. . "Teschenite, Hydrothermal alteration, Fluid inclusions, Stable isotopes, REE, Diagenesis, Petroleum, Outer Western Carpathians"@en . "Calcite-pyrite veinlets containing a small amount of quartz, chlorite, sphalerite and marcasite occur in teschenite which is situated within the Lower Cretaceous flysch siliciclastics of the Silesian Unit. Fluid inclusion study demonstrated the presence of a heterogeneous mixture of a low-salinity aqueous solution and mature methane-rich petroleum. The vein formation occurred during an increase in both temperature (from {80 \u00B0C to 220 \u00B0C) and pressure (~100-700 bar)."@en . . "RIV/61989592:15310/12:33140384" . . . . . "RIV/61989592:15310/12:33140384!RIV13-MSM-15310___" . . "0264-8172" . "15310" . "1" . . . . . "Doln\u00ED\u010Dek, Zden\u011Bk" . . . "[DE77A1974AA2]" . . "Diagenetic source of fluids causing the hydrothermal alteration of teschenites in the Silesian Unit, Outer Western Carpathians, Czech Republic: petroleum-bearing vein mineralization from the St\u0159\u00EDbrn\u00EDk site" . . "4"^^ . "Krop\u00E1\u010D, Kamil" . "Marine and petroleum geology" . "Diagenetic source of fluids causing the hydrothermal alteration of teschenites in the Silesian Unit, Outer Western Carpathians, Czech Republic: petroleum-bearing vein mineralization from the St\u0159\u00EDbrn\u00EDk site" . "14"^^ . . "Urubek, Tom\u00E1\u0161" . "Jan\u00ED\u010Dkov\u00E1, Kate\u0159ina" . "Diagenetic source of fluids causing the hydrothermal alteration of teschenites in the Silesian Unit, Outer Western Carpathians, Czech Republic: petroleum-bearing vein mineralization from the St\u0159\u00EDbrn\u00EDk site"@en . . "P(GP205/07/P130), S" . "37" . . "130926" . . "4"^^ . . "Diagenetic source of fluids causing the hydrothermal alteration of teschenites in the Silesian Unit, Outer Western Carpathians, Czech Republic: petroleum-bearing vein mineralization from the St\u0159\u00EDbrn\u00EDk site"@en . . . . "NL - Nizozemsko" . "10.1016/j.marpetgeo.2012.06.004" . "Calcite-pyrite veinlets containing a small amount of quartz, chlorite, sphalerite and marcasite occur in teschenite which is situated within the Lower Cretaceous flysch siliciclastics of the Silesian Unit. Fluid inclusion study demonstrated the presence of a heterogeneous mixture of a low-salinity aqueous solution and mature methane-rich petroleum. The vein formation occurred during an increase in both temperature (from {80 \u00B0C to 220 \u00B0C) and pressure (~100-700 bar)." . . "000308061200003" .