FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2196364964> ?p ?o ?g. }

• W2196364964 endingPage "381" @default.
• W2196364964 startingPage "371" @default.
• W2196364964 abstract "Zircon U–Pb ages, Hf isotopes and whole-rock geochemical data are used to constrain the petrogenesis of the Late Triassic–Early Jurassic granitoids in southeastern China and their tectonic settings. The 225 Ma Qiuwang and 178 Ma Xiepu granites at Ningbo, Zhejiang Province, have εHf(t) values of − 15.7 to − 9.9 and − 17.6 to − 13.4, respectively. They are both ilmenite-series granitoids derived from the Paleoproterozoic basement of the Cathaysia Block in South China. The Late Triassic Qiuwang granite is strongly peraluminous with high zircon saturation temperatures (850–900 °C), and high Gd/Yb (2.7–4.8) and Ga/Al ratios (3.7–4.6 × 10− 4). In contrast, the Early Jurassic Xiepu granite is weakly peraluminous with low zircon saturation temperatures (~ 670 °C), low Gd/Yb (1.0–1.1) and high Ga/Al ratios (2.4–2.6 × 10− 4). The Qiuwang granite records higher melting temperatures and pressures than the younger Xiepu granite, reflecting a change in the tectonic regime from collisional tectonics to orogenic collapse. A regional review indicates that Triassic flat-slab subduction along the western Pacific may have led to thickening of the continental crust and metasomatism-oxidation of the continental lithosphere in the regions relatively close to the trench, where Cordilleran-type magnesian granitoids were generated. However, contemporaneous magnesian granitoids were produced in the thickened crust away from the trench, where the source rocks have uniformly moderate oxygen fugacities and metasomatism-oxidation was insignificant. Such Early Mesozoic “A-type” granitoids in the coastal region of South China are related to water-deficient and reduced melting conditions rather than an anorogenic tectonic setting." @default.
• W2196364964 created "2016-06-24" @default.
• W2196364964 creator A5012837262 @default.
• W2196364964 creator A5033069108 @default.
• W2196364964 creator A5041120433 @default.
• W2196364964 creator A5055907746 @default.
• W2196364964 creator A5063587219 @default.
• W2196364964 date "2016-01-01" @default.
• W2196364964 modified "2023-10-15" @default.
• W2196364964 title "Early Mesozoic ferroan (A-type) and magnesian granitoids in eastern South China: Tracing the influence of flat-slab subduction at the western Pacific margin" @default.
• W2196364964 cites W1496612225 @default.
• W2196364964 cites W1525258218 @default.
• W2196364964 cites W1938436079 @default.
• W2196364964 cites W1967350781 @default.
• W2196364964 cites W1970922572 @default.
• W2196364964 cites W1974616352 @default.
• W2196364964 cites W1976158538 @default.
• W2196364964 cites W1977650828 @default.
• W2196364964 cites W1980000874 @default.
• W2196364964 cites W1981207838 @default.
• W2196364964 cites W1982093108 @default.
• W2196364964 cites W1982133624 @default.
• W2196364964 cites W1983131682 @default.
• W2196364964 cites W1983765861 @default.
• W2196364964 cites W1988961923 @default.
• W2196364964 cites W1993290622 @default.
• W2196364964 cites W1996489529 @default.
• W2196364964 cites W1997160866 @default.
• W2196364964 cites W2001034959 @default.
• W2196364964 cites W2002469616 @default.
• W2196364964 cites W2002694143 @default.
• W2196364964 cites W2002947230 @default.
• W2196364964 cites W2003954276 @default.
• W2196364964 cites W2008335913 @default.
• W2196364964 cites W2013388505 @default.
• W2196364964 cites W2013747430 @default.
• W2196364964 cites W2020973699 @default.
• W2196364964 cites W2022002352 @default.
• W2196364964 cites W2022859730 @default.
• W2196364964 cites W2024436619 @default.
• W2196364964 cites W2026430737 @default.
• W2196364964 cites W2026740526 @default.
• W2196364964 cites W2028120826 @default.
• W2196364964 cites W2029157156 @default.
• W2196364964 cites W2037240939 @default.
• W2196364964 cites W2039853569 @default.
• W2196364964 cites W2040126025 @default.
• W2196364964 cites W2053273118 @default.
• W2196364964 cites W2056061487 @default.
• W2196364964 cites W2059010589 @default.
• W2196364964 cites W2060003735 @default.
• W2196364964 cites W2060873154 @default.
• W2196364964 cites W2064155028 @default.
• W2196364964 cites W2065210509 @default.
• W2196364964 cites W2071512363 @default.
• W2196364964 cites W2078887974 @default.
• W2196364964 cites W2083558141 @default.
• W2196364964 cites W2085217600 @default.
• W2196364964 cites W2085691334 @default.
• W2196364964 cites W2087129024 @default.
• W2196364964 cites W2087669497 @default.
• W2196364964 cites W2088401751 @default.
• W2196364964 cites W2092528520 @default.
• W2196364964 cites W2099932450 @default.
• W2196364964 cites W2102811433 @default.
• W2196364964 cites W2103592777 @default.
• W2196364964 cites W2105269962 @default.
• W2196364964 cites W2111173087 @default.
• W2196364964 cites W2112435406 @default.
• W2196364964 cites W2120265417 @default.
• W2196364964 cites W2133017720 @default.
• W2196364964 cites W2134940746 @default.
• W2196364964 cites W2164468447 @default.
• W2196364964 cites W2283066148 @default.
• W2196364964 cites W2324896590 @default.
• W2196364964 doi "https://doi.org/10.1016/j.lithos.2015.11.025" @default.
• W2196364964 hasPublicationYear "2016" @default.
• W2196364964 type Work @default.
• W2196364964 sameAs 2196364964 @default.
• W2196364964 citedByCount "34" @default.
• W2196364964 countsByYear W21963649642017 @default.
• W2196364964 countsByYear W21963649642018 @default.
• W2196364964 countsByYear W21963649642019 @default.
• W2196364964 countsByYear W21963649642020 @default.
• W2196364964 countsByYear W21963649642021 @default.
• W2196364964 countsByYear W21963649642022 @default.
• W2196364964 countsByYear W21963649642023 @default.
• W2196364964 crossrefType "journal-article" @default.
• W2196364964 hasAuthorship W2196364964A5012837262 @default.
• W2196364964 hasAuthorship W2196364964A5033069108 @default.
• W2196364964 hasAuthorship W2196364964A5041120433 @default.
• W2196364964 hasAuthorship W2196364964A5055907746 @default.
• W2196364964 hasAuthorship W2196364964A5063587219 @default.
• W2196364964 hasConcept C109007969 @default.
• W2196364964 hasConcept C118270999 @default.
• W2196364964 hasConcept C127313418 @default.
• W2196364964 hasConcept C141646446 @default.
• W2196364964 hasConcept C151730666 @default.

• next