FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3206705969> ?p ?o ?g. }

• W3206705969 endingPage "550" @default.
• W3206705969 startingPage "535" @default.
• W3206705969 abstract "The late Permian to Early Triassic volcano-sedimentary succession associated with the Emeishan Large Igneous Province (LIP) is well preserved in the Binchuan area, Southwest China. This paper presents coupled zircon U-Pb age, trace element, and Hf isotope analyses from the succession, together with whole-rock geochemical compositions, to reveal the origin and evolution of volcanic rocks of the LIP. Zircons from the matrix and a rhyolite clast in the Lower Triassic conglomerate bed yield identical U-Pb ages of ca. 260 Ma and have geochemical affinities to those crystallized from within-plate magmas. These features, combined with the dominance of rhyolite clasts from this horizon, imply a source related to Emeishan silicic volcanic rocks. Zircons from silicic ignimbrite and rhyolite in the upper volcanic succession of the LIP display high εHf(t) values (+4.2 to +12.9), low Th/Nb and U/Yb ratios, and similar εNd(t) values (−0.17 to +0.47) to high-Ti basalts. These chemical and isotopic characteristics are consistent with the eroded silicic volcanic rocks, indicating that the late-stage silicic volcanic rocks were generated by fractionation of high-Ti basaltic magmas without significant crustal contamination. Although the late Permian zircons from the lower and upper low-Ti basalt successions all show arc-like geochemical characteristics with high Th/Nb and U/Yb ratios, the former has much lower εHf(t) values (−11.7 to −3.6) than the latter (+4.4 to +11.6), and the zircons from the upper low-Ti basalt succession show positive εHf(t) values similar to the studied rhyolites. Samples from the lower low-Ti basalt succession have relatively higher εNd(t) values (−2.66 to +3.38) than those from the upper low-Ti basalt succession (−4.48 to −0.82). These geochemical features indicate the early-stage low-Ti basalts may be mainly derived from a previously enriched subcontinental mantle lithosphere, whereas the late-stage low-Ti basalts may be generated from the increasing involvement of asthenospheric mantle source with crustal contamination." @default.
• W3206705969 created "2021-10-25" @default.
• W3206705969 creator A5002372684 @default.
• W3206705969 creator A5004588382 @default.
• W3206705969 creator A5019716362 @default.
• W3206705969 creator A5020407181 @default.
• W3206705969 creator A5068985640 @default.
• W3206705969 creator A5069605311 @default.
• W3206705969 creator A5073018472 @default.
• W3206705969 creator A5081894617 @default.
• W3206705969 date "2022-05-01" @default.
• W3206705969 modified "2023-10-14" @default.
• W3206705969 title "Zircon U-Pb age, trace element, and Hf isotopic constrains on the origin and evolution of the Emeishan Large Igneous Province" @default.
• W3206705969 cites W1933526536 @default.
• W3206705969 cites W1966990309 @default.
• W3206705969 cites W1967767697 @default.
• W3206705969 cites W1974356108 @default.
• W3206705969 cites W1977531160 @default.
• W3206705969 cites W1980000874 @default.
• W3206705969 cites W1981316911 @default.
• W3206705969 cites W1984945854 @default.
• W3206705969 cites W1987907556 @default.
• W3206705969 cites W1987974104 @default.
• W3206705969 cites W1988627424 @default.
• W3206705969 cites W1992245388 @default.
• W3206705969 cites W1994446497 @default.
• W3206705969 cites W1995982090 @default.
• W3206705969 cites W1997853880 @default.
• W3206705969 cites W1999448338 @default.
• W3206705969 cites W2000693231 @default.
• W3206705969 cites W2003693743 @default.
• W3206705969 cites W2013259970 @default.
• W3206705969 cites W2016223358 @default.
• W3206705969 cites W2029401070 @default.
• W3206705969 cites W2031194632 @default.
• W3206705969 cites W2035178582 @default.
• W3206705969 cites W2039176231 @default.
• W3206705969 cites W2040901440 @default.
• W3206705969 cites W2044971079 @default.
• W3206705969 cites W2049442993 @default.
• W3206705969 cites W2051704045 @default.
• W3206705969 cites W2052920966 @default.
• W3206705969 cites W2064411977 @default.
• W3206705969 cites W2066695862 @default.
• W3206705969 cites W2070047250 @default.
• W3206705969 cites W2073863738 @default.
• W3206705969 cites W2076068759 @default.
• W3206705969 cites W2081518814 @default.
• W3206705969 cites W2087494921 @default.
• W3206705969 cites W2088997939 @default.
• W3206705969 cites W2091143358 @default.
• W3206705969 cites W2093369526 @default.
• W3206705969 cites W2093592862 @default.
• W3206705969 cites W2097228887 @default.
• W3206705969 cites W2103592777 @default.
• W3206705969 cites W2120895966 @default.
• W3206705969 cites W2121221338 @default.
• W3206705969 cites W2133804198 @default.
• W3206705969 cites W2138522501 @default.
• W3206705969 cites W2140136526 @default.
• W3206705969 cites W2147038702 @default.
• W3206705969 cites W2154157536 @default.
• W3206705969 cites W2267222433 @default.
• W3206705969 cites W2510917724 @default.
• W3206705969 cites W2583906772 @default.
• W3206705969 cites W2619277305 @default.
• W3206705969 cites W2733371642 @default.
• W3206705969 cites W2765746014 @default.
• W3206705969 cites W2789900376 @default.
• W3206705969 cites W2790497323 @default.
• W3206705969 cites W2807789141 @default.
• W3206705969 cites W2808397930 @default.
• W3206705969 cites W2809537835 @default.
• W3206705969 cites W2915414273 @default.
• W3206705969 cites W2919971498 @default.
• W3206705969 cites W2952201615 @default.
• W3206705969 cites W2987446159 @default.
• W3206705969 cites W3005103415 @default.
• W3206705969 cites W3005365712 @default.
• W3206705969 cites W3005816334 @default.
• W3206705969 cites W3013186756 @default.
• W3206705969 cites W3015313699 @default.
• W3206705969 cites W3092918054 @default.
• W3206705969 cites W3094119674 @default.
• W3206705969 cites W3124936149 @default.
• W3206705969 cites W336103437 @default.
• W3206705969 cites W911873527 @default.
• W3206705969 doi "https://doi.org/10.1016/j.gr.2021.09.023" @default.
• W3206705969 hasPublicationYear "2022" @default.
• W3206705969 type Work @default.
• W3206705969 sameAs 3206705969 @default.
• W3206705969 citedByCount "7" @default.
• W3206705969 countsByYear W32067059692022 @default.
• W3206705969 countsByYear W32067059692023 @default.
• W3206705969 crossrefType "journal-article" @default.
• W3206705969 hasAuthorship W3206705969A5002372684 @default.
• W3206705969 hasAuthorship W3206705969A5004588382 @default.
• W3206705969 hasAuthorship W3206705969A5019716362 @default.

• next