FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2074041872> ?p ?o ?g. }

• W2074041872 endingPage "54" @default.
• W2074041872 startingPage "41" @default.
• W2074041872 abstract "The Tongbai–Dabie–Sulu orogen contains several eclogite-bearing terranes that were largely metamorphosed in Triassic time. Although petrologic and geochronologic data from these terranes have provided essential information on the geodynamic history of the orogenic cycle, the timing of onset of continental collision between Sino–Korean craton and the Yangtze craton is still unknown. To better our understanding of the transitional time of oceanic to continental subduction in this orogen, we have dated an eclogite with continental affinity in the Tongbai Mountains, located in the very west part of the Tongbai–Dabie–Sulu orogen, central China, using Lu–Hf geochronology. These eclogites formed at pressure temperature conditions of 1.8–2.1 GPa and 490–540 °C. Mineral–whole rock ages of multi-garnet fractions from three localities yield Lu–Hf ages of 256.4 ± 2.6 Ma, 252.3 ± 3.4 Ma and 246.9 ± 3.2 Ma. Garnet porphyroblasts from the three samples display evidence of prograde zoning but the major portion of the garnet grains grew exclusively at eclogite-facies conditions due to the occurrence of omphacite inclusions from core to rim. Taking the spherical geometry effect into account, these Lu–Hf ages are, therefore, interpreted to reflect high-pressure eclogite-facies metamorphism instead of the early phase of garnet growth despite the well-preserved prograde major- and trace-element zoning in garnets. Our results allow for a more detailed and complete picture of the tectonic evolution of the Tongbai–Dabie–Sulu orogen during the transitional time of oceanic to continental subduction. These new Lu–Hf ages mark the timing of onset of continental collision between Sino–Korean craton and the Yangtze craton, suggesting that the entry of the leading edge of the Yangtze craton continent into the Sino–Korean craton trench occurred no later than ca. 256 Ma." @default.
• W2074041872 created "2016-06-24" @default.
• W2074041872 creator A5007024896 @default.
• W2074041872 creator A5018968425 @default.
• W2074041872 creator A5024046512 @default.
• W2074041872 creator A5032782015 @default.
• W2074041872 creator A5038855167 @default.
• W2074041872 creator A5070546467 @default.
• W2074041872 creator A5075087804 @default.
• W2074041872 date "2011-01-01" @default.
• W2074041872 modified "2023-10-18" @default.
• W2074041872 title "New Lu–Hf geochronology constrains the onset of continental subduction in the Dabie orogen" @default.
• W2074041872 cites W1522860430 @default.
• W2074041872 cites W1587965322 @default.
• W2074041872 cites W1830358639 @default.
• W2074041872 cites W1837373594 @default.
• W2074041872 cites W1871734886 @default.
• W2074041872 cites W1950684065 @default.
• W2074041872 cites W1957793219 @default.
• W2074041872 cites W1965672065 @default.
• W2074041872 cites W1977595825 @default.
• W2074041872 cites W1978317343 @default.
• W2074041872 cites W1980155029 @default.
• W2074041872 cites W1980173354 @default.
• W2074041872 cites W1985048272 @default.
• W2074041872 cites W1985745494 @default.
• W2074041872 cites W1990742678 @default.
• W2074041872 cites W1992211265 @default.
• W2074041872 cites W1995119550 @default.
• W2074041872 cites W1997416903 @default.
• W2074041872 cites W2020139762 @default.
• W2074041872 cites W2021345743 @default.
• W2074041872 cites W2028330480 @default.
• W2074041872 cites W2028642961 @default.
• W2074041872 cites W2029243975 @default.
• W2074041872 cites W2034283772 @default.
• W2074041872 cites W2038516566 @default.
• W2074041872 cites W2042945599 @default.
• W2074041872 cites W2046239832 @default.
• W2074041872 cites W2048261322 @default.
• W2074041872 cites W2048857036 @default.
• W2074041872 cites W2049191257 @default.
• W2074041872 cites W2053381713 @default.
• W2074041872 cites W2053422899 @default.
• W2074041872 cites W2054312647 @default.
• W2074041872 cites W2058534321 @default.
• W2074041872 cites W2059013108 @default.
• W2074041872 cites W2062706977 @default.
• W2074041872 cites W2062780038 @default.
• W2074041872 cites W2066857758 @default.
• W2074041872 cites W2069141764 @default.
• W2074041872 cites W2070952980 @default.
• W2074041872 cites W2071917865 @default.
• W2074041872 cites W2073326270 @default.
• W2074041872 cites W2074716667 @default.
• W2074041872 cites W2078840355 @default.
• W2074041872 cites W2080325016 @default.
• W2074041872 cites W2080993999 @default.
• W2074041872 cites W2083841543 @default.
• W2074041872 cites W2083871626 @default.
• W2074041872 cites W2089832041 @default.
• W2074041872 cites W2100618503 @default.
• W2074041872 cites W2117933282 @default.
• W2074041872 cites W2118079032 @default.
• W2074041872 cites W2125270986 @default.
• W2074041872 cites W2126728479 @default.
• W2074041872 cites W2129379220 @default.
• W2074041872 cites W2131435321 @default.
• W2074041872 cites W2133042542 @default.
• W2074041872 cites W2138522501 @default.
• W2074041872 cites W2141890535 @default.
• W2074041872 cites W2155100807 @default.
• W2074041872 cites W2155773363 @default.
• W2074041872 cites W2160614281 @default.
• W2074041872 cites W2162094172 @default.
• W2074041872 cites W2163462779 @default.
• W2074041872 cites W2164404719 @default.
• W2074041872 cites W2189563616 @default.
• W2074041872 cites W2479922045 @default.
• W2074041872 cites W2580366857 @default.
• W2074041872 cites W2994817661 @default.
• W2074041872 doi "https://doi.org/10.1016/j.lithos.2010.10.004" @default.
• W2074041872 hasPublicationYear "2011" @default.
• W2074041872 type Work @default.
• W2074041872 sameAs 2074041872 @default.
• W2074041872 citedByCount "47" @default.
• W2074041872 countsByYear W20740418722012 @default.
• W2074041872 countsByYear W20740418722013 @default.
• W2074041872 countsByYear W20740418722014 @default.
• W2074041872 countsByYear W20740418722015 @default.
• W2074041872 countsByYear W20740418722016 @default.
• W2074041872 countsByYear W20740418722017 @default.
• W2074041872 countsByYear W20740418722018 @default.
• W2074041872 countsByYear W20740418722019 @default.
• W2074041872 countsByYear W20740418722020 @default.
• W2074041872 countsByYear W20740418722021 @default.
• W2074041872 countsByYear W20740418722022 @default.
• W2074041872 countsByYear W20740418722023 @default.

• next