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• W2536692826 abstract "The geodynamic setting of Late Triassic magmatic activity along the Longmu Co–Shuanghu suture zone (LSSZ) in central Qiangtang, Tibet is a matter of debate. This paper presents zircon LA–ICP–MS U–Pb ages, zircon Hf isotopic compositions, and whole-rock geochemical data for the Sangehu (SGH) granitic intrusion in central Qiangtang, and addresses the petrogenesis of Late Triassic magmatism, and the history of collision between the northern and southern Qiangtang terranes. The SGH pluton consists mainly of biotite adamellite with mafic microgranular enclaves (MMEs), and small amounts of K-feldspar granite. The biotite adamellite, MMEs, and K-feldspar granite give ages of 207.8 ± 3.0 Ma, 212.4 ± 31 Ma, and 211.6 ± 3.8 Ma, respectively. The MMEs show magmatic textures and acicular apatite, and are coeval with the host biotite adamellite, suggesting they were produced by magma mixing. All samples from the SGH pluton show high Sr and low Y contents, and positive Eu anomalies, similar to adakitic rocks. The high K2O contents and low Mg#, Cr, and Ni contents, and enriched Hf isotopic characteristics of the zircons indicate that these magmas were derived from the partial melting of thickened crust. However, the whole-rock geochemical data and zircon Hf isotopic compositions also reveal heterogeneity at the source. The combined magmatic and metamorphic records suggest that Triassic magmatic activity in central Qiangtang was closely related to the collision of the northern and southern Qiangtang terranes. The large-scale Late Triassic (225–200 Ma) magmatic event in central Qiangtang may have resulted from the breakoff of the Longmu Co–Shuanghu Tethys Ocean lithospheric slab in the early Late Triassic (236–230 Ma). The Late Triassic magmatic rocks, including adakitic rocks, are coeval with retrograde high-pressure (HP) to ultrahigh-pressure (UHP) metamorphic rocks in central Qiangtang, and show characteristics of syn-exhumation magmatism. The early adakitic rocks (>220 Ma) were generated by melting of the edge of the slab, which was heated by upwelling asthenospheric mantle after subduction slab breakoff, and the late adakitic rocks (<220 Ma) were generated by partial melting of the thickened crust." @default.
• W2536692826 created "2016-10-28" @default.
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• W2536692826 date "2016-12-01" @default.
• W2536692826 modified "2023-09-27" @default.
• W2536692826 title "Late Triassic syn-exhumation magmatism in central Qiangtang, Tibet: Evidence from the Sangehu adakitic rocks" @default.
• W2536692826 cites W1871734886 @default.
• W2536692826 cites W1967082613 @default.
• W2536692826 cites W1968538171 @default.
• W2536692826 cites W1969080760 @default.
• W2536692826 cites W1970595625 @default.
• W2536692826 cites W1971765285 @default.
• W2536692826 cites W1973219404 @default.
• W2536692826 cites W1978676610 @default.
• W2536692826 cites W1979705656 @default.
• W2536692826 cites W1979828445 @default.
• W2536692826 cites W1981207838 @default.
• W2536692826 cites W1982589593 @default.
• W2536692826 cites W1984799420 @default.
• W2536692826 cites W1986038871 @default.
• W2536692826 cites W1988215475 @default.
• W2536692826 cites W1988697677 @default.
• W2536692826 cites W1992860423 @default.
• W2536692826 cites W1995137849 @default.
• W2536692826 cites W1995555849 @default.
• W2536692826 cites W1997816021 @default.
• W2536692826 cites W2000249710 @default.
• W2536692826 cites W2002518560 @default.
• W2536692826 cites W2002974459 @default.
• W2536692826 cites W2003564352 @default.
• W2536692826 cites W2004780129 @default.
• W2536692826 cites W2013143414 @default.
• W2536692826 cites W2018376581 @default.
• W2536692826 cites W2019167641 @default.
• W2536692826 cites W2020152301 @default.
• W2536692826 cites W2023985047 @default.
• W2536692826 cites W2031663670 @default.
• W2536692826 cites W2032464438 @default.
• W2536692826 cites W2038748953 @default.
• W2536692826 cites W2038775297 @default.
• W2536692826 cites W2039872199 @default.
• W2536692826 cites W2040029696 @default.
• W2536692826 cites W2041837766 @default.
• W2536692826 cites W2044921168 @default.
• W2536692826 cites W2045538797 @default.
• W2536692826 cites W2045716957 @default.
• W2536692826 cites W2047634242 @default.
• W2536692826 cites W2047813963 @default.
• W2536692826 cites W2049612708 @default.
• W2536692826 cites W2051273227 @default.
• W2536692826 cites W2052579497 @default.
• W2536692826 cites W2055373009 @default.
• W2536692826 cites W2055736194 @default.
• W2536692826 cites W2059250966 @default.
• W2536692826 cites W2063030220 @default.
• W2536692826 cites W2080261231 @default.
• W2536692826 cites W2081673195 @default.
• W2536692826 cites W2083623123 @default.
• W2536692826 cites W2088298798 @default.
• W2536692826 cites W2088363446 @default.
• W2536692826 cites W2089129393 @default.
• W2536692826 cites W2090206242 @default.
• W2536692826 cites W2090446100 @default.
• W2536692826 cites W2091441425 @default.
• W2536692826 cites W2093369526 @default.
• W2536692826 cites W2102081901 @default.
• W2536692826 cites W2102534991 @default.
• W2536692826 cites W2102973797 @default.
• W2536692826 cites W2107790246 @default.
• W2536692826 cites W2113941003 @default.
• W2536692826 cites W2114856577 @default.
• W2536692826 cites W2126229897 @default.
• W2536692826 cites W2128624170 @default.
• W2536692826 cites W2130845410 @default.
• W2536692826 cites W2132513592 @default.
• W2536692826 cites W2138522501 @default.
• W2536692826 cites W2140093647 @default.
• W2536692826 cites W2144081161 @default.
• W2536692826 cites W2146943491 @default.
• W2536692826 cites W2159104880 @default.
• W2536692826 cites W2162577614 @default.
• W2536692826 cites W2164911500 @default.
• W2536692826 cites W2167856052 @default.
• W2536692826 cites W2312984247 @default.
• W2536692826 cites W2322013406 @default.
• W2536692826 cites W2328718358 @default.
• W2536692826 cites W62146380 @default.
• W2536692826 doi "https://doi.org/10.1016/j.jseaes.2016.10.009" @default.
• W2536692826 hasPublicationYear "2016" @default.
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