Origin and significance of calcite-marcasite-pyrite mineralisation in siliciclastic Lower Carboniferous rocks, eastern margin of the Bohemian massif, Czech Republic.

KUČEROVÁ CHARVÁTOVÁ, Klára, Jan KUČERA and Zdeněk DOLNÍČEK. Origin and significance of calcite-marcasite-pyrite mineralisation in siliciclastic Lower Carboniferous rocks, eastern margin of the Bohemian massif, Czech Republic. Berlin: Springer-Verlag, 2005, 1600 pp. 1. ISBN 3-540-27945-8.

Basic information

Original name

Origin and significance of calcite-marcasite-pyrite mineralisation in siliciclastic Lower Carboniferous rocks, eastern margin of the Bohemian massif, Czech Republic.

Name in Czech

Původ a význam kalcit-markazit-pyritové mineralizace v siliciklastických horninách spodního karbonu na východním okraji Českého masivu, Česká republika.

Authors

KUČEROVÁ CHARVÁTOVÁ, Klára, Jan KUČERA and Zdeněk DOLNÍČEK

Edition

Berlin, 1600 pp. 1, 2005

Publisher

Springer-Verlag

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Other information

Language

English

Type of outcome

Odborná kniha

Field of Study

10500 1.5. Earth and related environmental sciences

Confidentiality degree

není předmětem státního či obchodního tajemství

Organization unit

Faculty of Science

ISBN

3-540-27945-8

UT WoS

000237245800037

Keywords in English

Bohemian Massif; calcite-marcasite mineralisation; stable isotopes; fluid inclusions

Tags

Bohemian massif, calcite-marcasite mineralisation, fluid inclusions, Stable Isotopes

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Abstract

V originále

Field and petrographic observations combined with fluid inclusion measurements, geochemical data, and stable and radiogenic isotope results place important constraints on the genesis of calcite-marcasite-pyrite veinlets located in the Lower Carboniferous siliciclastic rocks of the Nízký Jeseník Upland. These data suggest that the veinlets formed from hydrothermal fluids derived from marine water that migrated, along with petroleum, out of the Carpathian Foredeep in Miocene time.