Coal deposit "Katrishte" located in south-western Bulgaria, Ro = 0.34%, was subjected to geochemical study. By chromatographic and spectral methods, a variety of coal biomarkers in bitumen extract has been revealed. n-Alkane distribution pattern indicated at least two possible sources, lacustrine and terrestrial ones. The aliphatic fraction was strongly dominated by 16a(H)-kaurane and 16a(H)-phyllocladane, a proof for the presence of Pinales in coal-forming palaeoplant community. The kaurane prevalence over phyllocladane could indicate the herbaceous flowering plant contribution. The combination of sesquiterpenoids/diterpenoids pointed to Pinaceae and Araucariceae.As a biomarker assemblage peculiarity, the lack of isoprenoids, tricyclic dit...
A petrological and organic geochemical study was performed on coal samples from the East field depos...
Peat depositional environments, the sites where and conditions under which peat accumulates, signifi...
Coal samples belonging to the Lower Permian Barakar Formation and the Upper Permian Raniganj Formati...
Abstract. The attention is focused on the “Chukurovo ” lignites of the Sofia coal-bearing province. ...
We investigated early diagenetic processes of the extractable organic matter from the Miocene freshw...
The maceral and biomarker characteristics of 4 sublithotypes of xylite-rich coal (SXCs), pale yellow...
International audienceCarboniferous (Viséan) coals from Dunbar, East Lothian, Scotland, contain well...
The composition of the saturated hydrocarbon fraction of soluble organic matter (bitumen) from the K...
The coal sediment under study was of Miocene/Pliocene geological age. The petrological data pointed ...
Biological markers in the alkane fraction of coal from the central and southern parts of the Kosovo ...
The origin of the organic matter (OM) and the characteristics of the depositional environment of lig...
AbstractMuaraWahau coal belongs to Wahau Formation which was deposited during Early Miocene in terre...
The origin of the organic matter (OM) and the characteristics of the paleoenvironment of Serbian bro...
The bitumens obtained as the extraction products from a series of coals and surrounding rocks sample...
The paper presents results of geochemical analyses of organic matter (OM) in a tonstein bed and surr...
A petrological and organic geochemical study was performed on coal samples from the East field depos...
Peat depositional environments, the sites where and conditions under which peat accumulates, signifi...
Coal samples belonging to the Lower Permian Barakar Formation and the Upper Permian Raniganj Formati...
Abstract. The attention is focused on the “Chukurovo ” lignites of the Sofia coal-bearing province. ...
We investigated early diagenetic processes of the extractable organic matter from the Miocene freshw...
The maceral and biomarker characteristics of 4 sublithotypes of xylite-rich coal (SXCs), pale yellow...
International audienceCarboniferous (Viséan) coals from Dunbar, East Lothian, Scotland, contain well...
The composition of the saturated hydrocarbon fraction of soluble organic matter (bitumen) from the K...
The coal sediment under study was of Miocene/Pliocene geological age. The petrological data pointed ...
Biological markers in the alkane fraction of coal from the central and southern parts of the Kosovo ...
The origin of the organic matter (OM) and the characteristics of the depositional environment of lig...
AbstractMuaraWahau coal belongs to Wahau Formation which was deposited during Early Miocene in terre...
The origin of the organic matter (OM) and the characteristics of the paleoenvironment of Serbian bro...
The bitumens obtained as the extraction products from a series of coals and surrounding rocks sample...
The paper presents results of geochemical analyses of organic matter (OM) in a tonstein bed and surr...
A petrological and organic geochemical study was performed on coal samples from the East field depos...
Peat depositional environments, the sites where and conditions under which peat accumulates, signifi...
Coal samples belonging to the Lower Permian Barakar Formation and the Upper Permian Raniganj Formati...