2015
A Geochemical and Petrographical Characterization of Organic Matter in the Jurassic Mikulov Marls from the Czech Republic
GERŠLOVÁ, Eva, Vladimír OPLETAL, Ivana SÝKOROVÁ, Iva SEDLÁKOVÁ, Milan GERŠL et. al.Základní údaje
Originální název
A Geochemical and Petrographical Characterization of Organic Matter in the Jurassic Mikulov Marls from the Czech Republic
Autoři
GERŠLOVÁ, Eva (203 Česká republika, garant, domácí), Vladimír OPLETAL (203 Česká republika), Ivana SÝKOROVÁ (203 Česká republika), Iva SEDLÁKOVÁ (203 Česká republika, domácí) a Milan GERŠL (203 Česká republika)
Vydání
International Journal of Coal Geology, 2015, 0166-5162
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Nizozemské království
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 3.294
Kód RIV
RIV/00216224:14310/15:00082897
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000354341200005
Klíčová slova anglicky
Mikulov Marls; kerogen type; thermal maturity; vitrinite reflectance; Rock-Eval pyrolysis
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 20. 9. 2018 19:37, doc. Mgr. Eva Geršlová, Ph.D.
Anotace
V originále
In this study a Rock-Eval pyrolysis, a petrographic composition of organic matter, vitrinite reflectance and gas chromatography were undertaken on borehole cores from the Mikulov Marls in order to define the organic matter type and determine the thermal maturity. The analyzed samples covered a depth interval of between 2,300 m and 4,500 m. The studied sediments were dark-colored, moderately laminated shale’s throughout which appear uniform upon visual examination. The geochemical analyses revealed that the source rock potential of the Mikulov Marls is from fair to good. According to the Rock-Eval pyrolysis, the organic matter in the samples was classified as kerogen type II-III. This classification is not supported by the results from the other used methods. The evaluation of the organic macerals demonstrated the dominant role of liptinite with prevailing liptodetrinite accompanied by a variable content of alginite, bituminite, and sporadic sporinite and resinite. The alginite consists mainly of lamalginite, derived from colonial planktonic or benthonic algae. Based on these results, the Mikulov Marls represent the kerogen type II. These results are also supported with a strong n-alkane odd-carbon-number predominance at n-C15, n-C17 and n-C19 range on the gas chromatography.