FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2066331331> ?p ?o ?g. }

• W2066331331 endingPage "591" @default.
• W2066331331 startingPage "583" @default.
• W2066331331 abstract "Abstract The Huize Zn-Pb- (Ag-Ge) district is a typical representative of the well-known medium-to large-sized carbonate-hosted Zn-Pb- (Ag-Ge) deposits, occurring in the Sichuan-Yunnan-Guizhou Pb-Zn Ore-forming Zone. Generally, fluid inclusions within calcite, one of the major gangue minerals, are dominated by two kinds of small (1–10 μm) inclusions including pure-liquid and liquid. The inclusions exist in concentrated groups along the crystal planes of the calcite. The ore-forming fluids containing Pb and Zn, which belong to the Na+-K+-Ca2+-Cl−-F− - SO2-4 type, are characterized by temperatures of 164–221°C, medium salinity in 5–10.8 wt% NaCl, and medium pressure at 410times105 to 661times105 Pa. The contents of Na+-K+ and Cl−-F−, and ratios of Na+/K+-Cl−/F− in fluid inclusions present good linearity. The ratios of Na+/K+ (4.66–6.71) and Cl−/F− (18.21–31.04) in the fluid inclusions of calcite are relatively high, while those of Na+/K+ (0.29–5.69) and Cl−/F− (5.00–26.0) in the inclusions of sphalerite and pyrite are relatively low. The ratio of Na+/K+ increases in accord with those of Cl−/F−, which indicates that ore-forming fluid of deep source participates in the mineralization. The waters of fluid inclusions have δD values from −43.5‰ to −55.4‰ of calcite. The δ18OV-SMOW values of the ore-forming fluids, calculated values, range from 17.09‰ to 18.56‰ of calcite and 17.80‰ to 23.14‰ for dolomite. δ3CV-PDB values range from −1.94‰ to −3.31‰ for calcite and −3.35‰ to 0.85‰ for the ore-bearing dolomite. These data better demonstrate that the ore-forming fluids were mainly derived from metamorphic water and magmatic hot fluid, in relation to the metamorphism of the Kunyang Group in the basement and magmatic hydrothermalism. The deposit itself might have resulted from ascending cycles of ore-forming fluid, enriched in Pb and Zn. The Huize Zn-Pb- (Ag-Ge) deposits related to carbonate-hosted Zn-Pb sulphides." @default.
• W2066331331 created "2016-06-24" @default.
• W2066331331 creator A5000554967 @default.
• W2066331331 creator A5004734492 @default.
• W2066331331 creator A5005585096 @default.
• W2066331331 creator A5044210709 @default.
• W2066331331 creator A5044288799 @default.
• W2066331331 creator A5046808100 @default.
• W2066331331 creator A5048946612 @default.
• W2066331331 creator A5087222691 @default.
• W2066331331 date "2010-09-07" @default.
• W2066331331 modified "2023-10-16" @default.
• W2066331331 title "Fluid Inclusions of Calcite and Sources of Ore-forming Fluids in the Huize Zn-Pb-(Ag-Ge) District, Yunnan, China" @default.
• W2066331331 cites W1970658925 @default.
• W2066331331 cites W1978288685 @default.
• W2066331331 cites W2001790553 @default.
• W2066331331 cites W2009399894 @default.
• W2066331331 cites W2012931482 @default.
• W2066331331 cites W2019151034 @default.
• W2066331331 cites W2021032724 @default.
• W2066331331 cites W2021241269 @default.
• W2066331331 cites W2071093988 @default.
• W2066331331 cites W2081149290 @default.
• W2066331331 cites W2089982870 @default.
• W2066331331 cites W2111967263 @default.
• W2066331331 cites W2134860114 @default.
• W2066331331 cites W2138580160 @default.
• W2066331331 cites W2159792889 @default.
• W2066331331 cites W2162439861 @default.
• W2066331331 cites W2170770997 @default.
• W2066331331 cites W2325001532 @default.
• W2066331331 doi "https://doi.org/10.1111/j.1755-6724.2004.tb00170.x" @default.
• W2066331331 hasPublicationYear "2010" @default.
• W2066331331 type Work @default.
• W2066331331 sameAs 2066331331 @default.
• W2066331331 citedByCount "14" @default.
• W2066331331 countsByYear W20663313312013 @default.
• W2066331331 countsByYear W20663313312014 @default.
• W2066331331 countsByYear W20663313312015 @default.
• W2066331331 countsByYear W20663313312020 @default.
• W2066331331 countsByYear W20663313312022 @default.
• W2066331331 countsByYear W20663313312023 @default.
• W2066331331 crossrefType "journal-article" @default.
• W2066331331 hasAuthorship W2066331331A5000554967 @default.
• W2066331331 hasAuthorship W2066331331A5004734492 @default.
• W2066331331 hasAuthorship W2066331331A5005585096 @default.
• W2066331331 hasAuthorship W2066331331A5044210709 @default.
• W2066331331 hasAuthorship W2066331331A5044288799 @default.
• W2066331331 hasAuthorship W2066331331A5046808100 @default.
• W2066331331 hasAuthorship W2066331331A5048946612 @default.
• W2066331331 hasAuthorship W2066331331A5087222691 @default.
• W2066331331 hasConcept C111696902 @default.
• W2066331331 hasConcept C127313418 @default.
• W2066331331 hasConcept C159390177 @default.
• W2066331331 hasConcept C159750122 @default.
• W2066331331 hasConcept C17409809 @default.
• W2066331331 hasConcept C191897082 @default.
• W2066331331 hasConcept C192562407 @default.
• W2066331331 hasConcept C199289684 @default.
• W2066331331 hasConcept C2776062231 @default.
• W2066331331 hasConcept C2776152364 @default.
• W2066331331 hasConcept C2776268066 @default.
• W2066331331 hasConcept C2779870107 @default.
• W2066331331 hasConcept C2780191791 @default.
• W2066331331 hasConcept C2780659211 @default.
• W2066331331 hasConcept C7028197 @default.
• W2066331331 hasConceptScore W2066331331C111696902 @default.
• W2066331331 hasConceptScore W2066331331C127313418 @default.
• W2066331331 hasConceptScore W2066331331C159390177 @default.
• W2066331331 hasConceptScore W2066331331C159750122 @default.
• W2066331331 hasConceptScore W2066331331C17409809 @default.
• W2066331331 hasConceptScore W2066331331C191897082 @default.
• W2066331331 hasConceptScore W2066331331C192562407 @default.
• W2066331331 hasConceptScore W2066331331C199289684 @default.
• W2066331331 hasConceptScore W2066331331C2776062231 @default.
• W2066331331 hasConceptScore W2066331331C2776152364 @default.
• W2066331331 hasConceptScore W2066331331C2776268066 @default.
• W2066331331 hasConceptScore W2066331331C2779870107 @default.
• W2066331331 hasConceptScore W2066331331C2780191791 @default.
• W2066331331 hasConceptScore W2066331331C2780659211 @default.
• W2066331331 hasConceptScore W2066331331C7028197 @default.
• W2066331331 hasIssue "2" @default.
• W2066331331 hasLocation W20663313311 @default.
• W2066331331 hasOpenAccess W2066331331 @default.
• W2066331331 hasPrimaryLocation W20663313311 @default.
• W2066331331 hasRelatedWork W2049803147 @default.
• W2066331331 hasRelatedWork W2134656900 @default.
• W2066331331 hasRelatedWork W2270654036 @default.
• W2066331331 hasRelatedWork W240046313 @default.
• W2066331331 hasRelatedWork W2623874265 @default.
• W2066331331 hasRelatedWork W2955366896 @default.
• W2066331331 hasRelatedWork W3045316441 @default.
• W2066331331 hasRelatedWork W312586180 @default.
• W2066331331 hasRelatedWork W3152158765 @default.
• W2066331331 hasRelatedWork W2416111802 @default.
• W2066331331 hasVolume "78" @default.
• W2066331331 isParatext "false" @default.
• W2066331331 isRetracted "false" @default.

• next