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- W3208920009 endingPage "104978" @default.
- W3208920009 startingPage "104978" @default.
- W3208920009 abstract "To unravel when, where, and how multiple arc systems were amalgamated is crucial for understanding the accretion processes of the Central Asian Orogenic Belt. Here we focus on the collision of the Siberian margin and the Kazakhstan collage along the Char Shear/Suture Zone in eastern Kazakhstan. We conducted U–Pb dating and Hf isotope analysis for detrital zircons of clastic rocks across the collisional zone of the Siberian margin (the Irtysh-Zaisan Complex) and the Kazakhstan collage (the Zharma-Saur Arc and the Char Zone). Our results show that the Irtysh-Zaisan Complex carries abundant early Paleozoic detrital zircons and minor Precambrian zircons, but there is a lack of such zircon populations in the Zharma-Saur Arc and the Char Zone. Devonian to Carboniferous detrital zircons appear in all sampling tectonic units, in which εHf(t) values of Carboniferous zircons from the Zharma-Saur Arc and the Char Zone are characterized by a narrow range (∼10–17) that is different from a relatively wider range of εHf(t) values of ∼5–18 for the Carboniferous zircons in the Irtysh-Zaisan Complex. The distinct sedimentary provenances of the Irtysh-Zaisan Complex and the Zharma-Saur Arc/Char Zone confirm that their tectonic boundary lies along the Char Shear Zone in eastern Kazakhstan. As the Late Carboniferous sedimentary rocks from the Zharma-Saur Arc and the Char Zone do not receive detritus from the Siberian margin, we consider that the Ob-Zaisan Ocean between the Siberian margin and the Kazakhstan collage was closed later than the deposition of these sedimentary rocks (<321 Ma)." @default.
- W3208920009 created "2021-11-08" @default.
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- W3208920009 creator A5068285146 @default.
- W3208920009 creator A5077566641 @default.
- W3208920009 creator A5088305376 @default.
- W3208920009 date "2022-07-01" @default.
- W3208920009 modified "2023-10-16" @default.
- W3208920009 title "Provenance of late Paleozoic sedimentary rocks in eastern Kazakhstan: Implications for the collision of the Siberian margin with the Kazakhstan collage" @default.
- W3208920009 cites W1480328088 @default.
- W3208920009 cites W1504724337 @default.
- W3208920009 cites W1518712899 @default.
- W3208920009 cites W1534101527 @default.
- W3208920009 cites W1650609279 @default.
- W3208920009 cites W1752342224 @default.
- W3208920009 cites W1837189634 @default.
- W3208920009 cites W1964276781 @default.
- W3208920009 cites W1964724263 @default.
- W3208920009 cites W1966541379 @default.
- W3208920009 cites W1969805407 @default.
- W3208920009 cites W1971856782 @default.
- W3208920009 cites W1977722167 @default.
- W3208920009 cites W1977875524 @default.
- W3208920009 cites W1982107830 @default.
- W3208920009 cites W1983054136 @default.
- W3208920009 cites W1983229146 @default.
- W3208920009 cites W1985956286 @default.
- W3208920009 cites W1994452969 @default.
- W3208920009 cites W1994561360 @default.
- W3208920009 cites W1995881565 @default.
- W3208920009 cites W1995924407 @default.
- W3208920009 cites W1998773567 @default.
- W3208920009 cites W1999623014 @default.
- W3208920009 cites W2000469042 @default.
- W3208920009 cites W2001552374 @default.
- W3208920009 cites W2001847912 @default.
- W3208920009 cites W2003323528 @default.
- W3208920009 cites W2004725253 @default.
- W3208920009 cites W2008290469 @default.
- W3208920009 cites W2010233366 @default.
- W3208920009 cites W2016216561 @default.
- W3208920009 cites W2016536555 @default.
- W3208920009 cites W2018960606 @default.
- W3208920009 cites W2019695435 @default.
- W3208920009 cites W2026287564 @default.
- W3208920009 cites W2027857855 @default.
- W3208920009 cites W2030057637 @default.
- W3208920009 cites W2034223887 @default.
- W3208920009 cites W2037498963 @default.
- W3208920009 cites W2039382632 @default.
- W3208920009 cites W2040963788 @default.
- W3208920009 cites W2043021600 @default.
- W3208920009 cites W2043844425 @default.
- W3208920009 cites W2044934678 @default.
- W3208920009 cites W2046220982 @default.
- W3208920009 cites W2047807381 @default.
- W3208920009 cites W2051273227 @default.
- W3208920009 cites W2054590577 @default.
- W3208920009 cites W2059324292 @default.
- W3208920009 cites W2061188678 @default.
- W3208920009 cites W2063157630 @default.
- W3208920009 cites W2063734888 @default.
- W3208920009 cites W2063964861 @default.
- W3208920009 cites W2066683906 @default.
- W3208920009 cites W2070070314 @default.
- W3208920009 cites W2070384449 @default.
- W3208920009 cites W2071686569 @default.
- W3208920009 cites W2071990661 @default.
- W3208920009 cites W2077653929 @default.
- W3208920009 cites W2079767098 @default.
- W3208920009 cites W2083354817 @default.
- W3208920009 cites W2089096123 @default.
- W3208920009 cites W2090206242 @default.
- W3208920009 cites W2090613745 @default.
- W3208920009 cites W2099932450 @default.
- W3208920009 cites W2107500918 @default.
- W3208920009 cites W2113634862 @default.
- W3208920009 cites W2127456773 @default.
- W3208920009 cites W2133042542 @default.
- W3208920009 cites W2134721808 @default.
- W3208920009 cites W2135384477 @default.
- W3208920009 cites W2141951312 @default.
- W3208920009 cites W2154954711 @default.
- W3208920009 cites W2162334444 @default.
- W3208920009 cites W2164555910 @default.
- W3208920009 cites W2169016685 @default.
- W3208920009 cites W2169766597 @default.
- W3208920009 cites W2169769753 @default.
- W3208920009 cites W2171086159 @default.
- W3208920009 cites W2192132413 @default.
- W3208920009 cites W2318010774 @default.
- W3208920009 cites W2395292659 @default.
- W3208920009 cites W2441695414 @default.
- W3208920009 cites W2548546070 @default.
- W3208920009 cites W2562357877 @default.