FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2056792227> ?p ?o ?g. }

• W2056792227 endingPage "423" @default.
• W2056792227 startingPage "406" @default.
• W2056792227 abstract "This paper reports new zircon LA–ICP–MS and SIMS U–Pb ages and Hf isotope data, and whole-rock major and trace element data for Late Triassic igneous rocks of eastern Heilongjiang Province, NE China. These data provide new insights into the timing of the initiation of subduction of the Paleo-Pacific Plate beneath the Eurasian continent. The zircon U–Pb age data indicate that a suite of Late Triassic (228–202 Ma) igneous rocks is present within the Songnen–Zhangguangcai Range Massif and within the western margin of the Khanka Massif. The Late Triassic igneous rocks within the Songnen–Zhangguangcai Range Massif consist of basalts, basaltic andesites, gabbro-diabases, and rhyolites, whereas coeval igneous rocks in the western margin of the Khanka Massif consist of hornblende gabbros and syenogranitic porphyries. These Late Triassic rocks constitute a geochemically bimodal igneous rock association that contains mafic rocks enriched in light rare earth elements (LREE) and large ion lithophile elements (LILE), and depleted in heavy rare earth elements (HREE) and high field strength elements (HFSE) such as Nb, Ta, Zr, Hf, and Ti. Zircons from these mafic rocks have εHf (t) values and TDM1 ages of +2.8 to +9.8 and 477–733 Ma, respectively, suggesting that they formed from a primary magma generated by the partial melting of depleted lithospheric mantle material that had been previously modified by subduction-related fluids. The coeval felsic rocks are characterized by enrichments in LREEs and LILEs, and depletions in HREEs and HFSEs (including Nb, Ta, and Ti), and their zircons have εHf (t) values and TDM2 ages of +0.6 to +7.9 and 766 to 1461 Ma, respectively, implying that these rocks were generated during the partial melting of juvenile crustal material. The Late Triassic bimodal igneous rocks in eastern Heilongjiang Province, combined with the regional geologic information, therefore record a post-orogenic extensional environment related to the final late Permian–Early Triassic closure of the Paleo-Asian Ocean. In addition, the presence of Late Triassic bimodal igneous rocks within the eastern margin of the Eurasian continent suggests that the subduction of the Paleo-Pacific Plate beneath the Eurasian continent began after the Late Triassic." @default.
• W2056792227 created "2016-06-24" @default.
• W2056792227 creator A5028473324 @default.
• W2056792227 creator A5074719379 @default.
• W2056792227 creator A5081554342 @default.
• W2056792227 creator A5085843802 @default.
• W2056792227 creator A5087127338 @default.
• W2056792227 date "2015-01-01" @default.
• W2056792227 modified "2023-10-16" @default.
• W2056792227 title "Late Triassic bimodal igneous rocks in eastern Heilongjiang Province, NE China: Implications for the initiation of subduction of the Paleo-Pacific Plate beneath Eurasia" @default.
• W2056792227 cites W1608302839 @default.
• W2056792227 cites W1964038242 @default.
• W2056792227 cites W1965835831 @default.
• W2056792227 cites W1965917434 @default.
• W2056792227 cites W1967827341 @default.
• W2056792227 cites W1970439132 @default.
• W2056792227 cites W1971685925 @default.
• W2056792227 cites W1972256629 @default.
• W2056792227 cites W1973165172 @default.
• W2056792227 cites W1973502650 @default.
• W2056792227 cites W1974600815 @default.
• W2056792227 cites W1974907985 @default.
• W2056792227 cites W1980640006 @default.
• W2056792227 cites W1983264858 @default.
• W2056792227 cites W1984329251 @default.
• W2056792227 cites W1986560096 @default.
• W2056792227 cites W1988317790 @default.
• W2056792227 cites W1991323502 @default.
• W2056792227 cites W1995698047 @default.
• W2056792227 cites W1995897602 @default.
• W2056792227 cites W1999448338 @default.
• W2056792227 cites W2003348019 @default.
• W2056792227 cites W2004072968 @default.
• W2056792227 cites W2007414840 @default.
• W2056792227 cites W2008264819 @default.
• W2056792227 cites W2014935809 @default.
• W2056792227 cites W2021987309 @default.
• W2056792227 cites W2022859730 @default.
• W2056792227 cites W2025402991 @default.
• W2056792227 cites W2032006288 @default.
• W2056792227 cites W2034250421 @default.
• W2056792227 cites W2035347372 @default.
• W2056792227 cites W2035595872 @default.
• W2056792227 cites W2040676068 @default.
• W2056792227 cites W2043063526 @default.
• W2056792227 cites W2044911516 @default.
• W2056792227 cites W2045345459 @default.
• W2056792227 cites W2047364329 @default.
• W2056792227 cites W2053514714 @default.
• W2056792227 cites W2053587074 @default.
• W2056792227 cites W2054624167 @default.
• W2056792227 cites W2059211005 @default.
• W2056792227 cites W2060089581 @default.
• W2056792227 cites W2063976160 @default.
• W2056792227 cites W2064527735 @default.
• W2056792227 cites W2066651036 @default.
• W2056792227 cites W2072680255 @default.
• W2056792227 cites W2074114517 @default.
• W2056792227 cites W2077568244 @default.
• W2056792227 cites W2081673195 @default.
• W2056792227 cites W2083355627 @default.
• W2056792227 cites W2086014962 @default.
• W2056792227 cites W2087662765 @default.
• W2056792227 cites W2089096123 @default.
• W2056792227 cites W2090780260 @default.
• W2056792227 cites W2095229570 @default.
• W2056792227 cites W2097502986 @default.
• W2056792227 cites W2103463307 @default.
• W2056792227 cites W2117217018 @default.
• W2056792227 cites W2119438235 @default.
• W2056792227 cites W2123985829 @default.
• W2056792227 cites W2126127241 @default.
• W2056792227 cites W2130869872 @default.
• W2056792227 cites W2133042542 @default.
• W2056792227 cites W2140093647 @default.
• W2056792227 cites W2145191782 @default.
• W2056792227 cites W2147682788 @default.
• W2056792227 cites W2325019720 @default.
• W2056792227 cites W2387920496 @default.
• W2056792227 cites W2897983685 @default.
• W2056792227 doi "https://doi.org/10.1016/j.jseaes.2014.05.025" @default.
• W2056792227 hasPublicationYear "2015" @default.
• W2056792227 type Work @default.
• W2056792227 sameAs 2056792227 @default.
• W2056792227 citedByCount "108" @default.
• W2056792227 countsByYear W20567922272015 @default.
• W2056792227 countsByYear W20567922272016 @default.
• W2056792227 countsByYear W20567922272017 @default.
• W2056792227 countsByYear W20567922272018 @default.
• W2056792227 countsByYear W20567922272019 @default.
• W2056792227 countsByYear W20567922272020 @default.
• W2056792227 countsByYear W20567922272021 @default.
• W2056792227 countsByYear W20567922272022 @default.
• W2056792227 countsByYear W20567922272023 @default.
• W2056792227 crossrefType "journal-article" @default.
• W2056792227 hasAuthorship W2056792227A5028473324 @default.
• W2056792227 hasAuthorship W2056792227A5074719379 @default.
• W2056792227 hasAuthorship W2056792227A5081554342 @default.

• next