139 @default.
• W2025603156 cites W2087071798 @default.
• W2025603156 cites W2094147317 @default.
• W2025603156 cites W2097897435 @default.
• W2025603156 cites W2103796536 @default.
• W2025603156 cites W2106921614 @default.
• W2025603156 cites W2107952396 @default.
• W2025603156 cites W2115518283 @default.
• W2025603156 cites W2119579051 @default.
• W2025603156 cites W2121290321 @default.
• W2025603156 cites W2122493817 @default.
• W2025603156 cites W2123355107 @default.
• W2025603156 cites W2124092109 @default.
• W2025603156 cites W2128135732 @default.
• W2025603156 cites W2131006763 @default.
• W2025603156 cites W2135159355 @default.
• W2025603156 cites W2135494568 @default.
• W2025603156 cites W2140334255 @default.
• W2025603156 cites W2144583290 @default.
• W2025603156 cites W2144762646 @default.
• W2025603156 cites W2145106077 @default.
• W2025603156 cites W2150938567 @default.
• W2025603156 cites W2153331827 @default.
• W2025603156 cites W2165878464 @default.
• W2025603156 cites W2170810558 @default.
• W2025603156 doi "https://doi.org/10.1016/j.epsl.2008.07.016" @default.
• W2025603156 hasPublicationYear "2008" @default.
• W2025603156 type Work @default.
• W2025603156 sameAs 2025603156 @default.
• W2025603156 citedByCount "531" @default.
• W2025603156 countsByYear W20256031562012 @default.
• W2025603156 countsByYear W20256031562013 @default.
• W2025603156 countsByYear W20256031562014 @default.
• W2025603156 countsByYear W20256031562015 @default.
• W2025603156 countsByYear W20256031562016 @default.
• W2025603156 countsByYear W20256031562017 @default.
• W2025603156 countsByYear W20256031562018 @default.
• W2025603156 countsByYear W20256031562019 @default.
• W2025603156 countsByYear W20256031562020 @default.
• W2025603156 countsByYear W20256031562021 @default.
• W2025603156 countsByYear W20256031562022 @default.
• W2025603156 countsByYear W20256031562023 @default.
• W2025603156 crossrefType "journal-article" @default.
• W2025603156 hasAuthorship W2025603156A5010507750 @default.
• W2025603156 hasAuthorship W2025603156A5044199252 @default.
• W2025603156 hasAuthorship W2025603156A5069334991 @default.
• W2025603156 hasAuthorship W2025603156A5075725903 @default.
• W2025603156 hasConcept C105702510 @default.
• W2025603156 hasConcept C113740112 @default.
• W2025603156 hasConcept C119477230 @default.
• W2025603156 hasConcept C127313418 @default.
• W2025603156 hasConcept C134306372 @default.
• W2025603156 hasConcept C151730666 @default.
• W2025603156 hasConcept C165205528 @default.
• W2025603156 hasConcept C16942324 @default.
• W2025603156 hasConcept C192367031 @default.
• W2025603156 hasConcept C2777327002 @default.
• W2025603156 hasConcept C2778261408 @default.
• W2025603156 hasConcept C2780030769 @default.
• W2025603156 hasConcept C33923547 @default.
• W2025603156 hasConcept C58097730 @default.

• next