FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2092738643> ?p ?o ?g. }

• W2092738643 endingPage "182" @default.
• W2092738643 startingPage "153" @default.
• W2092738643 abstract "The Bajiazi Zn–Pb–Ag skarn deposit is located in northwest Liaoning Province, China. The orebodies occur in a contact zone between Yanshanian (170–177.4 Ma) quartz monzodiorite and Middle Proterozoic dolomitic marble of the Gaoyuzhuang Formation as well as along the NW- and NS-trending fault systems in carbonate wall rocks. Metasomatic mineralization zoning in the deposit is very pronounced. From the intrusive contact zone to dolomitic marble along the NW-trending fault system, three ore-bearing skarn zones may be distinguished: magnesian skarn zone (Fe–Mo)→manganoan–magnesian skarn zone (Cu–S–Fe–Pb–Zn–Ag)→manganoan skarn zone (Zn–Pb–Ag). Magnesian skarn is composed of diopside, forsterite, tremolite, spinel, phlogopite, chondrodite, and serpentine, accompanied by magnetite, pyrite, and molybdenite. Manganoan–magnesian skarn consists mainly of manganoan diopside, manganoan tremolite, mangano-anthophyllite, and manganocummingtonite with minor spessartine and pyroxmangite, The associated ore minerals are pyrite, pyrrhotite, and chalcopyrite, with subordinate magnetite, sphalerite, galena, and Ag-bearing minerals. Manganoan skarn is composed chiefly of spessartine, pyroxmangite, magnesian rhodonite, manganocummingtonite, and manganopyrosmalite, with the associated ore minerals sphalerite, galena, alabandite, and Ag-bearing minerals. Studies of fluid inclusions and S, Pb, O, and H isotopic compositions suggest that ore-bearing fluids flowed from the deep contact zone of the intrusion in the southeast to the shallow depth in the northwest with decreasing temperatures, oxidation state, and increasing pH. When the ore-bearing fluids migrated, their frontal part constantly reacted with the dolomitic carbonate wall rocks to form different types of skarn and mineralization. Sulfur and lead (zinc) were mainly derived from the deep lower crust, while the Middle Proterozoic wall rocks may have provided most Al, Si, Mg, Ca, and Mn for the formation of skarns. The zonal model reflecting the variations in metallization assemblage, skarn mineralogy, composition, δ34S isotope values, and fluid inclusion characteristics can be used as a guide to exploration for Zn–Pb–Ag skarn deposits." @default.
• W2092738643 created "2016-06-24" @default.
• W2092738643 creator A5049592669 @default.
• W2092738643 creator A5053368014 @default.
• W2092738643 creator A5056618863 @default.
• W2092738643 creator A5082043001 @default.
• W2092738643 date "2003-10-01" @default.
• W2092738643 modified "2023-10-01" @default.
• W2092738643 title "Geology, mineralogy, geochemistry, and zonation of the Bajiazi dolostone-hosted Zn–Pb–Ag skarn deposit, Liaoning Province, China" @default.
• W2092738643 cites W1969185593 @default.
• W2092738643 cites W1970658925 @default.
• W2092738643 cites W1986213475 @default.
• W2092738643 cites W1996361224 @default.
• W2092738643 cites W2005121896 @default.
• W2092738643 cites W2007105153 @default.
• W2092738643 cites W2014541757 @default.
• W2092738643 cites W2019385064 @default.
• W2092738643 cites W2042114555 @default.
• W2092738643 cites W2050926313 @default.
• W2092738643 cites W2065131379 @default.
• W2092738643 cites W2077675035 @default.
• W2092738643 cites W2090757504 @default.
• W2092738643 cites W2108193971 @default.
• W2092738643 cites W2111968610 @default.
• W2092738643 cites W2129998778 @default.
• W2092738643 cites W2139367651 @default.
• W2092738643 cites W2141295458 @default.
• W2092738643 cites W2150954290 @default.
• W2092738643 doi "https://doi.org/10.1016/s0169-1368(03)00034-9" @default.
• W2092738643 hasPublicationYear "2003" @default.
• W2092738643 type Work @default.
• W2092738643 sameAs 2092738643 @default.
• W2092738643 citedByCount "30" @default.
• W2092738643 countsByYear W20927386432012 @default.
• W2092738643 countsByYear W20927386432013 @default.
• W2092738643 countsByYear W20927386432014 @default.
• W2092738643 countsByYear W20927386432015 @default.
• W2092738643 countsByYear W20927386432017 @default.
• W2092738643 countsByYear W20927386432018 @default.
• W2092738643 countsByYear W20927386432019 @default.
• W2092738643 countsByYear W20927386432020 @default.
• W2092738643 countsByYear W20927386432021 @default.
• W2092738643 countsByYear W20927386432022 @default.
• W2092738643 countsByYear W20927386432023 @default.
• W2092738643 crossrefType "journal-article" @default.
• W2092738643 hasAuthorship W2092738643A5049592669 @default.
• W2092738643 hasAuthorship W2092738643A5053368014 @default.
• W2092738643 hasAuthorship W2092738643A5056618863 @default.
• W2092738643 hasAuthorship W2092738643A5082043001 @default.
• W2092738643 hasConcept C111696902 @default.
• W2092738643 hasConcept C127313418 @default.
• W2092738643 hasConcept C151730666 @default.
• W2092738643 hasConcept C159390177 @default.
• W2092738643 hasConcept C159750122 @default.
• W2092738643 hasConcept C167919410 @default.
• W2092738643 hasConcept C17409809 @default.
• W2092738643 hasConcept C195843664 @default.
• W2092738643 hasConcept C199289684 @default.
• W2092738643 hasConcept C2776062231 @default.
• W2092738643 hasConcept C2776152364 @default.
• W2092738643 hasConcept C2776268066 @default.
• W2092738643 hasConcept C2777163820 @default.
• W2092738643 hasConcept C2777844515 @default.
• W2092738643 hasConcept C2778357522 @default.
• W2092738643 hasConcept C2779870107 @default.
• W2092738643 hasConcept C2781139676 @default.
• W2092738643 hasConcept C2781366471 @default.
• W2092738643 hasConcept C67236022 @default.
• W2092738643 hasConceptScore W2092738643C111696902 @default.
• W2092738643 hasConceptScore W2092738643C127313418 @default.
• W2092738643 hasConceptScore W2092738643C151730666 @default.
• W2092738643 hasConceptScore W2092738643C159390177 @default.
• W2092738643 hasConceptScore W2092738643C159750122 @default.
• W2092738643 hasConceptScore W2092738643C167919410 @default.
• W2092738643 hasConceptScore W2092738643C17409809 @default.
• W2092738643 hasConceptScore W2092738643C195843664 @default.
• W2092738643 hasConceptScore W2092738643C199289684 @default.
• W2092738643 hasConceptScore W2092738643C2776062231 @default.
• W2092738643 hasConceptScore W2092738643C2776152364 @default.
• W2092738643 hasConceptScore W2092738643C2776268066 @default.
• W2092738643 hasConceptScore W2092738643C2777163820 @default.
• W2092738643 hasConceptScore W2092738643C2777844515 @default.
• W2092738643 hasConceptScore W2092738643C2778357522 @default.
• W2092738643 hasConceptScore W2092738643C2779870107 @default.
• W2092738643 hasConceptScore W2092738643C2781139676 @default.
• W2092738643 hasConceptScore W2092738643C2781366471 @default.
• W2092738643 hasConceptScore W2092738643C67236022 @default.
• W2092738643 hasIssue "3-4" @default.
• W2092738643 hasLocation W20927386431 @default.
• W2092738643 hasOpenAccess W2092738643 @default.
• W2092738643 hasPrimaryLocation W20927386431 @default.
• W2092738643 hasRelatedWork W2065969677 @default.
• W2092738643 hasRelatedWork W2092738643 @default.
• W2092738643 hasRelatedWork W2386857744 @default.
• W2092738643 hasRelatedWork W2562019403 @default.
• W2092738643 hasRelatedWork W2888674363 @default.
• W2092738643 hasRelatedWork W2896832631 @default.
• W2092738643 hasRelatedWork W3126931700 @default.

• next