FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2020461753> ?p ?o ?g. }

• W2020461753 endingPage "271" @default.
• W2020461753 startingPage "257" @default.
• W2020461753 abstract "The Pingüino deposit, located in the low sulfidation epithermal metallogenetical province of the Deseado Massif, Patagonia, Argentina, represents a distinct deposit type in the region. It evolved through two different mineralization events: an early In-bearing polymetallic event that introduced In, Zn, Pb, Ag, Cd, Au, As, Cu, Sn, W and Bi represented by complex sulfide mineralogy, and a late Ag–Au quartz-rich vein type that crosscut and overprints the early polymetallic mineralization. The indium-bearing polymetallic mineralization developed in three stages: an early Cu–Au–In–As–Sn–W–Bi stage (Ps1), a Zn–Pb–Ag–In–Cd–Sb stage (Ps2) and a late Zn–In–Cd (Ps3). Indium concentrations in the polymetallic veins show a wide range (3.4 to 1,184 ppm In). The highest indium values (up to 1,184 ppm) relate to the Ps2 mineralization stage, and are associated with Fe-rich sphalerites, although significant In enrichment (up to 159 ppm) is also present in the Ps1 paragenesis associated with Sn-minerals (ferrokesterite and cassiterite). The hydrothermal alteration associated with the polymetallic mineralization is characterized by advanced argillic alteration within the immediate vein zone, and sericitic alteration enveloping the vein zone. Fluid inclusion studies indicate homogenisation temperatures of 308.2–327°C for Ps1 and 255–312.4°C for Ps2, and low to moderate salinities (2 to 5 eq.wt.% NaCl and 4 to 9 eq.wt.% NaCl, respectively). δ34S values of sulfide minerals (+0.76‰ to +3.61‰) indicate a possible magmatic source for the sulfur in the polymetallic mineralization while Pb isotope ratios for the sulfides and magmatic rocks (206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios of 17.379 to 18.502; 15.588 to 15.730 and 38.234 to 38.756, respectively) are consistent with the possibility that the Pb reservoirs for both had the same crustal source. Spatial relationships, hydrothermal alteration styles, S and Pb isotopic data suggest a probable genetic relation between the polymetallic mineralization and dioritic intrusions that could have been the source of metals and hydrothermal fluids. Mineralization paragenesis, alteration mineralogy, geochemical signatures, fluid inclusion data and isotopic data, confirm that the In-bearing polymetallic mineralization from Pingüino deposit is a distinct type, in comparison with the well-known epithermal low sulfidation mineralization from the Deseado Massif." @default.
• W2020461753 created "2016-06-24" @default.
• W2020461753 creator A5019383410 @default.
• W2020461753 creator A5029930846 @default.
• W2020461753 creator A5044198268 @default.
• W2020461753 creator A5056693792 @default.
• W2020461753 creator A5083338748 @default.
• W2020461753 creator A5089728816 @default.
• W2020461753 date "2011-01-08" @default.
• W2020461753 modified "2023-10-03" @default.
• W2020461753 title "Pingüino In-bearing polymetallic vein deposit, Deseado Massif, Patagonia, Argentina: characteristics of mineralization and ore-forming fluids" @default.
• W2020461753 cites W1553227945 @default.
• W2020461753 cites W1705390180 @default.
• W2020461753 cites W1970621049 @default.
• W2020461753 cites W1974596620 @default.
• W2020461753 cites W1977721570 @default.
• W2020461753 cites W1983843436 @default.
• W2020461753 cites W1986694990 @default.
• W2020461753 cites W1992376551 @default.
• W2020461753 cites W1993593163 @default.
• W2020461753 cites W1995054862 @default.
• W2020461753 cites W2003065479 @default.
• W2020461753 cites W2005121896 @default.
• W2020461753 cites W2010981570 @default.
• W2020461753 cites W2013804710 @default.
• W2020461753 cites W2018093298 @default.
• W2020461753 cites W2031882447 @default.
• W2020461753 cites W2043747344 @default.
• W2020461753 cites W2044181606 @default.
• W2020461753 cites W2061002420 @default.
• W2020461753 cites W2068036083 @default.
• W2020461753 cites W2068509334 @default.
• W2020461753 cites W2089717176 @default.
• W2020461753 cites W2098627944 @default.
• W2020461753 cites W2100168657 @default.
• W2020461753 cites W2106213418 @default.
• W2020461753 cites W2117343536 @default.
• W2020461753 cites W2123026017 @default.
• W2020461753 cites W2127521842 @default.
• W2020461753 cites W2159175300 @default.
• W2020461753 cites W2168769600 @default.
• W2020461753 cites W4206229011 @default.
• W2020461753 cites W4248714983 @default.
• W2020461753 cites W595159355 @default.
• W2020461753 doi "https://doi.org/10.1007/s00126-010-0324-5" @default.
• W2020461753 hasPublicationYear "2011" @default.
• W2020461753 type Work @default.
• W2020461753 sameAs 2020461753 @default.
• W2020461753 citedByCount "31" @default.
• W2020461753 countsByYear W20204617532012 @default.
• W2020461753 countsByYear W20204617532013 @default.
• W2020461753 countsByYear W20204617532014 @default.
• W2020461753 countsByYear W20204617532015 @default.
• W2020461753 countsByYear W20204617532016 @default.
• W2020461753 countsByYear W20204617532017 @default.
• W2020461753 countsByYear W20204617532018 @default.
• W2020461753 countsByYear W20204617532019 @default.
• W2020461753 countsByYear W20204617532020 @default.
• W2020461753 countsByYear W20204617532021 @default.
• W2020461753 countsByYear W20204617532022 @default.
• W2020461753 countsByYear W20204617532023 @default.
• W2020461753 crossrefType "journal-article" @default.
• W2020461753 hasAuthorship W2020461753A5019383410 @default.
• W2020461753 hasAuthorship W2020461753A5029930846 @default.
• W2020461753 hasAuthorship W2020461753A5044198268 @default.
• W2020461753 hasAuthorship W2020461753A5056693792 @default.
• W2020461753 hasAuthorship W2020461753A5083338748 @default.
• W2020461753 hasAuthorship W2020461753A5089728816 @default.
• W2020461753 hasBestOaLocation W20204617532 @default.
• W2020461753 hasConcept C111696902 @default.
• W2020461753 hasConcept C118552586 @default.
• W2020461753 hasConcept C120806208 @default.
• W2020461753 hasConcept C127313418 @default.
• W2020461753 hasConcept C151730666 @default.
• W2020461753 hasConcept C154401813 @default.
• W2020461753 hasConcept C156622251 @default.
• W2020461753 hasConcept C15744967 @default.
• W2020461753 hasConcept C159390177 @default.
• W2020461753 hasConcept C159750122 @default.
• W2020461753 hasConcept C160776313 @default.
• W2020461753 hasConcept C17409809 @default.
• W2020461753 hasConcept C178790620 @default.
• W2020461753 hasConcept C185592680 @default.
• W2020461753 hasConcept C192241223 @default.
• W2020461753 hasConcept C199289684 @default.
• W2020461753 hasConcept C26687426 @default.
• W2020461753 hasConcept C2776062231 @default.
• W2020461753 hasConcept C2776152364 @default.
• W2020461753 hasConcept C2776268066 @default.
• W2020461753 hasConcept C2777202286 @default.
• W2020461753 hasConcept C2779526359 @default.
• W2020461753 hasConcept C2780596425 @default.
• W2020461753 hasConcept C2781139676 @default.
• W2020461753 hasConcept C2781427754 @default.
• W2020461753 hasConcept C525849907 @default.
• W2020461753 hasConceptScore W2020461753C111696902 @default.
• W2020461753 hasConceptScore W2020461753C118552586 @default.
• W2020461753 hasConceptScore W2020461753C120806208 @default.

• next