FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2056553520> ?p ?o ?g. }

• W2056553520 endingPage "1359" @default.
• W2056553520 startingPage "1343" @default.
• W2056553520 abstract "Wall-rock alteration at the Getchell underground deposit was examined to determine the effects of Au-bear-ing fluids on host lithologies and the relationship between K-bearing alteration minerals and Au deposition. The major, minor, and trace element geochemistry of highly altered and mineralized to unmineralized rocks from the Getchell deposit was quantified for more than 50 samples collected along 13 transects through calcareous siltstone and carbonaceous limestone and along one transect through a rhyodacite dike. Each transect in sedimentary rocks was collected along a single homogeneous bed that could be followed from high-grade ore to moderately altered rock or waste rock. Analyses were obtained for 39 elements, 10 oxides, and loss on ignition, using multiple techniques. Petrographic studies were integrated with geochemistry and X-ray diffraction and electron microbeam analyses to identify ore and alteration minerals and to correlate mineralogy with geochemical fluxes. Geochemical analyses indicate that Ti, Al, Zr, and Th behave as immobile elements. Immobility isocon diagrams show that significant Hg, Sb, Se, Te, Tl, and Cs are typically added to the wall rocks with Au. Fe is im-mobile in some transects, added to wall rocks in others, and removed from rhyodacite host rocks. Minor S and W are usually added to the rock, whereas minor Cu and Mo are variably added or removed. SiO 2 appears to be either added during alteration or remain constant. Elements that are consistently removed during alteration include Ca, Mn, Sr, and Sc and minor Mg, Ba, and K. Na was significantly removed from the rhyodacite. Au correlates positively with Ag, Hg, Sb, Se, Si, Te, and Tl and negatively with Ca, Mn, and Sc. Element fluxes correspond with observations of mineral abundances and show that sulfidation and decar-bonitization are spatially associated with gold mineralization. Au, Hg, Sb, Tl, Cu, and possibly Te and W were incorporated in trace element-rich pyrite as host-rock Fe was sulfidized. Fe was added to mineralized rocks in some transects, indicating that pyritization occurred in addition to sulfidation. Cs is a component of galkhaite, a trace mineral that is relatively common in some parts of the Getchell system. Decarbonitization removed as much as 95 wt percent calcite from mineralized rocks in some transects and is responsible for loss of Ca, Mn, Sr, and Sc. Although SiO 2 , As, and S are significantly added to Carlin-type systems, they do not appear as major added components in the isocon diagrams. This is because the halos for these components are much larger than the areas examined by the sample transects. X-ray diffraction analyses identified minerals in ore and waste samples and quantified clay minerals, including illite and montmorillonite. Kaolinite was not identified or is present in low abundances in both mineralized and unmineralized rocks. Montmorillonite does not correlate with gold and textures are consistent with pore-filling deposition of montmorillonite following Au deposition. Illite abundance exhibits a positive correlation with Au ( r 2 = 0.80). Intergrowths of illite with ore-stage pyrite support a genetic relationship between the two minerals and indicate that illite formed as part of the Au-related hydrothermal event. Mineral abundances and textures suggest that illite formed by alteration of K feldspar during Au deposition. Results show that dating of K-bearing phases in sedimentary rocks, other than illite, would provide ages unrelated to gold deposition." @default.
• W2056553520 created "2016-06-24" @default.
• W2056553520 creator A5024848814 @default.
• W2056553520 creator A5056907222 @default.
• W2056553520 date "2001-09-01" @default.
• W2056553520 modified "2023-10-14" @default.
• W2056553520 title "Alteration Associated with Gold Deposition at the Getchell Carlin-Type Gold Deposit, North-Central Nevada" @default.
• W2056553520 cites W1964733635 @default.
• W2056553520 cites W1965787070 @default.
• W2056553520 cites W1978293439 @default.
• W2056553520 cites W1982952195 @default.
• W2056553520 cites W1998027905 @default.
• W2056553520 cites W2008632542 @default.
• W2056553520 cites W2013599096 @default.
• W2056553520 cites W2034703277 @default.
• W2056553520 cites W2039802085 @default.
• W2056553520 cites W2040485378 @default.
• W2056553520 cites W2048170009 @default.
• W2056553520 cites W2054116202 @default.
• W2056553520 cites W2081461486 @default.
• W2056553520 cites W2097260812 @default.
• W2056553520 cites W2115673156 @default.
• W2056553520 cites W2132610652 @default.
• W2056553520 cites W2146371856 @default.
• W2056553520 cites W2152195282 @default.
• W2056553520 cites W2163737148 @default.
• W2056553520 cites W2165908138 @default.
• W2056553520 cites W3199363773 @default.
• W2056553520 cites W4211058671 @default.
• W2056553520 doi "https://doi.org/10.2113/gsecongeo.96.6.1343" @default.
• W2056553520 hasPublicationYear "2001" @default.
• W2056553520 type Work @default.
• W2056553520 sameAs 2056553520 @default.
• W2056553520 citedByCount "45" @default.
• W2056553520 countsByYear W20565535202012 @default.
• W2056553520 countsByYear W20565535202014 @default.
• W2056553520 countsByYear W20565535202015 @default.
• W2056553520 countsByYear W20565535202016 @default.
• W2056553520 countsByYear W20565535202017 @default.
• W2056553520 countsByYear W20565535202018 @default.
• W2056553520 countsByYear W20565535202019 @default.
• W2056553520 countsByYear W20565535202020 @default.
• W2056553520 countsByYear W20565535202021 @default.
• W2056553520 countsByYear W20565535202022 @default.
• W2056553520 countsByYear W20565535202023 @default.
• W2056553520 crossrefType "journal-article" @default.
• W2056553520 hasAuthorship W2056553520A5024848814 @default.
• W2056553520 hasAuthorship W2056553520A5056907222 @default.
• W2056553520 hasBestOaLocation W20565535202 @default.
• W2056553520 hasConcept C114793014 @default.
• W2056553520 hasConcept C127313418 @default.
• W2056553520 hasConcept C16674752 @default.
• W2056553520 hasConcept C17409809 @default.
• W2056553520 hasConcept C199289684 @default.
• W2056553520 hasConcept C2816523 @default.
• W2056553520 hasConcept C64297162 @default.
• W2056553520 hasConceptScore W2056553520C114793014 @default.
• W2056553520 hasConceptScore W2056553520C127313418 @default.
• W2056553520 hasConceptScore W2056553520C16674752 @default.
• W2056553520 hasConceptScore W2056553520C17409809 @default.
• W2056553520 hasConceptScore W2056553520C199289684 @default.
• W2056553520 hasConceptScore W2056553520C2816523 @default.
• W2056553520 hasConceptScore W2056553520C64297162 @default.
• W2056553520 hasIssue "6" @default.
• W2056553520 hasLocation W20565535201 @default.
• W2056553520 hasLocation W20565535202 @default.
• W2056553520 hasOpenAccess W2056553520 @default.
• W2056553520 hasPrimaryLocation W20565535201 @default.
• W2056553520 hasRelatedWork W1758497512 @default.
• W2056553520 hasRelatedWork W1987691177 @default.
• W2056553520 hasRelatedWork W2036099453 @default.
• W2056553520 hasRelatedWork W2040829098 @default.
• W2056553520 hasRelatedWork W2124105426 @default.
• W2056553520 hasRelatedWork W2349947565 @default.
• W2056553520 hasRelatedWork W2361911732 @default.
• W2056553520 hasRelatedWork W2380934447 @default.
• W2056553520 hasRelatedWork W2538103680 @default.
• W2056553520 hasRelatedWork W4235203013 @default.
• W2056553520 hasVolume "96" @default.
• W2056553520 isParatext "false" @default.
• W2056553520 isRetracted "false" @default.
• W2056553520 magId "2056553520" @default.
• W2056553520 workType "article" @default.