FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2074557768> ?p ?o ?g. }

• W2074557768 endingPage "405" @default.
• W2074557768 startingPage "393" @default.
• W2074557768 abstract "Mesozoic granitic rocks are widely distributed in northeast (NE) China. However, high-Mg dioritic rocks are considerably rare. Here, we report a newly recognized high-Mg diorite (the Xintun diorite) in the Yanji area, NE China, to constrain its origin and implications for the tectonic evolution of eastern Asian continental margin. Zircon U–Pb dating yields a crystallization age of 128 ± 1 Ma for the Xintun diorite. The diorites are characterized by high MgO (4.4–6.6 wt.%), Cr (119–239 ppm), Ba (419–514 ppm) and Sr (649–747 ppm) contents and Mg# values (59–64), but low FeOtotal/MgO ratios (1.2–1.4), with geochemical features similar to those of sanukitic high-Mg andesites (HMAs). They show moderate radiogenic Sr (ISr = 0.7047–0.7050) and Nd (εNd = 0.3–1.1), with high La/Sm ratios, which are indicative of contributions from sediment components. The mineral assemblage of euhedral hornblende, magnetite and titanite, implies a water-rich and oxidized signature for their primitive magmas. These features suggest that the Xintun high-Mg diorites were probably formed via partial melting of the subducting sediments and subsequent interaction of mantle peridotites with both melts and aqueous fluids. Geochemical modeling reveals that hornblende-dominated fractional crystallization under water-sufficient conditions enabled the evolved magmas to acquire adakitic signatures. We believe that the Paleo-Pacific subduction beneath eastern Asian continental margin caused large-scale back-arc extension of NE China in the Early Cretaceous, and, consequently, induced the asthenospheric flow toward the mantle wedge, reheating subducting sediments enough to cause melting. Therefore, the occurrence of the Xintun high-Mg diorites signifies the onset of extensive back-arc extension of eastern Asian continental margin at ca. 128 Ma." @default.
• W2074557768 created "2016-06-24" @default.
• W2074557768 creator A5029686496 @default.
• W2074557768 creator A5034655117 @default.
• W2074557768 creator A5035484659 @default.
• W2074557768 creator A5047642108 @default.
• W2074557768 date "2015-01-01" @default.
• W2074557768 modified "2023-10-01" @default.
• W2074557768 title "Early Cretaceous high-Mg diorites in the Yanji area, northeastern China: Petrogenesis and tectonic implications" @default.
• W2074557768 cites W1587780337 @default.
• W2074557768 cites W1697907569 @default.
• W2074557768 cites W1964047299 @default.
• W2074557768 cites W1967082613 @default.
• W2074557768 cites W1967827341 @default.
• W2074557768 cites W1969371403 @default.
• W2074557768 cites W1970439132 @default.
• W2074557768 cites W1977638370 @default.
• W2074557768 cites W1979705656 @default.
• W2074557768 cites W1988317790 @default.
• W2074557768 cites W1990672888 @default.
• W2074557768 cites W1990701109 @default.
• W2074557768 cites W1991589759 @default.
• W2074557768 cites W2000713509 @default.
• W2074557768 cites W2000795509 @default.
• W2074557768 cites W2003323528 @default.
• W2074557768 cites W2003328691 @default.
• W2074557768 cites W2006510222 @default.
• W2074557768 cites W2008456126 @default.
• W2074557768 cites W2011721469 @default.
• W2074557768 cites W2013378824 @default.
• W2074557768 cites W2013639409 @default.
• W2074557768 cites W2014935809 @default.
• W2074557768 cites W2020973699 @default.
• W2074557768 cites W2022859730 @default.
• W2074557768 cites W2024321144 @default.
• W2074557768 cites W2025402991 @default.
• W2074557768 cites W2026722663 @default.
• W2074557768 cites W2031306284 @default.
• W2074557768 cites W2034577561 @default.
• W2074557768 cites W2035670944 @default.
• W2074557768 cites W2039085222 @default.
• W2074557768 cites W2039405518 @default.
• W2074557768 cites W2042266298 @default.
• W2074557768 cites W2043694977 @default.
• W2074557768 cites W2044609027 @default.
• W2074557768 cites W2044921168 @default.
• W2074557768 cites W2045345459 @default.
• W2074557768 cites W2049710327 @default.
• W2074557768 cites W2049907150 @default.
• W2074557768 cites W2053721096 @default.
• W2074557768 cites W2057550910 @default.
• W2074557768 cites W2061010525 @default.
• W2074557768 cites W2064839818 @default.
• W2074557768 cites W2067420036 @default.
• W2074557768 cites W2070854336 @default.
• W2074557768 cites W2072075526 @default.
• W2074557768 cites W2073971513 @default.
• W2074557768 cites W2077291658 @default.
• W2074557768 cites W2078011306 @default.
• W2074557768 cites W2078816109 @default.
• W2074557768 cites W2086815595 @default.
• W2074557768 cites W2087292109 @default.
• W2074557768 cites W2090563556 @default.
• W2074557768 cites W2094985587 @default.
• W2074557768 cites W2100966007 @default.
• W2074557768 cites W2130869872 @default.
• W2074557768 cites W2136162288 @default.
• W2074557768 cites W2144222955 @default.
• W2074557768 cites W2149787537 @default.
• W2074557768 cites W2167313938 @default.
• W2074557768 cites W2169766597 @default.
• W2074557768 cites W2314670496 @default.
• W2074557768 cites W2320888785 @default.
• W2074557768 cites W2332345147 @default.
• W2074557768 cites W2897983685 @default.
• W2074557768 cites W37262398 @default.
• W2074557768 doi "https://doi.org/10.1016/j.jseaes.2014.07.010" @default.
• W2074557768 hasPublicationYear "2015" @default.
• W2074557768 type Work @default.
• W2074557768 sameAs 2074557768 @default.
• W2074557768 citedByCount "27" @default.
• W2074557768 countsByYear W20745577682015 @default.
• W2074557768 countsByYear W20745577682016 @default.
• W2074557768 countsByYear W20745577682017 @default.
• W2074557768 countsByYear W20745577682018 @default.
• W2074557768 countsByYear W20745577682019 @default.
• W2074557768 countsByYear W20745577682020 @default.
• W2074557768 countsByYear W20745577682021 @default.
• W2074557768 countsByYear W20745577682022 @default.
• W2074557768 countsByYear W20745577682023 @default.
• W2074557768 crossrefType "journal-article" @default.
• W2074557768 hasAuthorship W2074557768A5029686496 @default.
• W2074557768 hasAuthorship W2074557768A5034655117 @default.
• W2074557768 hasAuthorship W2074557768A5035484659 @default.
• W2074557768 hasAuthorship W2074557768A5047642108 @default.
• W2074557768 hasConcept C11872896 @default.
• W2074557768 hasConcept C120806208 @default.
• W2074557768 hasConcept C127313418 @default.

• next