FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1570814245> ?p ?o ?g. }

• W1570814245 endingPage "1002" @default.
• W1570814245 startingPage "979" @default.
• W1570814245 abstract "The Qinling-Tongbai-Dabie-Sulu orogenic belt comprises a Palaeozoic accretion-dominated system in the north and a Mesozoic collision-dominated system in the south. A combined petrological and geochronological study of the medium-to-high grade metamorphic rocks from the diverse Palaeozoic tectonic units in the Tongbai orogen was undertaken to help elucidate the origins of Triassic ultrahigh-pressure metamorphism and collision dynamics between the Sino-Korean and Yangtze cratons. Peak metamorphic conditions are 570–610 °C and 9.3–11.2 kbar for the lower unit of the Kuanping Group, 630–650 °C and 6.6–8.9 kbar for the upper unit of the Kuanping Group, 550–600 °C and 6.3–7.7 kbar for the Erlangping Group, 770–830 °C and 6.9–8.5 kbar for the Qinling Group and 660–720 °C and 9.1–11.5 kbar for the Guishan complex. Reaction textures and garnet compositions indicate clockwise P–T paths for the amphibolite facies rocks of the Kuanping Group and Guishan complex, and an anticlockwise P–T path for the granulite facies rocks of the Qinling Group. Sensitive high-resolution ion microprobe U–Pb zircon dating on metamorphic rocks and deformed granite/pegmatites revealed two major Palaeozoic tectonometamorphic events. (i) During the Silurian-Devonian (c. 440–400 Ma), the Qinling continental arc and Erlangping intra-oceanic arc collided with the Sino-Korean craton. The emplacement of the Huanggang diorite complex resulted in an inverted thermal gradient in the underlying Kuanping Group and subsequent thermal relaxation during the exhumation. Meanwhile, the oceanic subduction beneath the Qinling continental arc produced magmatic underplating and intrusion, leading to granulite facies metamorphism followed by a near-isobaric cooling path. (ii) During the Carboniferous (c. 340–310 Ma), the northward subduction of the Palaeo-Tethyan ocean generated a medium P/T Guishan complex in the hangingwall and a high P/T Xiongdian eclogite belt in the footwall. The Guishan complex and Xiongdian eclogite belt are therefore considered to be paired metamorphic belts. Subsequent separation of the paired belts is inferred to be related to the juxtaposition of the Carboniferous eclogites with the Triassic HP metamorphic complex during continental subduction and exhumation." @default.
• W1570814245 created "2016-06-24" @default.
• W1570814245 creator A5002992949 @default.
• W1570814245 creator A5022125374 @default.
• W1570814245 creator A5022274692 @default.
• W1570814245 creator A5082519097 @default.
• W1570814245 creator A5085489139 @default.
• W1570814245 creator A5090434361 @default.
• W1570814245 date "2011-07-18" @default.
• W1570814245 modified "2023-10-18" @default.
• W1570814245 title "Metamorphic patterns and SHRIMP zircon ages of medium-to-high grade rocks from the Tongbai orogen, central China: implications for multiple accretion/collision processes prior to terminal continental collision" @default.
• W1570814245 cites W1497952855 @default.
• W1570814245 cites W1521262137 @default.
• W1570814245 cites W1575749970 @default.
• W1570814245 cites W1830358639 @default.
• W1570814245 cites W186841988 @default.
• W1570814245 cites W1930514495 @default.
• W1570814245 cites W1963607885 @default.
• W1570814245 cites W1967635228 @default.
• W1570814245 cites W1970483293 @default.
• W1570814245 cites W1973125903 @default.
• W1570814245 cites W1975652198 @default.
• W1570814245 cites W1985160890 @default.
• W1570814245 cites W1986092846 @default.
• W1570814245 cites W1986460045 @default.
• W1570814245 cites W1987423017 @default.
• W1570814245 cites W1990742678 @default.
• W1570814245 cites W1991394204 @default.
• W1570814245 cites W1993550769 @default.
• W1570814245 cites W1997774186 @default.
• W1570814245 cites W2003454252 @default.
• W1570814245 cites W2007307178 @default.
• W1570814245 cites W2008691821 @default.
• W1570814245 cites W2008693928 @default.
• W1570814245 cites W2018662544 @default.
• W1570814245 cites W2021221536 @default.
• W1570814245 cites W2021345743 @default.
• W1570814245 cites W2023696126 @default.
• W1570814245 cites W2027316964 @default.
• W1570814245 cites W2036174339 @default.
• W1570814245 cites W2040287076 @default.
• W1570814245 cites W2040549377 @default.
• W1570814245 cites W2042911974 @default.
• W1570814245 cites W2042945599 @default.
• W1570814245 cites W2043291535 @default.
• W1570814245 cites W2045046124 @default.
• W1570814245 cites W2054247338 @default.
• W1570814245 cites W2056296253 @default.
• W1570814245 cites W2062780038 @default.
• W1570814245 cites W2067019494 @default.
• W1570814245 cites W2068403951 @default.
• W1570814245 cites W2071369893 @default.
• W1570814245 cites W2075666876 @default.
• W1570814245 cites W2088348719 @default.
• W1570814245 cites W2089832041 @default.
• W1570814245 cites W2093306862 @default.
• W1570814245 cites W2094414093 @default.
• W1570814245 cites W2098003873 @default.
• W1570814245 cites W2100650744 @default.
• W1570814245 cites W2104177181 @default.
• W1570814245 cites W2106146079 @default.
• W1570814245 cites W2118079032 @default.
• W1570814245 cites W2127177584 @default.
• W1570814245 cites W2128383999 @default.
• W1570814245 cites W2130365567 @default.
• W1570814245 cites W2140816768 @default.
• W1570814245 cites W2160614281 @default.
• W1570814245 cites W2163462779 @default.
• W1570814245 cites W2164756098 @default.
• W1570814245 cites W2315536356 @default.
• W1570814245 cites W2317096966 @default.
• W1570814245 cites W2332162731 @default.
• W1570814245 cites W2347127932 @default.
• W1570814245 cites W2412269711 @default.
• W1570814245 doi "https://doi.org/10.1111/j.1525-1314.2011.00952.x" @default.
• W1570814245 hasPublicationYear "2011" @default.
• W1570814245 type Work @default.
• W1570814245 sameAs 1570814245 @default.
• W1570814245 citedByCount "110" @default.
• W1570814245 countsByYear W15708142452012 @default.
• W1570814245 countsByYear W15708142452013 @default.
• W1570814245 countsByYear W15708142452014 @default.
• W1570814245 countsByYear W15708142452015 @default.
• W1570814245 countsByYear W15708142452016 @default.
• W1570814245 countsByYear W15708142452017 @default.
• W1570814245 countsByYear W15708142452018 @default.
• W1570814245 countsByYear W15708142452019 @default.
• W1570814245 countsByYear W15708142452020 @default.
• W1570814245 countsByYear W15708142452021 @default.
• W1570814245 countsByYear W15708142452022 @default.
• W1570814245 countsByYear W15708142452023 @default.
• W1570814245 crossrefType "journal-article" @default.
• W1570814245 hasAuthorship W1570814245A5002992949 @default.
• W1570814245 hasAuthorship W1570814245A5022125374 @default.
• W1570814245 hasAuthorship W1570814245A5022274692 @default.
• W1570814245 hasAuthorship W1570814245A5082519097 @default.
• W1570814245 hasAuthorship W1570814245A5085489139 @default.
• W1570814245 hasAuthorship W1570814245A5090434361 @default.

• next