Migration of palaeofluids in the contact zone between the Dukla and Silesian units, Western Carpathians - evidence from fluid inclusions and stable isotopes in quartz and calcite

Jarmołowicz-Szulc, K.; Dudok, I.

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Migration of palaeofluids in the contact zone between the Dukla and Silesian units, Western Carpathians - evidence from fluid inclusions and stable isotopes in quartz and calcite

Autorzy

Jarmołowicz-Szulc K. , Dudok I.

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jarmolowicz-szulc_dudok_migration_3_2005.pdf

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Abstrakty

This study reconstructs the type and migration history of fluids within the Cretaceous-Paleogene rocks of the Silesian and Dukla units in the border area of the Polish and Ukrainian Carpathians. Quartz (the “Marmarosh diamonds”), calcite and organic matter fill fractures in the sedimentary rocks of the Tertiary accretionary prism of the Carpathian thrust units. The calcite and quartz contain numerous solid, liquid and gaseous inclusions. Generally two types of fluids are distinguished — aqueous and hydrocarbon. Homogenisation temperatures of hydrocarbons in quartz range from -128 to + 85°C. Hydrocarbon fluids contain light (methane) and heavier (oil) compounds. Aqueous inclusions generally display homogenisation temperatures between 110 and 230°C. The δ^I3C_PBD values for calcite range from -3.5to +2.9%o, while the δ^I8Osmow range from 18.9 to 27.7%o. The 8I8OSMOwvalues for quartz range from 15.7 and 26.7%o. Fluidinclu- sions indicate that maximum pressures and temperatures occur at the early development of the vein mineralization. They vary from 2.4 to 2.7kbarin the Krosno (Silesian) Unit and from1.7to 1.9kbarinthe Dukla Unit at 190-230°C. The crystallisation of the “Marmarosh diamonds” in the NW part of the study area occurred at lower P-T conditions of 0.9 kbar and 110-175°C. Generally, the migrating fluids are represented by a mixture ofthe low salinity aqueous and the hydrocarbon-rich fluids.

Słowa kluczowe

Carpathians quartz Marmarosh diamonds fluid inclusions hydrocarbons

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2005

Tom

Vol. 49, No. 3

Strony

291--304

Opis fizyczny

Bibliogr. 61 poz., rys., tab.

Twórcy

autor

Jarmołowicz-Szulc K.

Polish Geological Institute, Rakowiecka 4, PL-00-975 Warsaw, Poland

autor

Dudok I.

Institute of Geology and Geochemistry of Combustible Minerals, Naukova 3a,79053 Lviv,Ukraine

Bibliografia

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