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- W2920807611 abstract "The central Great Xing’an Range contains widespread exposures of Mesozoic igneous rocks, yet the origin of its Late Mesozoic volcanic rocks has long been controversial. They are composed of andesite, trachyte, trachyandesite, trachydacite, rhyolite, and minor basaltic andesite. The intermediate rocks are enriched in large ion lithophiles and light rare earth elements (LILEs and LREEs) and are depleted in high field strength elements (HFSEs) such as Nb, Ta, and Ti, with positive εHf(t) values (+6.2 to +13.4) and Hf single-stage model ages (TDM1 = 556–227 Ma). This indicates that they were derived from the partial melting of a mantle wedge that was modified by previously subducted slab-derived fluids was likely introduced with limited crustal contamination. The felsic rocks show positive εHf(t) values (+4.3 to +10.2) and Hf two-stage model ages (TDM2 = 910–544 Ma), with more enrichment of LILEs and LREEs and more depletion of HFSEs and negative Eu anomalies. This indicates that felsic rocks were mainly derived from partial melting of Neoproterozoic accreted quartz-amphibolite facies mafic crust. We summarise the geochronological and Hf-Nd isotope data for Mesozoic igneous rocks within the central Great Xing’an Range (CGXR), the northern Xing’an block (NXB), and the Erguna block (EB), with the aim of constraining the geochronological framework for Mesozoic volcanism and comparing the growth of continental crust. The evolution of Late Mesozoic magmatism in the three areas reached its climax ~125 Ma ago. Our data, together with regional isotope evidence, suggest that crustal accretion of the CGXR occurred during the Neoproterozoic–Phanerozoic. However, that of the EB occurred during the Meso- to Neoproterozoic. The EB exhibits more lateral and vertical heterogeneities and ancient continental crust than the CGXR and NXB in the northern magma source region." @default.
- W2920807611 created "2019-03-22" @default.
- W2920807611 creator A5005344083 @default.
- W2920807611 creator A5055082070 @default.
- W2920807611 creator A5072681445 @default.
- W2920807611 date "2019-03-17" @default.
- W2920807611 modified "2023-10-16" @default.
- W2920807611 title "Geochemistry of Late Mesozoic volcanic rocks in the central Great Xing’an Range, NE China: petrogenesis and crustal growth in comparison with adjacent areas" @default.
- W2920807611 cites W1051026135 @default.
- W2920807611 cites W1104249897 @default.
- W2920807611 cites W1441480832 @default.
- W2920807611 cites W1550913970 @default.
- W2920807611 cites W1578424743 @default.
- W2920807611 cites W1602682606 @default.
- W2920807611 cites W1755439729 @default.
- W2920807611 cites W1815706132 @default.
- W2920807611 cites W1880555926 @default.
- W2920807611 cites W1964909252 @default.
- W2920807611 cites W1966870578 @default.
- W2920807611 cites W1967437614 @default.
- W2920807611 cites W1967827341 @default.
- W2920807611 cites W1968450376 @default.
- W2920807611 cites W1968685730 @default.
- W2920807611 cites W1969859799 @default.
- W2920807611 cites W1970439132 @default.
- W2920807611 cites W1971000065 @default.
- W2920807611 cites W1972337416 @default.
- W2920807611 cites W1974413429 @default.
- W2920807611 cites W1974505893 @default.
- W2920807611 cites W1974795382 @default.
- W2920807611 cites W1975011645 @default.
- W2920807611 cites W1975657796 @default.
- W2920807611 cites W1976304054 @default.
- W2920807611 cites W1977650828 @default.
- W2920807611 cites W1979694545 @default.
- W2920807611 cites W1981207838 @default.
- W2920807611 cites W1982005903 @default.
- W2920807611 cites W1982221118 @default.
- W2920807611 cites W1982277211 @default.
- W2920807611 cites W1982527737 @default.
- W2920807611 cites W1984329251 @default.
- W2920807611 cites W1986955931 @default.
- W2920807611 cites W1986983284 @default.
- W2920807611 cites W1987084495 @default.
- W2920807611 cites W1988317790 @default.
- W2920807611 cites W1988557437 @default.
- W2920807611 cites W1995104720 @default.
- W2920807611 cites W1995527208 @default.
- W2920807611 cites W1995897602 @default.
- W2920807611 cites W1996340995 @default.
- W2920807611 cites W1997142214 @default.
- W2920807611 cites W1997705537 @default.
- W2920807611 cites W1999448338 @default.
- W2920807611 cites W2003311821 @default.
- W2920807611 cites W2003323528 @default.
- W2920807611 cites W2004780523 @default.
- W2920807611 cites W2008057549 @default.
- W2920807611 cites W2011721469 @default.
- W2920807611 cites W2018798695 @default.
- W2920807611 cites W2023621032 @default.
- W2920807611 cites W2025402991 @default.
- W2920807611 cites W2026313871 @default.
- W2920807611 cites W2029497855 @default.
- W2920807611 cites W2029506771 @default.
- W2920807611 cites W2032353260 @default.
- W2920807611 cites W2033127801 @default.
- W2920807611 cites W2034223887 @default.
- W2920807611 cites W2034428765 @default.
- W2920807611 cites W2035003573 @default.
- W2920807611 cites W2035056660 @default.
- W2920807611 cites W2035347372 @default.
- W2920807611 cites W2036227241 @default.
- W2920807611 cites W2036274526 @default.
- W2920807611 cites W2036642627 @default.
- W2920807611 cites W2038677898 @default.
- W2920807611 cites W2038768328 @default.
- W2920807611 cites W2039085222 @default.
- W2920807611 cites W2039291242 @default.
- W2920807611 cites W2039405518 @default.
- W2920807611 cites W2040908727 @default.
- W2920807611 cites W2042878180 @default.
- W2920807611 cites W2044394940 @default.
- W2920807611 cites W2048084357 @default.
- W2920807611 cites W2050360542 @default.
- W2920807611 cites W2051164400 @default.
- W2920807611 cites W2053291957 @default.
- W2920807611 cites W2054295913 @default.
- W2920807611 cites W2054366973 @default.
- W2920807611 cites W2054590577 @default.
- W2920807611 cites W2054765896 @default.
- W2920807611 cites W2055112659 @default.
- W2920807611 cites W2056792227 @default.
- W2920807611 cites W2057876276 @default.
- W2920807611 cites W2059027044 @default.
- W2920807611 cites W2061010525 @default.
- W2920807611 cites W2061962408 @default.
- W2920807611 cites W2062052372 @default.
- W2920807611 cites W2070070314 @default.