Matches in SemOpenAlex for { <https://semopenalex.org/work/W4385582504> ?p ?o ?g. }
- W4385582504 abstract "Organic‐rich shale samples of the Late Cretaceous Mukalla Formation from the Al‐Fatk1 well in the offshore Jiza‐Qamar Basin, eastern Yemen, were examined using bulk organic geochemistry, microscopic examination, and biomarker measurements combined with 1‐D basin modelling, to evaluate the organic matter characteristics and their ability to generate gas. The studied Mukalla shale samples are characterized by their high organic matter content with total values of up to 14.50 wt.%, and contain mainly hydrogen‐poor Type III kerogen, indicating elevated gas generation potential. The hydrogen‐poor kerogen was also demonstrated by biomarker measurements combined with an abundance of land‐derived organic matter (i.e., vitrinite and inertinite) as established by microscopic investigation. The biomarkers of the studied organic‐rich shales were characterized by a high Pr/Ph ratio, abundance of C 29 regular steranes, high C 27 17α (H)‐22, 29, 30‐trisnorhopane compared with C 27 18α (H)‐22, 29, 30‐trisnorneohopane, all providing evidence for the organic matter being derived primarily from higher land plant organic matter, deposited in fluvial deltaic environments under highly oxic conditions. The bulk carbon isotope data agree with the findings of terrigenous organic matter. The maturity indicators show that the examined organic‐rich shale samples have entered the main oil stage and are at the beginning of wet gas generation windows, exhibiting vitrinite reflectance values that range between 0.73% and 1.20%. Kerogen to gas conversion has been simulated by the basin models and shows that between 10% and 15% of kerogen has transformed into gas during the late Miocene until the present‐day, consistent with the wet gas generation window (1.00–1.20 %Ro). Substantial gas exploration potential may exist in the fluvial deltaic Mukalla source rock system in the deeper structural units of the Qamar‐Jiza Basin, where the Mukalla Formation has reached the high maturity level of the gas generation window." @default.
- W4385582504 created "2023-08-05" @default.
- W4385582504 creator A5024368157 @default.
- W4385582504 creator A5029716563 @default.
- W4385582504 creator A5036262291 @default.
- W4385582504 creator A5039797710 @default.
- W4385582504 creator A5077319141 @default.
- W4385582504 creator A5078404334 @default.
- W4385582504 creator A5085811814 @default.
- W4385582504 date "2023-08-03" @default.
- W4385582504 modified "2023-10-17" @default.
- W4385582504 title "Organic matter characteristics and gas generation prospect of the Late Cretaceous fluvial deltaic organic‐rich shale in the offshore <scp>Jiza‐Qamar</scp> Basin, Yemen based on organic geochemical, macerals composition, and biomarker results combined with <scp>1‐D</scp> basin modelling" @default.
- W4385582504 cites W142464504 @default.
- W4385582504 cites W1498211423 @default.
- W4385582504 cites W1891617492 @default.
- W4385582504 cites W1964797430 @default.
- W4385582504 cites W1967719167 @default.
- W4385582504 cites W1971617177 @default.
- W4385582504 cites W1971762715 @default.
- W4385582504 cites W1988525477 @default.
- W4385582504 cites W1997338331 @default.
- W4385582504 cites W1997532313 @default.
- W4385582504 cites W1998468359 @default.
- W4385582504 cites W2001651429 @default.
- W4385582504 cites W2002305807 @default.
- W4385582504 cites W2004490797 @default.
- W4385582504 cites W2008087765 @default.
- W4385582504 cites W2010119788 @default.
- W4385582504 cites W2011575869 @default.
- W4385582504 cites W2044073149 @default.
- W4385582504 cites W2045386399 @default.
- W4385582504 cites W2053531749 @default.
- W4385582504 cites W2053640801 @default.
- W4385582504 cites W2069777772 @default.
- W4385582504 cites W2080675455 @default.
- W4385582504 cites W2099225250 @default.
- W4385582504 cites W2107580469 @default.
- W4385582504 cites W2142200614 @default.
- W4385582504 cites W2163289772 @default.
- W4385582504 cites W2170995602 @default.
- W4385582504 cites W2263691624 @default.
- W4385582504 cites W2340812574 @default.
- W4385582504 cites W2463001004 @default.
- W4385582504 cites W2593095157 @default.
- W4385582504 cites W2784061531 @default.
- W4385582504 cites W2810428037 @default.
- W4385582504 cites W2998414226 @default.
- W4385582504 cites W3036237614 @default.
- W4385582504 cites W3083450441 @default.
- W4385582504 cites W3128910221 @default.
- W4385582504 cites W3130441956 @default.
- W4385582504 cites W3137574652 @default.
- W4385582504 cites W3183077921 @default.
- W4385582504 cites W3211849541 @default.
- W4385582504 cites W4280627044 @default.
- W4385582504 cites W4283817102 @default.
- W4385582504 cites W4313251871 @default.
- W4385582504 doi "https://doi.org/10.1002/gj.4846" @default.
- W4385582504 hasPublicationYear "2023" @default.
- W4385582504 type Work @default.
- W4385582504 citedByCount "0" @default.
- W4385582504 crossrefType "journal-article" @default.
- W4385582504 hasAuthorship W4385582504A5024368157 @default.
- W4385582504 hasAuthorship W4385582504A5029716563 @default.
- W4385582504 hasAuthorship W4385582504A5036262291 @default.
- W4385582504 hasAuthorship W4385582504A5039797710 @default.
- W4385582504 hasAuthorship W4385582504A5077319141 @default.
- W4385582504 hasAuthorship W4385582504A5078404334 @default.
- W4385582504 hasAuthorship W4385582504A5085811814 @default.
- W4385582504 hasConcept C101433766 @default.
- W4385582504 hasConcept C107872376 @default.
- W4385582504 hasConcept C109007969 @default.
- W4385582504 hasConcept C126559015 @default.
- W4385582504 hasConcept C127313418 @default.
- W4385582504 hasConcept C138496976 @default.
- W4385582504 hasConcept C151730666 @default.
- W4385582504 hasConcept C153127940 @default.
- W4385582504 hasConcept C15744967 @default.
- W4385582504 hasConcept C158787203 @default.
- W4385582504 hasConcept C17409809 @default.
- W4385582504 hasConcept C178790620 @default.
- W4385582504 hasConcept C185592680 @default.
- W4385582504 hasConcept C199285206 @default.
- W4385582504 hasConcept C199289684 @default.
- W4385582504 hasConcept C2777069839 @default.
- W4385582504 hasConcept C2777101687 @default.
- W4385582504 hasConcept C2779196632 @default.
- W4385582504 hasConcept C30370900 @default.
- W4385582504 hasConcept C48743137 @default.
- W4385582504 hasConcept C59235061 @default.
- W4385582504 hasConcept C6494504 @default.
- W4385582504 hasConceptScore W4385582504C101433766 @default.
- W4385582504 hasConceptScore W4385582504C107872376 @default.
- W4385582504 hasConceptScore W4385582504C109007969 @default.
- W4385582504 hasConceptScore W4385582504C126559015 @default.
- W4385582504 hasConceptScore W4385582504C127313418 @default.
- W4385582504 hasConceptScore W4385582504C138496976 @default.
- W4385582504 hasConceptScore W4385582504C151730666 @default.
- W4385582504 hasConceptScore W4385582504C153127940 @default.
- W4385582504 hasConceptScore W4385582504C15744967 @default.