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Fluorite and related fluids in the Karkonosze granitoid pluton, SW Poland

cris.lastimport.scopus2024-02-12T19:42:05Z
dc.abstract.enFluorite mineralization was studied in the Variscan granitoid Karkonosze pluton in the northern part of the Bohemian massif (Lower Silesia, Poland). Fluid inclusions in fluorite and quartz were investigated by the following methods: heating and freezing on an immersion microscope stage, spectrophotometric and electron probe analysis, calcination and water leachate. The parent fluids of fluorite were of the Na-Ca-Cl type with a low CO₂ content. The fluoride ions had sources in the pluton and in its host rocks. Fluid inclusion observations provide evidence of various post-formation alteration. such as refilling, partition, cracking, migration, expulsion or vacuole modification from irregular to cubic habit. A final model of fluorite origin and parent fluid evolution is presented.
dc.affiliationUniwersytet Warszawski
dc.contributor.authorMatyszczak, Witold
dc.contributor.authorKozłowski, Andrzej
dc.date.accessioned2024-01-25T01:14:02Z
dc.date.available2024-01-25T01:14:02Z
dc.date.issued2022
dc.description.financePublikacja bezkosztowa
dc.description.number1
dc.description.volume72
dc.identifier.doi10.24425/AGP.2021.137710
dc.identifier.issn0001-5709
dc.identifier.urihttps://repozytorium.uw.edu.pl//handle/item/107310
dc.identifier.weblinkhttps://geojournals.pgi.gov.pl/agp/article/view/33309
dc.languageeng
dc.pbn.affiliationearth and related environmental sciences
dc.relation.ispartofActa Geologica Polonica
dc.relation.pages9-31
dc.rightsClosedAccess
dc.sciencecloudnosend
dc.subject.enKarkonosze pluton
dc.subject.enVariscan granitoid
dc.subject.enPegmatite
dc.subject.enFluorite
dc.subject.enFluid inclusions
dc.subject.enInclusion alterations
dc.subject.enPost-magmatic fluids.
dc.titleFluorite and related fluids in the Karkonosze granitoid pluton, SW Poland
dc.typeJournalArticle
dspace.entity.typePublication