Matches in SemOpenAlex for { <https://semopenalex.org/work/W2743687970> ?p ?o ?g. }
- W2743687970 endingPage "325" @default.
- W2743687970 startingPage "311" @default.
- W2743687970 abstract "Geochemical variations in granitic rocks may be controlled by their source rocks, melting reactions and subsequent magmatic processes, which resulted from various geodynamic processes related to subduction, collision, or slab break-off. Here we report new LA–ICP-MS zircon U–Pb ages and Hf isotopes, whole-rock chemistry and Sr–Nd isotopes for the late Early Cretaceous quartz diorite, granodiorite and monzogranite in the Gaoligong belt, southeastern Tibet Plateau. The zircon U–Pb dating yield ages of 113.9 ± 1.6, 111.7 ± 0.8, and 112.8 ± 1.7 Ma for the quartz diorite, granodiorite, and monzogranite, respectively, which are coeval with bimodal magmatism in the central and northern Lhasa sub-terrane. There are the distinct sources regions for the quartz diorite and granodiorite–monzogranite association. The quartz diorites are sodic, calc-alkaline and have high Mg# (52–54) values. They also have elevated initial 87Sr/86Sr (0.707019 to 0.709176) and low εNd(t) (− 5.16 to − 7.63), with variable zircon εHf(t) values (+ 5.65 to − 9.02). Zircon chemical data indicate a typical crustal-derived character with high Th (142–1260 ppm) and U (106–1082 ppm) and moderate U/Yb ratios (0.30 to 2.32) and Y content (705–1888 ppm). Those data suggest that the quartz diorites were derived from partial melting of ancient basaltic lower crust by a mantle-derived magma in source region. The granodiorite–monzogranite association has high-K calc-alkaline, weakly peraluminous characters. They show lower Nb/Ta (5.57 to 13.8), CaO/Na2O (0.62 to 1.21), higher Al2O3/TiO2 (24.4 to 44.4) ratios, more evolved whole-rock Sr–Nd and zircon Hf isotopic signatures, all of which suggest derivation from mixed basaltic and metasedimentary source rocks in a deep crustal zone. We propose that the granitic magmatisms at ca. 113–110 Ma in the Gaologong belt was triggered by the slab break-off of Bangong–Nujiang Tethyan oceanic lithosphere." @default.
- W2743687970 created "2017-08-17" @default.
- W2743687970 creator A5003317896 @default.
- W2743687970 creator A5048537490 @default.
- W2743687970 creator A5066222175 @default.
- W2743687970 creator A5084344063 @default.
- W2743687970 creator A5091148425 @default.
- W2743687970 date "2017-09-01" @default.
- W2743687970 modified "2023-10-15" @default.
- W2743687970 title "Late Early-Cretaceous quartz diorite–granodiorite–monzogranite association from the Gaoligong belt, southeastern Tibet Plateau: Chemical variations and geodynamic implications" @default.
- W2743687970 cites W1521262137 @default.
- W2743687970 cites W1871734886 @default.
- W2743687970 cites W1967082613 @default.
- W2743687970 cites W1969859799 @default.
- W2743687970 cites W1970363584 @default.
- W2743687970 cites W1970740923 @default.
- W2743687970 cites W1977911355 @default.
- W2743687970 cites W1980640006 @default.
- W2743687970 cites W1983396787 @default.
- W2743687970 cites W1990736031 @default.
- W2743687970 cites W1992429612 @default.
- W2743687970 cites W2001772043 @default.
- W2743687970 cites W2002460023 @default.
- W2743687970 cites W2002469616 @default.
- W2743687970 cites W2009280724 @default.
- W2743687970 cites W2009314098 @default.
- W2743687970 cites W2009464970 @default.
- W2743687970 cites W2010897022 @default.
- W2743687970 cites W2022859730 @default.
- W2743687970 cites W2023890163 @default.
- W2743687970 cites W2034397592 @default.
- W2743687970 cites W2036443034 @default.
- W2743687970 cites W2044983368 @default.
- W2743687970 cites W2047128953 @default.
- W2743687970 cites W2047879568 @default.
- W2743687970 cites W2051080397 @default.
- W2743687970 cites W2051273227 @default.
- W2743687970 cites W2058764465 @default.
- W2743687970 cites W2068157565 @default.
- W2743687970 cites W2068559197 @default.
- W2743687970 cites W2068668821 @default.
- W2743687970 cites W2068671620 @default.
- W2743687970 cites W2069547979 @default.
- W2743687970 cites W2072699489 @default.
- W2743687970 cites W2074675244 @default.
- W2743687970 cites W2075149957 @default.
- W2743687970 cites W2078397793 @default.
- W2743687970 cites W2082800626 @default.
- W2743687970 cites W2085153167 @default.
- W2743687970 cites W2086557360 @default.
- W2743687970 cites W2087041310 @default.
- W2743687970 cites W2092235841 @default.
- W2743687970 cites W2094727526 @default.
- W2743687970 cites W2095038610 @default.
- W2743687970 cites W2105111360 @default.
- W2743687970 cites W2114856901 @default.
- W2743687970 cites W2115054621 @default.
- W2743687970 cites W2115268527 @default.
- W2743687970 cites W2117129511 @default.
- W2743687970 cites W2128624170 @default.
- W2743687970 cites W2135830789 @default.
- W2743687970 cites W2138522501 @default.
- W2743687970 cites W2140559978 @default.
- W2743687970 cites W2160412587 @default.
- W2743687970 cites W2164468447 @default.
- W2743687970 cites W2164723659 @default.
- W2743687970 cites W2165601332 @default.
- W2743687970 cites W2167359669 @default.
- W2743687970 cites W2171801505 @default.
- W2743687970 cites W2227505540 @default.
- W2743687970 cites W2325514473 @default.
- W2743687970 cites W2466877594 @default.
- W2743687970 cites W2523726712 @default.
- W2743687970 cites W2621205510 @default.
- W2743687970 cites W786077987 @default.
- W2743687970 cites W816190195 @default.
- W2743687970 doi "https://doi.org/10.1016/j.lithos.2017.07.021" @default.
- W2743687970 hasPublicationYear "2017" @default.
- W2743687970 type Work @default.
- W2743687970 sameAs 2743687970 @default.
- W2743687970 citedByCount "27" @default.
- W2743687970 countsByYear W27436879702018 @default.
- W2743687970 countsByYear W27436879702020 @default.
- W2743687970 countsByYear W27436879702021 @default.
- W2743687970 countsByYear W27436879702022 @default.
- W2743687970 countsByYear W27436879702023 @default.
- W2743687970 crossrefType "journal-article" @default.
- W2743687970 hasAuthorship W2743687970A5003317896 @default.
- W2743687970 hasAuthorship W2743687970A5048537490 @default.
- W2743687970 hasAuthorship W2743687970A5066222175 @default.
- W2743687970 hasAuthorship W2743687970A5084344063 @default.
- W2743687970 hasAuthorship W2743687970A5091148425 @default.
- W2743687970 hasConcept C127313418 @default.
- W2743687970 hasConcept C151730666 @default.
- W2743687970 hasConcept C161509811 @default.
- W2743687970 hasConcept C17409809 @default.
- W2743687970 hasConcept C2776698055 @default.
- W2743687970 hasConcept C2778849375 @default.