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• W2079119359 endingPage "197" @default.
• W2079119359 startingPage "187" @default.
• W2079119359 abstract "A 700 km deep seismic velocity cross-section beneath the Lhasa to Golmud transect across the Tibetan plateau is presented. In contrast to the first version of this cross-section, which comprised an 800 km wide swath centred on the Lhasa to Golmud transect, due to the recent proliferation of publications concerning the mantle structure beneath Tibet, this study is based only on seismic profiles which either run along or cross the transect and arrays or studies which at least partly cover the transect. The results from the recent INDEPTH IV project indicate that the crustal thickness change from 70 km beneath the Songpan–Ganzi terrane and Kunlun mountains to 54 km beneath the Qaidam basin is located about 100 km north of the Kunlun Fault and almost 45 km north of the North Kunlun Thrust. The Qaidam basin Moho is underlain by crustal velocity material for almost 45 km and the apparently overlapping crustal material may represent Songpan–Ganzi lower crust underthrusting or flowing northward beneath the Qaidam basin Moho. Thus the high Tibetan plateau may be thickening northward into south Qaidam as its weak, thickened lower crust is injected beneath the stronger Qaidam crust. Beneath the crust, high-velocity, dense, cold Indian lithospheric mantle extends northwards until about the Banggong–Nujiang suture. Northwards, Asian lithospheric mantle is overlain by a low-velocity, less dense, warm Tibetan plate consisting of an upper lithospheric and a lower asthenospheric part. The apparent northwards deepening of the 410 and 660 km discontinuities by about 20 km implies that the upper mantle beneath north Tibet is slower, less dense and warmer than under south Tibet, in agreement with the observed uppermost mantle velocities. This, in turn, could provide some of the isostatic support for the high elevations in the north where the crust is somewhat thinner than in the southern plateau." @default.
• W2079119359 created "2016-06-24" @default.
• W2079119359 creator A5004297558 @default.
• W2079119359 creator A5068663349 @default.
• W2079119359 date "2013-10-01" @default.
• W2079119359 modified "2023-09-23" @default.
• W2079119359 title "A model of the crust and mantle structure down to 700 km depth beneath the Lhasa to Golmud transect across the Tibetan plateau as derived from seismological data" @default.
• W2079119359 cites W1532415420 @default.
• W2079119359 cites W1568278051 @default.
• W2079119359 cites W1667564097 @default.
• W2079119359 cites W1845341270 @default.
• W2079119359 cites W1914375665 @default.
• W2079119359 cites W1964108044 @default.
• W2079119359 cites W1964838527 @default.
• W2079119359 cites W1966431820 @default.
• W2079119359 cites W1968327637 @default.
• W2079119359 cites W1973250961 @default.
• W2079119359 cites W1974864488 @default.
• W2079119359 cites W1975639861 @default.
• W2079119359 cites W1977139589 @default.
• W2079119359 cites W1977440368 @default.
• W2079119359 cites W1978445071 @default.
• W2079119359 cites W1981438429 @default.
• W2079119359 cites W1983936487 @default.
• W2079119359 cites W1990695930 @default.
• W2079119359 cites W1991116113 @default.
• W2079119359 cites W2001021729 @default.
• W2079119359 cites W2001603858 @default.
• W2079119359 cites W2001820253 @default.
• W2079119359 cites W2006802934 @default.
• W2079119359 cites W2006936051 @default.
• W2079119359 cites W2007751710 @default.
• W2079119359 cites W2010819331 @default.
• W2079119359 cites W2012512380 @default.
• W2079119359 cites W2016033596 @default.
• W2079119359 cites W2016209199 @default.
• W2079119359 cites W2022449515 @default.
• W2079119359 cites W2022890384 @default.
• W2079119359 cites W2024090768 @default.
• W2079119359 cites W2025603156 @default.
• W2079119359 cites W2025768898 @default.
• W2079119359 cites W2027934726 @default.
• W2079119359 cites W2032342521 @default.
• W2079119359 cites W2034822468 @default.
• W2079119359 cites W2036078919 @default.
• W2079119359 cites W2036590770 @default.
• W2079119359 cites W2045673924 @default.
• W2079119359 cites W2045699793 @default.
• W2079119359 cites W2048995147 @default.
• W2079119359 cites W2049605743 @default.
• W2079119359 cites W2069875270 @default.
• W2079119359 cites W2071470124 @default.
• W2079119359 cites W2073684465 @default.
• W2079119359 cites W2075103055 @default.
• W2079119359 cites W2076823546 @default.
• W2079119359 cites W2082314404 @default.
• W2079119359 cites W2084176139 @default.
• W2079119359 cites W2086653277 @default.
• W2079119359 cites W2087071798 @default.
• W2079119359 cites W2088679672 @default.
• W2079119359 cites W2091261697 @default.
• W2079119359 cites W2091429264 @default.
• W2079119359 cites W2095367117 @default.
• W2079119359 cites W2101299597 @default.
• W2079119359 cites W2102864817 @default.
• W2079119359 cites W2103789938 @default.
• W2079119359 cites W2107952396 @default.
• W2079119359 cites W2110779410 @default.
• W2079119359 cites W2116027322 @default.
• W2079119359 cites W2116309200 @default.
• W2079119359 cites W2119915260 @default.
• W2079119359 cites W2122084771 @default.
• W2079119359 cites W2124092109 @default.
• W2079119359 cites W2125218893 @default.
• W2079119359 cites W2128523303 @default.
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• W2079119359 cites W2148418336 @default.
• W2079119359 cites W2148490873 @default.
• W2079119359 cites W2149578166 @default.
• W2079119359 cites W2150938567 @default.
• W2079119359 cites W2164395980 @default.
• W2079119359 cites W2164681216 @default.
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• W2079119359 doi "https://doi.org/10.1016/j.tecto.2013.04.030" @default.
• W2079119359 hasPublicationYear "2013" @default.
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