FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2034303241> ?p ?o ?g. }

• W2034303241 endingPage "209" @default.
• W2034303241 startingPage "195" @default.
• W2034303241 abstract "Abstract The significance of isotopic data on constraining the physical conditions of fluid-rock interaction and mineralization processes in carbonate rocks is discussed, based on the example of barite-tetrahedrite mineralization in Lower Devonian platform carbonates of the Western Greywacke Zone (Tyrol, Austria). Available strontium, oxygen, carbon and sulfur isotopic data are complemented with oxygen isotopic data for barite. Barites are homogeneous in δ18OV-SMOW and δ34SCDT with values of ∼ + 15.4 and ∼ + 23.5‰ , respectively. Their 87 Sr 86 Sr ratios vary between 0.7128 and 0.7113 for the first generation and between 0.7117 and 0.7123 for younger remobilization. The dolomitic host rock shows a significant variation in Sr, O and C isotopic composition between non-mineralized and mineralized zones: 87 Sr 86 Sr ratios vary between 0.7076 and 0.7133, δ18OV-SMOW-values between +28.11 and +20.65‰, and δ13CPDB-values between −1.15 and + 3.06‰. Fluid/rock volume ratios on the order of 1.3–3.2 are calculated for open-system behaviour by modelling Sr, O and C isotopic shifting capacities. The isotope data combined with other geological evidence support the following genetic model: Subsequent to synsedimentary sulfide mineralization during an Early Devonian rifting stage, collision tectonics in Carboniferous time led to the expulsion of Ba- and Sr-rich orogenic brines, which evolved from metamorphic fluids consisting essentially of H2O and some CH4, into an external sedimentary fold-and-thrust belt. The brines remobilized the synsedimentary sulfides, mixed with meteoric waters in the platform carbonates, reacted with evaporitic horizons and finally caused the recrystallization of dolomite and the precipitation of Sr-rich barite in structurally weak zones at ∼ 70–130°C. During the later Alpine orogeny supergene oxidation products were formed, and sulfates, sulfides and carbonates were further remobilized into late faults and fractures." @default.
• W2034303241 created "2016-06-24" @default.
• W2034303241 creator A5087827547 @default.
• W2034303241 date "1991-06-01" @default.
• W2034303241 modified "2023-09-26" @default.
• W2034303241 title "Isotopic constraints on fluid/rock ratios in carbonate rocks: Barite-sulfide mineralization in the Schwaz Dolomite, Tyrol (Eastern Alps, Austria)" @default.
• W2034303241 cites W1631121278 @default.
• W2034303241 cites W1647010324 @default.
• W2034303241 cites W1970196312 @default.
• W2034303241 cites W1987445809 @default.
• W2034303241 cites W1998426957 @default.
• W2034303241 cites W2014945279 @default.
• W2034303241 cites W2019795776 @default.
• W2034303241 cites W2034309465 @default.
• W2034303241 cites W2039573271 @default.
• W2034303241 cites W2045295561 @default.
• W2034303241 cites W2067685831 @default.
• W2034303241 cites W2072429119 @default.
• W2034303241 cites W2078378096 @default.
• W2034303241 cites W2095563214 @default.
• W2034303241 cites W2099876786 @default.
• W2034303241 cites W2164220172 @default.
• W2034303241 cites W2319917352 @default.
• W2034303241 cites W2320582823 @default.
• W2034303241 cites W2517847674 @default.
• W2034303241 cites W2913350784 @default.
• W2034303241 doi "https://doi.org/10.1016/0009-2541(91)90100-6" @default.
• W2034303241 hasPublicationYear "1991" @default.
• W2034303241 type Work @default.
• W2034303241 sameAs 2034303241 @default.
• W2034303241 citedByCount "11" @default.
• W2034303241 countsByYear W20343032412013 @default.
• W2034303241 countsByYear W20343032412020 @default.
• W2034303241 countsByYear W20343032412021 @default.
• W2034303241 countsByYear W20343032412022 @default.
• W2034303241 crossrefType "journal-article" @default.
• W2034303241 hasAuthorship W2034303241A5087827547 @default.
• W2034303241 hasConcept C111696902 @default.
• W2034303241 hasConcept C127313418 @default.
• W2034303241 hasConcept C159390177 @default.
• W2034303241 hasConcept C159750122 @default.
• W2034303241 hasConcept C17409809 @default.
• W2034303241 hasConcept C178790620 @default.
• W2034303241 hasConcept C185592680 @default.
• W2034303241 hasConcept C191897082 @default.
• W2034303241 hasConcept C192562407 @default.
• W2034303241 hasConcept C19320362 @default.
• W2034303241 hasConcept C199289684 @default.
• W2034303241 hasConcept C2780181037 @default.
• W2034303241 hasConcept C2780596425 @default.
• W2034303241 hasConcept C2780659211 @default.
• W2034303241 hasConcept C6494504 @default.
• W2034303241 hasConceptScore W2034303241C111696902 @default.
• W2034303241 hasConceptScore W2034303241C127313418 @default.
• W2034303241 hasConceptScore W2034303241C159390177 @default.
• W2034303241 hasConceptScore W2034303241C159750122 @default.
• W2034303241 hasConceptScore W2034303241C17409809 @default.
• W2034303241 hasConceptScore W2034303241C178790620 @default.
• W2034303241 hasConceptScore W2034303241C185592680 @default.
• W2034303241 hasConceptScore W2034303241C191897082 @default.
• W2034303241 hasConceptScore W2034303241C192562407 @default.
• W2034303241 hasConceptScore W2034303241C19320362 @default.
• W2034303241 hasConceptScore W2034303241C199289684 @default.
• W2034303241 hasConceptScore W2034303241C2780181037 @default.
• W2034303241 hasConceptScore W2034303241C2780596425 @default.
• W2034303241 hasConceptScore W2034303241C2780659211 @default.
• W2034303241 hasConceptScore W2034303241C6494504 @default.
• W2034303241 hasIssue "3-4" @default.
• W2034303241 hasLocation W20343032411 @default.
• W2034303241 hasOpenAccess W2034303241 @default.
• W2034303241 hasPrimaryLocation W20343032411 @default.
• W2034303241 hasRelatedWork W144520048 @default.
• W2034303241 hasRelatedWork W1969761773 @default.
• W2034303241 hasRelatedWork W2030204966 @default.
• W2034303241 hasRelatedWork W2038889380 @default.
• W2034303241 hasRelatedWork W2117463334 @default.
• W2034303241 hasRelatedWork W2169242934 @default.
• W2034303241 hasRelatedWork W2385515337 @default.
• W2034303241 hasRelatedWork W3149861528 @default.
• W2034303241 hasRelatedWork W4285005292 @default.
• W2034303241 hasRelatedWork W4285046152 @default.
• W2034303241 hasVolume "90" @default.
• W2034303241 isParatext "false" @default.
• W2034303241 isRetracted "false" @default.
• W2034303241 magId "2034303241" @default.
• W2034303241 workType "article" @default.