Matches in SemOpenAlex for { <https://semopenalex.org/work/W3201908788> ?p ?o ?g. }
- W3201908788 abstract "The Jurassic–Cretaceous Tsoltak Formation from the eastern borderlands of Ladakh Himalaya consists of conglomerates, sandstones and shales, and is intruded by norite sills. It is the oldest sequence of continent-derived sedimentary rocks within the Shyok Suture. It also represents a rare outcrop of the basement rocks to the voluminous Late Cretaceous–Eocene Ladakh Batholith. The Shyok Formation is a younger sequence of volcaniclastic rocks that overlie the Tsoltak Formation and record the Late Cretaceous closure of the Mesotethys Ocean. The petrogenesis of these formations, ophiolite-related harzburgites and norite sill is investigated through petrography, whole-rock geochemistry and U–Pb zircon geochronology. The youngest detrital zircon grains from the Tsoltak Formation indicate Early Cretaceous maximum depositional age and distinctly Gondwanan, Lhasa microcontinent-related provenance with no Eurasian input. The Shyok Formation has Late Cretaceous maximum depositional age and displays a distinct change in provenance to igneous detritus characteristic of the Jurassic–Cretaceous magmatic arc along the southern margin of Eurasia. This is interpreted as a sign of collision of the Lhasa microcontinent and the Shyok ophiolite with Eurasia along the once continuous Shyok–Bangong Suture. The accreted terranes became the new southernmost margin of Eurasia and the basement to the Trans-Himalayan Batholith associated with the India-Eurasia convergence. Supplementary material: https://doi.org/10.6084/m9.figshare.c.5633162" @default.
- W3201908788 created "2021-10-11" @default.
- W3201908788 creator A5002586631 @default.
- W3201908788 creator A5063726774 @default.
- W3201908788 creator A5075006383 @default.
- W3201908788 creator A5082680064 @default.
- W3201908788 date "2021-10-28" @default.
- W3201908788 modified "2023-10-15" @default.
- W3201908788 title "Jurassic–Cretaceous arc magmatism along the Shyok–Bangong Suture of NW Himalaya: formation of the peri-Gondwana basement to the Ladakh Arc" @default.
- W3201908788 cites W141993106 @default.
- W3201908788 cites W1579624063 @default.
- W3201908788 cites W1963523229 @default.
- W3201908788 cites W1963662898 @default.
- W3201908788 cites W1969859799 @default.
- W3201908788 cites W1969894116 @default.
- W3201908788 cites W1970268065 @default.
- W3201908788 cites W1970363584 @default.
- W3201908788 cites W1977073296 @default.
- W3201908788 cites W1980860725 @default.
- W3201908788 cites W1983425689 @default.
- W3201908788 cites W1984100307 @default.
- W3201908788 cites W1989982832 @default.
- W3201908788 cites W1993290622 @default.
- W3201908788 cites W1998621819 @default.
- W3201908788 cites W2003527498 @default.
- W3201908788 cites W2003663124 @default.
- W3201908788 cites W2005593574 @default.
- W3201908788 cites W2009851579 @default.
- W3201908788 cites W2011607179 @default.
- W3201908788 cites W2015876559 @default.
- W3201908788 cites W2016904677 @default.
- W3201908788 cites W2016976548 @default.
- W3201908788 cites W2017840788 @default.
- W3201908788 cites W2019578783 @default.
- W3201908788 cites W2019748000 @default.
- W3201908788 cites W2020973699 @default.
- W3201908788 cites W2021300589 @default.
- W3201908788 cites W2024259689 @default.
- W3201908788 cites W2029904324 @default.
- W3201908788 cites W2030661236 @default.
- W3201908788 cites W2033121371 @default.
- W3201908788 cites W2033542443 @default.
- W3201908788 cites W2034397592 @default.
- W3201908788 cites W2034459516 @default.
- W3201908788 cites W2035737599 @default.
- W3201908788 cites W2036484456 @default.
- W3201908788 cites W2037035891 @default.
- W3201908788 cites W2039872199 @default.
- W3201908788 cites W2047938785 @default.
- W3201908788 cites W2059010589 @default.
- W3201908788 cites W2060839143 @default.
- W3201908788 cites W2062011476 @default.
- W3201908788 cites W2067221562 @default.
- W3201908788 cites W2068668821 @default.
- W3201908788 cites W2071156335 @default.
- W3201908788 cites W2071284073 @default.
- W3201908788 cites W2076012598 @default.
- W3201908788 cites W2081673195 @default.
- W3201908788 cites W2085292995 @default.
- W3201908788 cites W2086456118 @default.
- W3201908788 cites W2089507620 @default.
- W3201908788 cites W2094226394 @default.
- W3201908788 cites W2096276260 @default.
- W3201908788 cites W2097103166 @default.
- W3201908788 cites W2102111921 @default.
- W3201908788 cites W2105111360 @default.
- W3201908788 cites W2113810005 @default.
- W3201908788 cites W2114276383 @default.
- W3201908788 cites W2114856901 @default.
- W3201908788 cites W2115518283 @default.
- W3201908788 cites W2116527388 @default.
- W3201908788 cites W2124698750 @default.
- W3201908788 cites W2127250595 @default.
- W3201908788 cites W2132130380 @default.
- W3201908788 cites W2135015385 @default.
- W3201908788 cites W2135183977 @default.
- W3201908788 cites W2135830789 @default.
- W3201908788 cites W2136892820 @default.
- W3201908788 cites W2141391066 @default.
- W3201908788 cites W2145604970 @default.
- W3201908788 cites W2148928597 @default.
- W3201908788 cites W2156744603 @default.
- W3201908788 cites W2161188118 @default.
- W3201908788 cites W2163683674 @default.
- W3201908788 cites W2167359669 @default.
- W3201908788 cites W2172119052 @default.
- W3201908788 cites W2325019720 @default.
- W3201908788 cites W2413903027 @default.
- W3201908788 cites W2474674081 @default.
- W3201908788 cites W2485227959 @default.
- W3201908788 cites W2491281185 @default.
- W3201908788 cites W2515388358 @default.
- W3201908788 cites W2554889271 @default.
- W3201908788 cites W2594221245 @default.
- W3201908788 cites W2658192030 @default.
- W3201908788 cites W2769181414 @default.
- W3201908788 cites W2884572813 @default.
- W3201908788 cites W2912669412 @default.
- W3201908788 cites W2938669072 @default.
- W3201908788 cites W2943726258 @default.