Matches in SemOpenAlex for { <https://semopenalex.org/work/W3080168691> ?p ?o ?g. }
- W3080168691 endingPage "748" @default.
- W3080168691 startingPage "748" @default.
- W3080168691 abstract "The South China Block (SCB) is a globally important metallogenic district containing numerous W-Sn deposits. Extensive studies of W-polymetallic deposits in this region have greatly improved our understanding of the petrogenesis, geochronology and metallogenesis of these systems. However, studies on the mobilization of ore-forming elements between mineralization- and alteration-related minerals using in situ analyses are rare. Using laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS), we analyzed W, Pb, Mo and Bi concentrations in silicate minerals and scheelite from granites and skarns associated with the Shizhuyuan W-polymetallic deposit in the Nanling Range in the SCB. Data show that muscovitized biotite in granites contains high W contents. Pb mainly occurs in K-feldspar and plagioclase in granites and epidote and scheelite in skarns. Bi mainly occurs in epidote in skarns. Scheelite in skarns contains high W and Mo contents. Pb isomorphously substitutes K or Ca in silicate minerals and scheelite. W isomorphously substitutes Ti in biotite. Mo isomorphously substitutes W in scheelite and occurs as W-bearing submicroscopic inclusions in minerals with low contents. Bi isomorphously substitutes Pb when the Pb content is relatively high and occurs as Bi-bearing micro or submicroscopic inclusions in minerals when the Pb content is low. Biotite and feldspar are altered in a magmatic-hydrothermal process, W enriched in biotite, Pb enriched in feldspar and the W-, Pb-, Mo- and Bi-bearing submicroscopic inclusions are excluded from minerals and released to the magmatic-hydrothermal fluids. Large amounts of W are precipitated in scheelite when the fluids come in contact with carbonate rocks to form skarn, while a few contents of Pb, Mo and Bi are distributed in skarn minerals. Thus, large amounts of Pb, Mo, Bi and residual W remain in the fluids, which results in the formation of a W-Sn-Mo-Bi massive skarn ore." @default.
- W3080168691 created "2020-09-01" @default.
- W3080168691 creator A5031749803 @default.
- W3080168691 creator A5064899276 @default.
- W3080168691 creator A5072734824 @default.
- W3080168691 creator A5074644089 @default.
- W3080168691 creator A5084263315 @default.
- W3080168691 date "2020-08-24" @default.
- W3080168691 modified "2023-10-13" @default.
- W3080168691 title "LA-ICP-MS Analysis of Minerals from the Shizhuyuan W-Polymetallic Deposit, South China: Implications for Mineralization of Pb, W, Mo and Bi" @default.
- W3080168691 cites W1541910269 @default.
- W3080168691 cites W1596437162 @default.
- W3080168691 cites W1964432997 @default.
- W3080168691 cites W1968583876 @default.
- W3080168691 cites W1975700771 @default.
- W3080168691 cites W1987844446 @default.
- W3080168691 cites W1996328804 @default.
- W3080168691 cites W2008042768 @default.
- W3080168691 cites W2009421219 @default.
- W3080168691 cites W2013366222 @default.
- W3080168691 cites W2013535259 @default.
- W3080168691 cites W2017095019 @default.
- W3080168691 cites W2045860233 @default.
- W3080168691 cites W2051805987 @default.
- W3080168691 cites W2059058479 @default.
- W3080168691 cites W2076440051 @default.
- W3080168691 cites W2082164364 @default.
- W3080168691 cites W2090914108 @default.
- W3080168691 cites W2092778941 @default.
- W3080168691 cites W2093503795 @default.
- W3080168691 cites W2120908352 @default.
- W3080168691 cites W2122338764 @default.
- W3080168691 cites W2126884842 @default.
- W3080168691 cites W2133042542 @default.
- W3080168691 cites W2146959098 @default.
- W3080168691 cites W2154966130 @default.
- W3080168691 cites W2155803469 @default.
- W3080168691 cites W2317598683 @default.
- W3080168691 cites W2326878849 @default.
- W3080168691 cites W2328037678 @default.
- W3080168691 cites W2403988321 @default.
- W3080168691 cites W2411603221 @default.
- W3080168691 cites W2415081471 @default.
- W3080168691 cites W2435741850 @default.
- W3080168691 cites W2460337695 @default.
- W3080168691 cites W2535653206 @default.
- W3080168691 cites W2568656431 @default.
- W3080168691 cites W2771382009 @default.
- W3080168691 cites W2778083169 @default.
- W3080168691 cites W2790776546 @default.
- W3080168691 cites W2790995103 @default.
- W3080168691 cites W2791236146 @default.
- W3080168691 cites W2807179416 @default.
- W3080168691 cites W2813907669 @default.
- W3080168691 cites W2884081006 @default.
- W3080168691 cites W2886103464 @default.
- W3080168691 cites W2911869590 @default.
- W3080168691 cites W2917370678 @default.
- W3080168691 cites W2949465872 @default.
- W3080168691 cites W2951188712 @default.
- W3080168691 cites W2955903816 @default.
- W3080168691 cites W2970730650 @default.
- W3080168691 cites W2977423849 @default.
- W3080168691 cites W2978552685 @default.
- W3080168691 cites W2982201360 @default.
- W3080168691 cites W2982864600 @default.
- W3080168691 cites W2995056917 @default.
- W3080168691 cites W2998353435 @default.
- W3080168691 cites W3002507091 @default.
- W3080168691 cites W3024762294 @default.
- W3080168691 doi "https://doi.org/10.3390/min10090748" @default.
- W3080168691 hasPublicationYear "2020" @default.
- W3080168691 type Work @default.
- W3080168691 sameAs 3080168691 @default.
- W3080168691 citedByCount "2" @default.
- W3080168691 countsByYear W30801686912022 @default.
- W3080168691 countsByYear W30801686912023 @default.
- W3080168691 crossrefType "journal-article" @default.
- W3080168691 hasAuthorship W3080168691A5031749803 @default.
- W3080168691 hasAuthorship W3080168691A5064899276 @default.
- W3080168691 hasAuthorship W3080168691A5072734824 @default.
- W3080168691 hasAuthorship W3080168691A5074644089 @default.
- W3080168691 hasAuthorship W3080168691A5084263315 @default.
- W3080168691 hasBestOaLocation W30801686912 @default.
- W3080168691 hasConcept C111696902 @default.
- W3080168691 hasConcept C127313418 @default.
- W3080168691 hasConcept C151730666 @default.
- W3080168691 hasConcept C156622251 @default.
- W3080168691 hasConcept C159390177 @default.
- W3080168691 hasConcept C159750122 @default.
- W3080168691 hasConcept C165205528 @default.
- W3080168691 hasConcept C17409809 @default.
- W3080168691 hasConcept C178790620 @default.
- W3080168691 hasConcept C185592680 @default.
- W3080168691 hasConcept C195843664 @default.
- W3080168691 hasConcept C195845463 @default.
- W3080168691 hasConcept C199289684 @default.
- W3080168691 hasConcept C2776152364 @default.