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Methane Degassing and Exhumation of the Tertiary Accretionary Complex and Fore-arc Basin of the Western Carpathians
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Geolines
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January 1, 2004
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Copyright informationCopyright Institute of Geology 2004. Provided by ProQuest LLC. (Hide copyright information)
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Cretaceous-Oligocene flysch of the Western Carpathians contains mineralised joints filled with several generations of calcite and quartz. Composite textures of the mineral infillings reflect a multi-stage development coincidental with diagenesis, syn-sedimentary folding, thrusting, and regional collapse of the Outer Carpathians (Swierczewska et al., 1999, Swierczewska et al., 2000). Blocky and drusy quartz of the joints represents the latest stage, corresponding to the regional collapse-related extension.
Fluid inclusion study on the blocky and drusy quartz has corroborated circulation of hydrocarbons in flysch sediments of Central and Outer Carpathians (Swierczewska et al., 1999, Hurai et ...
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