J 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 VÖRÖŠ

Základní 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.