Matches in SemOpenAlex for { <https://semopenalex.org/work/W1982328597> ?p ?o ?g. }
Showing items 1 to 93 of
93
with 100 items per page.
- W1982328597 endingPage "427" @default.
- W1982328597 startingPage "413" @default.
- W1982328597 abstract "The deposit of dawsonite and realgar–orpiment in the Koman area, northern Albania, is aligned along the NE–SW-trending tectonic line joining the Krasta–Cukal and Mirdita structural-tectonic zones. The deposit contains the following main paragenet ic assemblages: i) marcasite – greigite (Fe-sulfide stage), ii) stibnite – realgar – orpiment (As–Sb-sulfide stage), iii) dolomite – calcite – dawsonite – aragonite – barite – gypsum (carbonate–sulfate stage), iv) native As – gibbsite (supergene stage). There was lithostratigraphic control of mineralization; carbonate-rich wallrocks reacted with the mineralizing fluids emanating from a bu ried magmatic body and migrating along Albanian transversal faults, rather than argillaceous lithotypes. Values of � 18 O and � 13 C indicate that dawsonite and hydrothermal dolomite are derived at the expense of carbonate rocks, which occur extensively in the stratigraphic sequence of the host rocks. The water:rock ratio during the carbonate–sulfate stage of deposition was probably small. Moreover, oxygen and carbon isotopic exchange during metasomatic transformation of the rocks, recrystallization and late involvement of groundwater, probably all occurred. The sulfur involved in realgar and orpiment deposition may be of magmatic origin, and there was enrichment of heavier S during late hydrothermal processes. Both marcasite and greigite have low Co/Ni values reflecting low-temperature conditions during their formation; the amount of As in the fluids was relatively high during both Fe- and As–Sb-sulfide stages of deposition. The wallrocks were the source of Al and Na involved in dawsonite deposition. Al, Na, K and Si were the elements most effectively leached from rocks during hydrothermal alteration." @default.
- W1982328597 created "2016-06-24" @default.
- W1982328597 creator A5023105644 @default.
- W1982328597 creator A5032180631 @default.
- W1982328597 creator A5054934589 @default.
- W1982328597 creator A5063541986 @default.
- W1982328597 creator A5083604694 @default.
- W1982328597 date "2003-04-01" @default.
- W1982328597 modified "2023-10-03" @default.
- W1982328597 title "THE KOMAN DAWSONITE AND REALGAR ORPIMENT DEPOSIT, NORTHERN ALBANIA: INFERENCES ON PROCESSES OF FORMATION" @default.
- W1982328597 cites W128244193 @default.
- W1982328597 cites W1487925322 @default.
- W1982328597 cites W1598453376 @default.
- W1982328597 cites W1600129654 @default.
- W1982328597 cites W1972273256 @default.
- W1982328597 cites W1974639733 @default.
- W1982328597 cites W1975321253 @default.
- W1982328597 cites W2012685041 @default.
- W1982328597 cites W2018093298 @default.
- W1982328597 cites W2019795776 @default.
- W1982328597 cites W2019797299 @default.
- W1982328597 cites W2028034535 @default.
- W1982328597 cites W2032763907 @default.
- W1982328597 cites W2039037006 @default.
- W1982328597 cites W2044343221 @default.
- W1982328597 cites W2046890912 @default.
- W1982328597 cites W2050109850 @default.
- W1982328597 cites W2052848232 @default.
- W1982328597 cites W2064235356 @default.
- W1982328597 cites W2077381422 @default.
- W1982328597 cites W2078320350 @default.
- W1982328597 cites W2101687391 @default.
- W1982328597 cites W2102967105 @default.
- W1982328597 cites W2116175163 @default.
- W1982328597 cites W2131946949 @default.
- W1982328597 cites W2141295458 @default.
- W1982328597 cites W2146260558 @default.
- W1982328597 cites W2147027979 @default.
- W1982328597 cites W2157100113 @default.
- W1982328597 cites W2161551235 @default.
- W1982328597 cites W2212178433 @default.
- W1982328597 cites W2319851954 @default.
- W1982328597 cites W2885299708 @default.
- W1982328597 cites W2910731972 @default.
- W1982328597 cites W3000063164 @default.
- W1982328597 cites W3125722252 @default.
- W1982328597 doi "https://doi.org/10.2113/gscanmin.41.2.413" @default.
- W1982328597 hasPublicationYear "2003" @default.
- W1982328597 type Work @default.
- W1982328597 sameAs 1982328597 @default.
- W1982328597 citedByCount "20" @default.
- W1982328597 countsByYear W19823285972012 @default.
- W1982328597 countsByYear W19823285972014 @default.
- W1982328597 countsByYear W19823285972016 @default.
- W1982328597 countsByYear W19823285972017 @default.
- W1982328597 countsByYear W19823285972021 @default.
- W1982328597 countsByYear W19823285972022 @default.
- W1982328597 countsByYear W19823285972023 @default.
- W1982328597 crossrefType "journal-article" @default.
- W1982328597 hasAuthorship W1982328597A5023105644 @default.
- W1982328597 hasAuthorship W1982328597A5032180631 @default.
- W1982328597 hasAuthorship W1982328597A5054934589 @default.
- W1982328597 hasAuthorship W1982328597A5063541986 @default.
- W1982328597 hasAuthorship W1982328597A5083604694 @default.
- W1982328597 hasConcept C127313418 @default.
- W1982328597 hasConcept C17409809 @default.
- W1982328597 hasConcept C199289684 @default.
- W1982328597 hasConcept C2778548315 @default.
- W1982328597 hasConceptScore W1982328597C127313418 @default.
- W1982328597 hasConceptScore W1982328597C17409809 @default.
- W1982328597 hasConceptScore W1982328597C199289684 @default.
- W1982328597 hasConceptScore W1982328597C2778548315 @default.
- W1982328597 hasIssue "2" @default.
- W1982328597 hasLocation W19823285971 @default.
- W1982328597 hasOpenAccess W1982328597 @default.
- W1982328597 hasPrimaryLocation W19823285971 @default.
- W1982328597 hasRelatedWork W1758497512 @default.
- W1982328597 hasRelatedWork W1987691177 @default.
- W1982328597 hasRelatedWork W2036099453 @default.
- W1982328597 hasRelatedWork W2040829098 @default.
- W1982328597 hasRelatedWork W2124105426 @default.
- W1982328597 hasRelatedWork W2349947565 @default.
- W1982328597 hasRelatedWork W2361911732 @default.
- W1982328597 hasRelatedWork W2538103680 @default.
- W1982328597 hasRelatedWork W3008763070 @default.
- W1982328597 hasRelatedWork W4235203013 @default.
- W1982328597 hasVolume "41" @default.
- W1982328597 isParatext "false" @default.
- W1982328597 isRetracted "false" @default.
- W1982328597 magId "1982328597" @default.
- W1982328597 workType "article" @default.