FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022871572> ?p ?o ?g. }

• W2022871572 endingPage "84" @default.
• W2022871572 startingPage "74" @default.
• W2022871572 abstract "The Liuqu Conglomerate, exposed along the Yarlung-Zangbo suture zone in southern Tibet, has been interpreted as a Paleogene molasse deposited during India–Asia collision or the product of collision between India and an intra-oceanic arc. Detailed petrographic studies and analyses of U–Pb and Hf isotopes of detrital zircon indicate multiple sources for the conglomerate, including the sedimentary succession within the Xigaze forearc basin to the north of the suture, the Yarlung-Zangbo ophiolite within the suture itself, and the Langjiexue Group and Tethyan Himalayan sedimentary rocks to the south of the suture. The occurrence of clasts of both Indian and Asian origin suggests that the conglomerate was deposited after India–Asia collision. The present data suggest that the onset of Himalayan–Tibetan orogenic erosion occurred as early as the Middle Eocene, when the Yarlung-Zangbo suture zone and Xigaze forearc succession were uplifted and became sources for the Liuqu Conglomerate. Thus, the results are inconsistent with the proposal that the provenance and age of the Liuqu Conglomerate support the hypothesis that India–Asia collision did not occur until the Oligocene. It is further suggested that Eocene Neotethyan slab breakoff, which may result in accelerated exhumation and uplift of the orogen, provided a deep-level dynamic control on the deposition of the Liuqu Conglomerate." @default.
• W2022871572 created "2016-06-24" @default.
• W2022871572 creator A5023735787 @default.
• W2022871572 creator A5038111698 @default.
• W2022871572 creator A5047814321 @default.
• W2022871572 creator A5061287436 @default.
• W2022871572 date "2010-11-01" @default.
• W2022871572 modified "2023-09-26" @default.
• W2022871572 title "Provenance of the Liuqu Conglomerate in southern Tibet: A Paleogene erosional record of the Himalayan–Tibetan orogen" @default.
• W2022871572 cites W1488283778 @default.
• W2022871572 cites W1538567586 @default.
• W2022871572 cites W1871734886 @default.
• W2022871572 cites W1959048442 @default.
• W2022871572 cites W1969685321 @default.
• W2022871572 cites W1975501184 @default.
• W2022871572 cites W1976467450 @default.
• W2022871572 cites W1976963145 @default.
• W2022871572 cites W1981207838 @default.
• W2022871572 cites W1997698506 @default.
• W2022871572 cites W2003835722 @default.
• W2022871572 cites W2012416391 @default.
• W2022871572 cites W2013727374 @default.
• W2022871572 cites W2013747285 @default.
• W2022871572 cites W2015923510 @default.
• W2022871572 cites W2019679381 @default.
• W2022871572 cites W2020471886 @default.
• W2022871572 cites W2020595994 @default.
• W2022871572 cites W2020973699 @default.
• W2022871572 cites W2024462757 @default.
• W2022871572 cites W2025750942 @default.
• W2022871572 cites W2027225510 @default.
• W2022871572 cites W2030661236 @default.
• W2022871572 cites W2031013946 @default.
• W2022871572 cites W2032188738 @default.
• W2022871572 cites W2035162197 @default.
• W2022871572 cites W2037089269 @default.
• W2022871572 cites W2050487135 @default.
• W2022871572 cites W2051273227 @default.
• W2022871572 cites W2051298113 @default.
• W2022871572 cites W2051327427 @default.
• W2022871572 cites W2052839102 @default.
• W2022871572 cites W2053480315 @default.
• W2022871572 cites W2054590577 @default.
• W2022871572 cites W2055356153 @default.
• W2022871572 cites W2055406819 @default.
• W2022871572 cites W2065105994 @default.
• W2022871572 cites W2068668821 @default.
• W2022871572 cites W2073739165 @default.
• W2022871572 cites W2074776366 @default.
• W2022871572 cites W2075385990 @default.
• W2022871572 cites W2076395812 @default.
• W2022871572 cites W2082181291 @default.
• W2022871572 cites W2090206242 @default.
• W2022871572 cites W2095674345 @default.
• W2022871572 cites W2097595144 @default.
• W2022871572 cites W2097671688 @default.
• W2022871572 cites W2102081901 @default.
• W2022871572 cites W2105191111 @default.
• W2022871572 cites W2106465464 @default.
• W2022871572 cites W2106802393 @default.
• W2022871572 cites W2110179328 @default.
• W2022871572 cites W2112077113 @default.
• W2022871572 cites W2115518283 @default.
• W2022871572 cites W2124299111 @default.
• W2022871572 cites W2125981652 @default.
• W2022871572 cites W2127250595 @default.
• W2022871572 cites W2128209044 @default.
• W2022871572 cites W2130419354 @default.
• W2022871572 cites W2140087217 @default.
• W2022871572 cites W2142145377 @default.
• W2022871572 cites W2143270202 @default.
• W2022871572 cites W2146622853 @default.
• W2022871572 cites W2148928597 @default.
• W2022871572 cites W2161702350 @default.
• W2022871572 cites W2265202465 @default.
• W2022871572 doi "https://doi.org/10.1016/j.sedgeo.2010.09.004" @default.
• W2022871572 hasPublicationYear "2010" @default.
• W2022871572 type Work @default.
• W2022871572 sameAs 2022871572 @default.
• W2022871572 citedByCount "44" @default.
• W2022871572 countsByYear W20228715722012 @default.
• W2022871572 countsByYear W20228715722013 @default.
• W2022871572 countsByYear W20228715722014 @default.
• W2022871572 countsByYear W20228715722015 @default.
• W2022871572 countsByYear W20228715722016 @default.
• W2022871572 countsByYear W20228715722017 @default.
• W2022871572 countsByYear W20228715722018 @default.
• W2022871572 countsByYear W20228715722019 @default.
• W2022871572 countsByYear W20228715722021 @default.
• W2022871572 countsByYear W20228715722022 @default.
• W2022871572 countsByYear W20228715722023 @default.
• W2022871572 crossrefType "journal-article" @default.
• W2022871572 hasAuthorship W2022871572A5023735787 @default.
• W2022871572 hasAuthorship W2022871572A5038111698 @default.
• W2022871572 hasAuthorship W2022871572A5047814321 @default.
• W2022871572 hasAuthorship W2022871572A5061287436 @default.
• W2022871572 hasConcept C105702510 @default.
• W2022871572 hasConcept C106804226 @default.

• next