Matches in SemOpenAlex for { <https://semopenalex.org/work/W2195992687> ?p ?o ?g. }
- W2195992687 endingPage "234" @default.
- W2195992687 startingPage "222" @default.
- W2195992687 abstract "The Xiukang Mélange of the Yarlung-Zangbo suture zone in south Tibet documents low efficiency of accretion along the southern active margin of Asia during Cretaceous Neotethyan subduction, followed by final development during the early Paleogene stages of the India–Asia collision. Here we present integrated petrologic, U–Pb detrital-zircon geochronology and Hf isotope data on different types of sandstone blocks in the Xiukang Mélange. Three groups of sandstone blocks with different provenance and depositional setting are distinguished by their petrographic, geochronological and isotopic fingerprints. Blocks of turbiditic quartzarenite originally sourced from the Indian continent were deposited in pre-Cretaceous time on the northernmost edge of the Indian passive margin and eventually involved into the mélange at the early stage of the India–Asia collision. Two distinct groups of volcaniclastic-sandstone blocks were derived from the central Lhasa block and Gangdese magmatic arc. One group was deposited in the trench and/or on the trench slope of the Asian margin during the early Late Cretaceous, and the other group in a syn-collisional basin just after the onset of the India–Asia collision in the Early Eocene. The largely erosional character of the Asian active margin in the Late Cretaceous is indicated by the scarcity of off-scraped trench-fill deposits and the relatively small subduction complex developed during limited episodes of accretion. The Xiukang Mélange was finally structured in the Late Paleocene/Eocene, when sandstone blocks of both Indian and Asian origin were progressively incorporated tectonically in the suture zone of the nascent Himalayan Orogen." @default.
- W2195992687 created "2016-06-24" @default.
- W2195992687 creator A5011011554 @default.
- W2195992687 creator A5025749069 @default.
- W2195992687 creator A5038111698 @default.
- W2195992687 date "2017-01-01" @default.
- W2195992687 modified "2023-10-17" @default.
- W2195992687 title "Sandstone provenance and tectonic evolution of the Xiukang Mélange from Neotethyan subduction to India–Asia collision (Yarlung-Zangbo suture, south Tibet)" @default.
- W2195992687 cites W1488283778 @default.
- W2195992687 cites W1671207528 @default.
- W2195992687 cites W1890006364 @default.
- W2195992687 cites W1944076124 @default.
- W2195992687 cites W1959048442 @default.
- W2195992687 cites W1965256236 @default.
- W2195992687 cites W1965425556 @default.
- W2195992687 cites W1965598263 @default.
- W2195992687 cites W1974653614 @default.
- W2195992687 cites W1975501184 @default.
- W2195992687 cites W1975615717 @default.
- W2195992687 cites W1976568771 @default.
- W2195992687 cites W1976963145 @default.
- W2195992687 cites W1976967272 @default.
- W2195992687 cites W1977073296 @default.
- W2195992687 cites W1978465122 @default.
- W2195992687 cites W1982501717 @default.
- W2195992687 cites W1982581643 @default.
- W2195992687 cites W1984200080 @default.
- W2195992687 cites W1986045856 @default.
- W2195992687 cites W1987671538 @default.
- W2195992687 cites W1994476706 @default.
- W2195992687 cites W1998789817 @default.
- W2195992687 cites W2003835722 @default.
- W2195992687 cites W2011876596 @default.
- W2195992687 cites W2012416391 @default.
- W2195992687 cites W2016427837 @default.
- W2195992687 cites W2016976548 @default.
- W2195992687 cites W2017512729 @default.
- W2195992687 cites W2019679381 @default.
- W2195992687 cites W2019748000 @default.
- W2195992687 cites W2020371038 @default.
- W2195992687 cites W2020483745 @default.
- W2195992687 cites W2020973699 @default.
- W2195992687 cites W2022880292 @default.
- W2195992687 cites W2030661236 @default.
- W2195992687 cites W2030800261 @default.
- W2195992687 cites W2031013946 @default.
- W2195992687 cites W2031447434 @default.
- W2195992687 cites W2032184518 @default.
- W2195992687 cites W2034798494 @default.
- W2195992687 cites W2037035891 @default.
- W2195992687 cites W2046517163 @default.
- W2195992687 cites W2047634242 @default.
- W2195992687 cites W2055406819 @default.
- W2195992687 cites W2059165230 @default.
- W2195992687 cites W2062678238 @default.
- W2195992687 cites W2066045233 @default.
- W2195992687 cites W2070470769 @default.
- W2195992687 cites W2073739165 @default.
- W2195992687 cites W2075694434 @default.
- W2195992687 cites W2075929412 @default.
- W2195992687 cites W2076395812 @default.
- W2195992687 cites W2080013106 @default.
- W2195992687 cites W2081918183 @default.
- W2195992687 cites W2082181291 @default.
- W2195992687 cites W2083159755 @default.
- W2195992687 cites W2085337907 @default.
- W2195992687 cites W2085600742 @default.
- W2195992687 cites W2093240326 @default.
- W2195992687 cites W2097103166 @default.
- W2195992687 cites W2097595144 @default.
- W2195992687 cites W2105246524 @default.
- W2195992687 cites W2107624787 @default.
- W2195992687 cites W2112836744 @default.
- W2195992687 cites W2114125023 @default.
- W2195992687 cites W2115518283 @default.
- W2195992687 cites W2122170492 @default.
- W2195992687 cites W2127250595 @default.
- W2195992687 cites W2133079848 @default.
- W2195992687 cites W2135830789 @default.
- W2195992687 cites W2137645231 @default.
- W2195992687 cites W2137782692 @default.
- W2195992687 cites W2141391066 @default.
- W2195992687 cites W2142145377 @default.
- W2195992687 cites W2148928597 @default.
- W2195992687 cites W2149951012 @default.
- W2195992687 cites W2158535335 @default.
- W2195992687 cites W2161702350 @default.
- W2195992687 cites W2317391324 @default.
- W2195992687 cites W2318607738 @default.
- W2195992687 cites W2326048568 @default.
- W2195992687 cites W2615048764 @default.
- W2195992687 doi "https://doi.org/10.1016/j.gr.2015.08.010" @default.
- W2195992687 hasPublicationYear "2017" @default.
- W2195992687 type Work @default.
- W2195992687 sameAs 2195992687 @default.
- W2195992687 citedByCount "53" @default.
- W2195992687 countsByYear W21959926872016 @default.
- W2195992687 countsByYear W21959926872017 @default.