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- W3170702861 abstract "Abstract The nature and source of magmatism associated with large igneous provinces (LIPs) remain disputed. Here we investigate the role of recycled materials that contributed to mantle heterogeneity in the Tarim Large Igneous Province (TLIP) in China through integrated Zn–Mg–Sr–Nd isotopes of a rare tephritic rock suite. The Sr–Nd isotopes [(87Sr/86Sr)i = 0.70368–0.70629; εNd(t) = −0.25–4.64] and δ26Mg values (−0.23‰ to −0.34‰) of the tephritic porphyries are consistent with a normal mantle origin. In contrast, the whole rock and pyroxene phenocrysts yield δ66Zn values of +0.28‰ to +0.46‰ and +0.30‰ to +0.39‰, which are slightly heavier than those of the terrestrial mantle (+0.16 ± 0.06‰) and mid-oceanic-ridge basalts (MORBs) (+0.27 ± 0.05‰). We exclude the possibility that the heavy Zn isotopes of the Wajilitag tephritic porphyries are caused by magmatic processes such as fractional crystallization and partial melting and correlate the isotopic features to the role of altered oceanic crust along with magnesite in the mantle source. The Wajilitag tephritic porphyry displays trace-element patterns similar to those of the melts from natural hornblendite, especially those of hornblendite + peridotite. Additionally, the geochemical characteristics such as enrichment in Nb and Ta, depletion in K, high TiO2, and constant Na2O/K2O ratios also suggest that the tephritic porphyries were derived from an amphibole-bearing source contributed by altered oceanic crust along with sedimentary carbonates. Our study provides insight into the contribution of subducted materials to the mantle heterogeneity beneath the TLIP and highlights the role of subduction in the deep carbon cycle and subducted slab-lithosphere-plume interaction in the generation of LIPs." @default.
- W3170702861 created "2021-06-22" @default.
- W3170702861 creator A5000573728 @default.
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- W3170702861 date "2021-06-15" @default.
- W3170702861 modified "2023-09-29" @default.
- W3170702861 title "Mantle source of tephritic porphyry in the Tarim Large Igneous Province constrained from Mg, Zn, Sr, and Nd isotope systematics: Implications for deep carbon cycling" @default.
- W3170702861 cites W1528158128 @default.
- W3170702861 cites W1578122124 @default.
- W3170702861 cites W1853219909 @default.
- W3170702861 cites W1965439550 @default.
- W3170702861 cites W1970758245 @default.
- W3170702861 cites W1977410051 @default.
- W3170702861 cites W1979999752 @default.
- W3170702861 cites W1981602009 @default.
- W3170702861 cites W1984264698 @default.
- W3170702861 cites W1990619959 @default.
- W3170702861 cites W1993661498 @default.
- W3170702861 cites W1994380392 @default.
- W3170702861 cites W2001030594 @default.
- W3170702861 cites W2003446684 @default.
- W3170702861 cites W2003948785 @default.
- W3170702861 cites W2005195754 @default.
- W3170702861 cites W2005682964 @default.
- W3170702861 cites W2008782416 @default.
- W3170702861 cites W2014814915 @default.
- W3170702861 cites W2015207803 @default.
- W3170702861 cites W2026455415 @default.
- W3170702861 cites W2031894158 @default.
- W3170702861 cites W2034673247 @default.
- W3170702861 cites W2038979071 @default.
- W3170702861 cites W2040473333 @default.
- W3170702861 cites W2042423268 @default.
- W3170702861 cites W2042537339 @default.
- W3170702861 cites W2043466950 @default.
- W3170702861 cites W2044309397 @default.
- W3170702861 cites W2045092985 @default.
- W3170702861 cites W2047197891 @default.
- W3170702861 cites W2050582708 @default.
- W3170702861 cites W2051060113 @default.
- W3170702861 cites W2052473341 @default.
- W3170702861 cites W2063948740 @default.
- W3170702861 cites W2066028168 @default.
- W3170702861 cites W2066735401 @default.
- W3170702861 cites W2082667528 @default.
- W3170702861 cites W2086769098 @default.
- W3170702861 cites W2089425747 @default.
- W3170702861 cites W2091065826 @default.
- W3170702861 cites W2091154424 @default.
- W3170702861 cites W2100252388 @default.
- W3170702861 cites W2105089162 @default.
- W3170702861 cites W2109622426 @default.
- W3170702861 cites W2113840820 @default.
- W3170702861 cites W2119330075 @default.
- W3170702861 cites W2121755657 @default.
- W3170702861 cites W2125654971 @default.
- W3170702861 cites W2127568053 @default.
- W3170702861 cites W2128673582 @default.
- W3170702861 cites W2133103627 @default.
- W3170702861 cites W2137126784 @default.
- W3170702861 cites W2138522501 @default.
- W3170702861 cites W2146117929 @default.
- W3170702861 cites W2147283649 @default.
- W3170702861 cites W2147703958 @default.
- W3170702861 cites W2148501813 @default.
- W3170702861 cites W2152384549 @default.
- W3170702861 cites W2152967648 @default.
- W3170702861 cites W2154699907 @default.
- W3170702861 cites W2161759270 @default.
- W3170702861 cites W2167782460 @default.
- W3170702861 cites W2171801505 @default.
- W3170702861 cites W2218148394 @default.
- W3170702861 cites W2336365893 @default.
- W3170702861 cites W2376402588 @default.
- W3170702861 cites W2403973578 @default.
- W3170702861 cites W2419075829 @default.
- W3170702861 cites W2467245281 @default.
- W3170702861 cites W2478962634 @default.
- W3170702861 cites W2527002221 @default.
- W3170702861 cites W2555955218 @default.
- W3170702861 cites W2556678425 @default.
- W3170702861 cites W2571129369 @default.
- W3170702861 cites W2585007529 @default.
- W3170702861 cites W2588613439 @default.
- W3170702861 cites W2594095801 @default.
- W3170702861 cites W2602434750 @default.
- W3170702861 cites W2737628941 @default.
- W3170702861 cites W2772963007 @default.
- W3170702861 cites W2791006370 @default.
- W3170702861 cites W2806285718 @default.
- W3170702861 cites W2863985156 @default.