Post-magmatic hydrothermal mineralization associated with Cretaceous picrite (Outer Western Carpathians, Czech Republic): interaction between host rock and externally derived fluid
Published: Aug 2010
Pages: 327 - 339
DOI: https://doi.org/10.2478/v10096-010-0019-y
Authors: ZDENEK DOLNICEK, TOMAS URUBEK, KAMIL KROPAC
Abstract: Mineralogy, fluid inclusions, C, O, S, Sr isotopes and trace elements have been studied in amygdule and vein mineralization hosted by the Lower Cretaceous effusive picrite at Honcova hurka (Silesian Unit, Flysch Belt of the Outer Western Carpathians). Besides dominating dolomite, magnesite, siderite, quartz, calcite, chlorite, glauconite, fluorite, barite, pyrite and millerite were also identified. The parent fluids are characterized by low temperatures (
Keywords: Outer Western Carpathians, stable isotopes, strontium isotopes, fluid-rock interaction, veins, fluid inclusions, amygdules, REE, picrite
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