FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4362608266> ?p ?o ?g. }

• W4362608266 endingPage "107166" @default.
• W4362608266 startingPage "107166" @default.
• W4362608266 abstract "In the world-class Gejiu Sn district, South China, tin mineralization is related to the Gejiu granitoids, which consist of porphyritic quartz monzonite, syenogranite, and porphyritic/equigranular biotite monzogranites. Zircon UPb dating shows that these granitoids were emplaced at ca. 77.9–81.7 Ma. Close spatio-temporal associations, systematic element distribution patterns, and similar isotopic compositions, together reveal that they are consanguineous, and the porphyritic quartz monzonite represents relatively primitive magma. The occurrence of hornblende, high apatite NdN/NdN* (mostly > 1), and whole-rock evolutionary trends, collectively indicate that the Gejiu granitoids are fractionated I-type granites. Negative and fluctuant εHf(t) values (−13.3 to −3.8) reveal that their I-type affinities could be caused by a mixing source through partial melting of metasedimentary rocks with minor input of mantle-derived materials, which is supported by the presence of mafic microgranular enclaves (MMEs). Zircon and apatite elemental fingerprints, combined with Rayleigh fractional crystallization modeling, decipher a two-stage fractional crystallization of hornblende-dominated and feldspar-dominated. The negative correlation between whole-rock Fe2O3/FeO and Rb/Sr ratios suggests that the magmatic oxygen fugacity gradually decreases with fractional crystallization. High zircon saturation temperatures (∼ 835 °C) indicate that the additional heat from the mantle provided a higher melting temperature to trigger biotite breakdown reactions, which can effectively release Sn into the initial melt. Subsequently, tin in magma underwent a two-stage enrichment process under the conjunctive effect of the variation of fractionating phases and magmatic redox state. In the first stage, there is no significant Sn enrichment during hornblende, magnetite, and titanite fractionation, which is due to the compatibility of Sn with these Ti-bearing minerals under oxidized conditions. In the second stage, the dominant Sn-poor feldspar with limited Sn-sequestering biotite fractionation under more reduced conditions efficiently increases Sn concentration in the residual melt by a factor of ∼ 8, as demonstrated by systematic apatite geochemical data. The hysteretic crystallization of biotite prevents the premature sequestration of Sn and reserves adequate metals for eventual mineralization. Finally, fluid exsolution during the magmatic-hydrothermal transition loads magmatically enriched Sn into the hydrothermal system, leading to the formation of the Gejiu Sn district." @default.
• W4362608266 created "2023-04-06" @default.
• W4362608266 creator A5009365645 @default.
• W4362608266 creator A5014215034 @default.
• W4362608266 creator A5017698636 @default.
• W4362608266 creator A5022526821 @default.
• W4362608266 creator A5029484872 @default.
• W4362608266 creator A5030046993 @default.
• W4362608266 creator A5030103329 @default.
• W4362608266 creator A5060753420 @default.
• W4362608266 date "2023-07-01" @default.
• W4362608266 modified "2023-10-18" @default.
• W4362608266 title "Petrogenesis of Sn-related granitoids and implications for the formation of the world-class Gejiu Sn district, South China: Insights from whole-rock and accessory mineral geochemistry" @default.
• W4362608266 cites W1966189692 @default.
• W4362608266 cites W1971685925 @default.
• W4362608266 cites W1973923863 @default.
• W4362608266 cites W1977650828 @default.
• W4362608266 cites W1978870013 @default.
• W4362608266 cites W1980255347 @default.
• W4362608266 cites W1983396787 @default.
• W4362608266 cites W1997710040 @default.
• W4362608266 cites W1999708461 @default.
• W4362608266 cites W2003026770 @default.
• W4362608266 cites W2008435820 @default.
• W4362608266 cites W2019034794 @default.
• W4362608266 cites W2021987309 @default.
• W4362608266 cites W2022002352 @default.
• W4362608266 cites W2027149122 @default.
• W4362608266 cites W2028048720 @default.
• W4362608266 cites W2035662349 @default.
• W4362608266 cites W2046961523 @default.
• W4362608266 cites W2049306346 @default.
• W4362608266 cites W2053396208 @default.
• W4362608266 cites W2054653182 @default.
• W4362608266 cites W2061837047 @default.
• W4362608266 cites W2067408094 @default.
• W4362608266 cites W2071103381 @default.
• W4362608266 cites W2074463495 @default.
• W4362608266 cites W2075449021 @default.
• W4362608266 cites W2081284207 @default.
• W4362608266 cites W2081673195 @default.
• W4362608266 cites W2088848716 @default.
• W4362608266 cites W2103859457 @default.
• W4362608266 cites W2107790246 @default.
• W4362608266 cites W2124562339 @default.
• W4362608266 cites W2138522501 @default.
• W4362608266 cites W2139280138 @default.
• W4362608266 cites W2154178101 @default.
• W4362608266 cites W2163402984 @default.
• W4362608266 cites W2181312688 @default.
• W4362608266 cites W2262537693 @default.
• W4362608266 cites W2264240170 @default.
• W4362608266 cites W2275101079 @default.
• W4362608266 cites W2460600588 @default.
• W4362608266 cites W2511531429 @default.
• W4362608266 cites W2548439805 @default.
• W4362608266 cites W2567323638 @default.
• W4362608266 cites W2586194886 @default.
• W4362608266 cites W2594092089 @default.
• W4362608266 cites W2611807494 @default.
• W4362608266 cites W2797020800 @default.
• W4362608266 cites W2804120792 @default.
• W4362608266 cites W2897393521 @default.
• W4362608266 cites W2908119072 @default.
• W4362608266 cites W2966635181 @default.
• W4362608266 cites W3012974908 @default.
• W4362608266 cites W3037565632 @default.
• W4362608266 cites W3049285815 @default.
• W4362608266 cites W3148708686 @default.
• W4362608266 cites W3192839583 @default.
• W4362608266 cites W3199551901 @default.
• W4362608266 cites W3199685712 @default.
• W4362608266 cites W3203034236 @default.
• W4362608266 cites W3207482323 @default.
• W4362608266 cites W3209269921 @default.
• W4362608266 cites W4212774731 @default.
• W4362608266 cites W4221124808 @default.
• W4362608266 cites W4281383560 @default.
• W4362608266 cites W4285589385 @default.
• W4362608266 cites W4292749658 @default.
• W4362608266 cites W4293069636 @default.
• W4362608266 cites W4307721997 @default.
• W4362608266 doi "https://doi.org/10.1016/j.lithos.2023.107166" @default.
• W4362608266 hasPublicationYear "2023" @default.
• W4362608266 type Work @default.
• W4362608266 citedByCount "0" @default.
• W4362608266 crossrefType "journal-article" @default.
• W4362608266 hasAuthorship W4362608266A5009365645 @default.
• W4362608266 hasAuthorship W4362608266A5014215034 @default.
• W4362608266 hasAuthorship W4362608266A5017698636 @default.
• W4362608266 hasAuthorship W4362608266A5022526821 @default.
• W4362608266 hasAuthorship W4362608266A5029484872 @default.
• W4362608266 hasAuthorship W4362608266A5030046993 @default.
• W4362608266 hasAuthorship W4362608266A5030103329 @default.
• W4362608266 hasAuthorship W4362608266A5060753420 @default.
• W4362608266 hasConcept C11872896 @default.
• W4362608266 hasConcept C127313418 @default.
• W4362608266 hasConcept C151730666 @default.

• next