FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2978552685> ?p ?o ?g. }

• W2978552685 endingPage "103160" @default.
• W2978552685 startingPage "103160" @default.
• W2978552685 abstract "The supergiant Shizhuyuan W–Sn–Mo–Bi polymetallic deposit is located in the Nanling Range, and is intimately related to the Qianlishan granite complex intruded during the Late Jurassic period. The complex consists of three intrusive phases: porphyritic biotite granite (PBG), equigranular biotite granite (EBG), and porphyritic granite dyke. In this work, the distinct geochemical features of magmatic and hydrothermally-altered zircons from the Qianlishan complex are used to reveal the magmatic-hydrothermal evolution of the deposit. Whole-rock geochemistry and mineralogy show that EBG samples have experienced stronger fractional crystallization than PBG samples. Zircon U–Pb dating constrains the intrusive episodes at 155–153 Ma and ~152 Ma for the PBG and EBG, respectively, and subsequent hydrothermal events (revealed by hydrothermal zircon ages) at 154–153 Ma and 152–150 Ma. Hydrothermally-altered zircon and paragenetic mineral inclusions from EBG samples show textures and compositional properties suggesting they were intensely altered by a zirconium saturated aqueous fluid (Type 1), enriched in most trace and metallogenic elements (e.g., Zr, REEs, Hf, P, U, Th, Nb, Ta, Ti, Pb, Al, Fe, Mg, Ca, Mn, W, and Sn) and volatiles (F, Cl, Li, CO2 and H2O). This fluid was relatively lower in temperature, pressure and oxygen fugacity (average Ce4+/Ce3+ = 11.2). Type 2 fluid, represented by hydrothermally-altered zircons found in PBG, was depleted in trace elements and had a relatively higher temperature and pressure and low fO2 (Ce4+/Ce3+ = 2.12–29.16). Type 3 fluid, as evidenced by fluid-altered zircons from the greisenized granite, was likely a further evolved product of the Type 2 fluid, given its moderate cargo of most trace elements but also with exceedingly low Ce4+/Ce3+ values (2.9–33.45). The Type 3 fluids might be precursors of W–Sn mineralizing fluids, whereas the Type 1 fluids were likely to represent mature ore-forming fluids, which were activated during the late skarn stage but before the retrograde mineralization stage. Compared with the fO2 of PBG and EBG magmas calculated by non-altered magmatic zircons (average Ce4+/Ce3+ = 31.47 and 49.21), it seems that the hydrothermal fluids generated by them became more reduced during the further evolution. A progressive process can thus be divided: PBG → Type 2 → Type 3 → EBG → Type 1, with the gradual accumulation of ore-forming materials. The enrichment of most elements in hydrothermal zircons further indicates a substitution of Y, REEs, P, Hf, U, Th, Ti, Nb, Ta, Ca, K, Fe, and Mn for Zr4+ and Si4+ in the zircon lattice. Most fluid-altered zircons exhibit a similar 176Hf/177Hf distribution range (−11 to −6) but evidently elevated 176Lu/177Hf and 176Yb/177Hf ratios with magmatic ones. This indicates that three types of hydrothermal fluids were magmatic-derived, whereas Lu and Yb were highly mobile during the hydrothermal event. Based on the results, a magmatic-hydrothermal evolution model is presented for Shizhuyuan zircons. This research highlights the use of zircon as a powerful tool in revealing the complex magmatic-hydrothermal processes and perhaps mineralization potential in (highly evolved) granite-associated mineralization systems." @default.
• W2978552685 created "2019-10-10" @default.
• W2978552685 creator A5032732866 @default.
• W2978552685 creator A5049514311 @default.
• W2978552685 creator A5052648518 @default.
• W2978552685 creator A5052716474 @default.
• W2978552685 date "2019-12-01" @default.
• W2978552685 modified "2023-10-12" @default.
• W2978552685 title "Zircon records multiple magmatic-hydrothermal processes at the giant Shizhuyuan W–Sn–Mo–Bi polymetallic deposit, South China" @default.
• W2978552685 cites W1525258218 @default.
• W2978552685 cites W1541910269 @default.
• W2978552685 cites W1570456448 @default.
• W2978552685 cites W1572418335 @default.
• W2978552685 cites W1959662544 @default.
• W2978552685 cites W1968409933 @default.
• W2978552685 cites W1968583876 @default.
• W2978552685 cites W1970270960 @default.
• W2978552685 cites W1974156473 @default.
• W2978552685 cites W1975700771 @default.
• W2978552685 cites W1986226338 @default.
• W2978552685 cites W1986560096 @default.
• W2978552685 cites W1988744847 @default.
• W2978552685 cites W1991851675 @default.
• W2978552685 cites W1991987220 @default.
• W2978552685 cites W1992552401 @default.
• W2978552685 cites W1996328804 @default.
• W2978552685 cites W1997040345 @default.
• W2978552685 cites W1999166202 @default.
• W2978552685 cites W1999708461 @default.
• W2978552685 cites W2003311821 @default.
• W2978552685 cites W2006991140 @default.
• W2978552685 cites W2007592351 @default.
• W2978552685 cites W2010021674 @default.
• W2978552685 cites W2013366222 @default.
• W2978552685 cites W2013535259 @default.
• W2978552685 cites W2016359595 @default.
• W2978552685 cites W2017161252 @default.
• W2978552685 cites W2017496723 @default.
• W2978552685 cites W2020139762 @default.
• W2978552685 cites W2020316016 @default.
• W2978552685 cites W2020688605 @default.
• W2978552685 cites W2020782995 @default.
• W2978552685 cites W2028048720 @default.
• W2978552685 cites W2029157156 @default.
• W2978552685 cites W2030066062 @default.
• W2978552685 cites W2032816924 @default.
• W2978552685 cites W2034383015 @default.
• W2978552685 cites W2036174339 @default.
• W2978552685 cites W2036918177 @default.
• W2978552685 cites W2046447115 @default.
• W2978552685 cites W2046961523 @default.
• W2978552685 cites W2048554967 @default.
• W2978552685 cites W2051805987 @default.
• W2978552685 cites W2052443737 @default.
• W2978552685 cites W2054653182 @default.
• W2978552685 cites W2059206475 @default.
• W2978552685 cites W2066240400 @default.
• W2978552685 cites W2071103381 @default.
• W2978552685 cites W2073226128 @default.
• W2978552685 cites W2074559552 @default.
• W2978552685 cites W2075348117 @default.
• W2978552685 cites W2076321735 @default.
• W2978552685 cites W2076725365 @default.
• W2978552685 cites W2079255985 @default.
• W2978552685 cites W2079946659 @default.
• W2978552685 cites W2087470623 @default.
• W2978552685 cites W2090426664 @default.
• W2978552685 cites W2090695609 @default.
• W2978552685 cites W2093369526 @default.
• W2978552685 cites W2093978379 @default.
• W2978552685 cites W2094636417 @default.
• W2978552685 cites W2098235917 @default.
• W2978552685 cites W2117964524 @default.
• W2978552685 cites W2133958255 @default.
• W2978552685 cites W2139280138 @default.
• W2978552685 cites W2149931102 @default.
• W2978552685 cites W2152181325 @default.
• W2978552685 cites W2154966130 @default.
• W2978552685 cites W2163661859 @default.
• W2978552685 cites W2164073782 @default.
• W2978552685 cites W2164468447 @default.
• W2978552685 cites W2179617371 @default.
• W2978552685 cites W2192105522 @default.
• W2978552685 cites W2262537693 @default.
• W2978552685 cites W2320712877 @default.
• W2978552685 cites W2349186271 @default.
• W2978552685 cites W2411603221 @default.
• W2978552685 cites W2535653206 @default.
• W2978552685 cites W2586561663 @default.
• W2978552685 cites W2594092089 @default.
• W2978552685 cites W2601882231 @default.
• W2978552685 cites W2771382009 @default.
• W2978552685 cites W2774551849 @default.
• W2978552685 cites W2775260090 @default.
• W2978552685 cites W2788715054 @default.
• W2978552685 cites W2792765141 @default.
• W2978552685 cites W2793866479 @default.
• W2978552685 cites W2800069843 @default.

• next