FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2068700279> ?p ?o ?g. }

• W2068700279 abstract "The tectonic features of Tunisia are complex and include folds, all types of faults, evaporite diapirs, and the Saharan flexure, which separates a stable Paleozoic province on the south from a subsidence zone of Mesozoic and Cenozoic strata of the offshore Ashtart and Tripolitania basins. The remainder of the offshore region is mostly stable shelf of the Pelagian craton, which also extends onshore. The present study focused on this shelf, where two carbonate intervals contain proven hydrocarbon reservoirs: the Metlaoui Formation of earliest Eocene (Ypresian) age and the Zebbag Formation of Late Cretaceous (Turonian) age. Regionally, well-defined belts of Metlaoui carbonates trend northwest. On the northeast are open-marine deep-water micrites and marls with abundant planktonic foraminifers. Thick bars of nummulitid packstone/grainstone were deposited in shallow water at an angle to the paleoshelf. The reservoir is confined largely to the bars, and visible effective porosity is best developed in those areas among the foraminifers filled with sand-size nummulitid debris, where secondary solution enlargement has occurred. This lithology tested oil in two recent wildcat wells and is a commercial reservoir at Sidi El Itayem and Ashtart fields. Distribution of Zebbag carbonates is more complex. A northwest-trending platform was bounded on three sides by deep water, where shale and micrite with planktonic foraminifers were deposited. Predominately back-reef and lagoonal foraminifer/rudist wackestones and packstones occur in narrow belts, apparently controlled at least locally by block faulting. They tested oil in two recent discoveries. The most significant porosity is interparticle, generally enlarged by solution, in foraminifer packstones, but intraparticle voids in foraminifers and rudists commonly contribute to the porosity. Analyses of surface and subsurface samples identified the Bahloul (basal Turonian) and Bou Dabbous (Ypresian) formations as source rocks. Fluorescence spectra of several oils were compared with extracts from these samples and indicate the Bahloul to be the source of oils in recent Metlaoui and Zebbag discoveries." @default.
• W2068700279 created "2016-06-24" @default.
• W2068700279 creator A5005865141 @default.
• W2068700279 date "1988-01-01" @default.
• W2068700279 modified "2023-09-26" @default.
• W2068700279 title "Petroleum Geology of East-Central Tunisia" @default.
• W2068700279 cites W1969983822 @default.
• W2068700279 cites W1989003977 @default.
• W2068700279 cites W2004500747 @default.
• W2068700279 cites W2009563511 @default.
• W2068700279 cites W2044132451 @default.
• W2068700279 cites W2076127137 @default.
• W2068700279 cites W2081061341 @default.
• W2068700279 cites W2123335600 @default.
• W2068700279 cites W2140331061 @default.
• W2068700279 cites W2288512605 @default.
• W2068700279 cites W2316141647 @default.
• W2068700279 cites W2332922829 @default.
• W2068700279 cites W3123293049 @default.
• W2068700279 cites W3176031103 @default.
• W2068700279 cites W46868219 @default.
• W2068700279 cites W2015979064 @default.
• W2068700279 cites W3118209237 @default.
• W2068700279 doi "https://doi.org/10.1306/703c97b7-1707-11d7-8645000102c1865d" @default.
• W2068700279 hasPublicationYear "1988" @default.
• W2068700279 type Work @default.
• W2068700279 sameAs 2068700279 @default.
• W2068700279 citedByCount "14" @default.
• W2068700279 countsByYear W20687002792012 @default.
• W2068700279 countsByYear W20687002792013 @default.
• W2068700279 countsByYear W20687002792014 @default.
• W2068700279 countsByYear W20687002792016 @default.
• W2068700279 countsByYear W20687002792021 @default.
• W2068700279 countsByYear W20687002792023 @default.
• W2068700279 crossrefType "journal-article" @default.
• W2068700279 hasAuthorship W2068700279A5005865141 @default.
• W2068700279 hasConcept C127313418 @default.
• W2068700279 hasConcept C128777474 @default.
• W2068700279 hasConcept C151730666 @default.
• W2068700279 hasConcept C16674752 @default.
• W2068700279 hasConcept C17409809 @default.
• W2068700279 hasConcept C2985768699 @default.
• W2068700279 hasConcept C548895740 @default.
• W2068700279 hasConceptScore W2068700279C127313418 @default.
• W2068700279 hasConceptScore W2068700279C128777474 @default.
• W2068700279 hasConceptScore W2068700279C151730666 @default.
• W2068700279 hasConceptScore W2068700279C16674752 @default.
• W2068700279 hasConceptScore W2068700279C17409809 @default.
• W2068700279 hasConceptScore W2068700279C2985768699 @default.
• W2068700279 hasConceptScore W2068700279C548895740 @default.
• W2068700279 hasLocation W20687002791 @default.
• W2068700279 hasOpenAccess W2068700279 @default.
• W2068700279 hasPrimaryLocation W20687002791 @default.
• W2068700279 hasRelatedWork W1970149378 @default.
• W2068700279 hasRelatedWork W2066627560 @default.
• W2068700279 hasRelatedWork W2067055967 @default.
• W2068700279 hasRelatedWork W2149036922 @default.
• W2068700279 hasRelatedWork W2325365690 @default.
• W2068700279 hasRelatedWork W2327025226 @default.
• W2068700279 hasRelatedWork W2352627138 @default.
• W2068700279 hasRelatedWork W2385403154 @default.
• W2068700279 hasRelatedWork W2388871325 @default.
• W2068700279 hasRelatedWork W1924308321 @default.
• W2068700279 hasVolume "72" @default.
• W2068700279 isParatext "false" @default.
• W2068700279 isRetracted "false" @default.
• W2068700279 magId "2068700279" @default.
• W2068700279 workType "article" @default.