Fluid inclusion studies were conducted in the vein quartz known as the "Marmarosh diamonds" of the Krosno and Dukla zones of the Ukrainian Carpathians, which are potentially oil- and gas-bearing. The "Marmarosh diamonds" contain different types of fluid inclusions which record the evolution of the quartz formation. The inclusions were studied by means of gas chromatography, microthermometry and fluorescence. The following sequence has been observed: methane inclusions displaying characteristic features due to crystallography, light hydrocarbons, complex inclusions with a variety of bitumens, and gas-liquid inclusions with two different hydrocarbon phases. The regions where the light hydrocarbon inclusions occur seem to be the most promising...
This paper presents an integrated workflow for investigating hydrocarbon charge history using fluid ...
Based on sedimentological and organic geochemical investigations, a systematic approach toward the c...
Fluid inclusions - tiny portions of palaeofluids trapped in minerals filling pore space in sedimenta...
Fissures in the nappes of the Folded Carpathians contain euhedral quartz crystals known as Marmarosh...
Based on the assumption that fluorescence studies are an important tool in search and characterizati...
The origin of hydrocarbon-bearing fluid inclusions in igneous rocks remains controversial. The hydro...
Primary and secondary hydrocarbon-bearing fluid inclusion (HCFI) assemblages occur in the Middle Tri...
The quartz grains from the sandstone of Jaisalmer, Pariwar and Goru Formations of the Jaisalmer basi...
Research subject. This article analyses specific features of secondary transformations of quartz gra...
International audienceThe fluid history of “diamond” quartz crystals from Caravia-Berbes Fluorite di...
Na podstawie badań przeprowadzonych w obrębie trzech obszarów w Polsce przedstawiono charakterystykę...
The occurrence of hydrocarbon-bearing fluids in alkaline igneous rocks has been known for many years...
© 2020 IOP Publishing Ltd. All rights reserved. Fluid inclusions from calcite veins were studied the...
This thesis deals with fluid inclusion study of quartz samples from Ratibořské Hory and Stará Vožice...
are often infilled with quartz, carbonates, sulphides, and hydrocarbons. The quartz contains a mi...
This paper presents an integrated workflow for investigating hydrocarbon charge history using fluid ...
Based on sedimentological and organic geochemical investigations, a systematic approach toward the c...
Fluid inclusions - tiny portions of palaeofluids trapped in minerals filling pore space in sedimenta...
Fissures in the nappes of the Folded Carpathians contain euhedral quartz crystals known as Marmarosh...
Based on the assumption that fluorescence studies are an important tool in search and characterizati...
The origin of hydrocarbon-bearing fluid inclusions in igneous rocks remains controversial. The hydro...
Primary and secondary hydrocarbon-bearing fluid inclusion (HCFI) assemblages occur in the Middle Tri...
The quartz grains from the sandstone of Jaisalmer, Pariwar and Goru Formations of the Jaisalmer basi...
Research subject. This article analyses specific features of secondary transformations of quartz gra...
International audienceThe fluid history of “diamond” quartz crystals from Caravia-Berbes Fluorite di...
Na podstawie badań przeprowadzonych w obrębie trzech obszarów w Polsce przedstawiono charakterystykę...
The occurrence of hydrocarbon-bearing fluids in alkaline igneous rocks has been known for many years...
© 2020 IOP Publishing Ltd. All rights reserved. Fluid inclusions from calcite veins were studied the...
This thesis deals with fluid inclusion study of quartz samples from Ratibořské Hory and Stará Vožice...
are often infilled with quartz, carbonates, sulphides, and hydrocarbons. The quartz contains a mi...
This paper presents an integrated workflow for investigating hydrocarbon charge history using fluid ...
Based on sedimentological and organic geochemical investigations, a systematic approach toward the c...
Fluid inclusions - tiny portions of palaeofluids trapped in minerals filling pore space in sedimenta...