2020
Hydrocarbon potential and depositional paleoenvironment of a Middle Jurassic succession in the Falak-21 well, Shushan Basin, Egypt: Integrated palynological, geochemical and organic petrographic approach
MANSOUR, Ahmed; Eva GERŠLOVÁ; Ivana SÝKOROVÁ a Dominik VÖRÖŠZákladní údaje
Originální název
Hydrocarbon potential and depositional paleoenvironment of a Middle Jurassic succession in the Falak-21 well, Shushan Basin, Egypt: Integrated palynological, geochemical and organic petrographic approach
Název česky
Uhlovodíkový potenciál a depoziční prostředí jurských sedimentů ve vrtu Falak 21, Egypt: integrované zhodnocení na základě palynologie, geochemie a organické petrografie
Autoři
MANSOUR, Ahmed; Eva GERŠLOVÁ; Ivana SÝKOROVÁ a Dominik VÖRÖŠ
Vydání
International Journal of Coal Geology International Journal of Coal Geology, ELSEVIERRADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS, 2020, 0166-5162
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Stát vydavatele
Nizozemské království
Utajení
není předmětem státního či obchodního tajemství
Impakt faktor
Impact factor: 6.806
Označené pro přenos do RIV
Ne
Klíčová slova česky
organická petrografie, palynologie, palynofacie, Shushan pánev, Egypt
Klíčová slova anglicky
Organic petrology, Palynology, Palynofacies, Shushan Basin, Egypt
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 8. 12. 2021 10:49, doc. Mgr. Eva Geršlová, Ph.D.
Anotace
V originále
The topmost Lower and Middle Jurassic formations of organic-rich clastics with minor carbonate deposits were recognized as very significant source/reservoir rocks in the North Western Desert of Egypt. Although several studies are devoted to their source rock characteristics and petroleum potential, the depositional paleoenvironment and paleoredox conditions are still poorly understood. In the current study, these sediments were assessed in terms of their organic matter richness, hydrocarbon generative potential and thermal maturity, total sulfur (TS) contents and organic petrographic characteristics. Depositional paleoenvironment was investigated using dinoflagellate cysts (dinocysts) and the composition of particulate organic matter along with organic petrographic characteristics. Redox conditions were assessed based on TS- total organic carbon (TOC) relationship and type of kerogen that was derived mainly from palynofacies analysis. TOC contents show fair to excellent generative potential of hydrocarbons mainly of kerogen type III (gasprone). The thermal maturity, based on Tmax and Rr, indicates mature stage of oil window. Palynological analysis yielded poor to rich intervals of moderately-preserved, biostratigraphically useful dinocysts in the upper part of the Khatatba Formation. An assemblage of 81 species belonging to 54 genera of moderately diverse dinocysts, spores and pollen grains was identified. Freshwater algae, acritarchs and microforaminiferal test linings are sporadically documented within the studied interval.