Origin and significance of calcite-marcasite-pyrite mineralisation in siliciclastic Lower Carboniferous rocks, eastern margin of the Bohemian Massif, Czech Republic
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F05%3A00010006" target="_blank" >RIV/61989592:15310/05:00010006 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Origin and significance of calcite-marcasite-pyrite mineralisation in siliciclastic Lower Carboniferous rocks, eastern margin of the Bohemian Massif, Czech Republic
Original language description
Field and petrographic observations combined with fluid inclusion measurements, geochemical data, and stable and radiogenic isotope resultsplace important constraints on the genesis of calcite-marcasite-pyrite veinlets located in the Lower Carboniferoussiliciclastic 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.
Czech name
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Czech description
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Classification
Type
D - Article in proceedings
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
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Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2005
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Article name in the collection
Mineral Deposit Research: Meeting the Global Challenge. Proceedings of the eight biennial SGA meeting Beijing, China, 18-21 August 2005
ISBN
3-540-27945-8
ISSN
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e-ISSN
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Number of pages
871
Pages from-to
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Publisher name
Springer
Place of publication
Heidelberg
Event location
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Event date
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Type of event by nationality
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UT code for WoS article
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