1-20 OF 26 RESULTS FOR

Sabil Carbonate

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Image
The regional time-structure map of Upper <span class="search-highlight">Sabil</span> <span class="search-highlight">Carbonate</span> is derived from th...
Published: 01 March 2023
Figure 7. The regional time-structure map of Upper Sabil Carbonate is derived from three-dimensional seismic data showing the Intisar pinnacle reefs.
Image
Paleogeographic map of the Upper <span class="search-highlight">Sabil</span> <span class="search-highlight">Carbonate</span>, an update of  Figure 3  b...
Published: 01 March 2023
Figure 18. Paleogeographic map of the Upper Sabil Carbonate, an update of Figure 3 based on this study.
Journal Article
Published: 01 March 2023
Bulletin of Canadian Energy Geoscience (2023) 70 (1): 21–52.
...Figure 7. The regional time-structure map of Upper Sabil Carbonate is derived from three-dimensional seismic data showing the Intisar pinnacle reefs. ...
FIGURES | View All (21)
Image
Approximate location of the Paleocene Upper <span class="search-highlight">Sabil</span> <span class="search-highlight">carbonate</span> shelf edge, Ajd...
Published: 11 December 1999
Figure. 8 Approximate location of the Paleocene Upper Sabil carbonate shelf edge, Ajdabiya Trough: a zone of potential reef and shoal development. Shelf slope pinnacle reef oil fields are shown.
Image
Multi-attribute surface maps and the main facies elements of Upper <span class="search-highlight">Sabil</span> Ca...
Published: 01 March 2023
Figure 10. Multi-attribute surface maps and the main facies elements of Upper Sabil Carbonate.
Journal Article
Published: 26 February 2024
Petroleum Geoscience (2024) 30 (1): petgeo2023-008.
.... The reservoirs are charged from the underlying mature Upper Cretaceous shales via faults and fractures. This study will focus on palaeokarsts that exist within the Upper Sabil Carbonate in the Sirt Basin. Palaeokarst features are buried deep beneath younger sediment, so the tools available to study them...
FIGURES | View All (12)
Journal Article
Journal: AAPG Bulletin
Published: 11 December 1999
AAPG Bulletin (1999) 83 (12): 1–40.
...Figure. 8 Approximate location of the Paleocene Upper Sabil carbonate shelf edge, Ajdabiya Trough: a zone of potential reef and shoal development. Shelf slope pinnacle reef oil fields are shown. ...
FIGURES | View All (21)
Journal Article
Journal: Interpretation
Published: 07 October 2015
Interpretation (2016) 4 (1): SB1–SB11.
... of the eastern Sirte Basin in Middle Paleocene (Selandian) time. The Sheterat Formation separates the Lower Sabil Formation from the basal dolomite-anhydrite section of the Upper Sabil Formation. Carbonate shelf conditions returned during the Thanetian, and the Upper Sabil succession was deposited, along...
FIGURES | View All (9)
Journal Article
Published: 01 June 1997
Journal of the Geological Society (1997) 154 (3): 483–489.
.... Poupeau G. Riou L. Sabil N. Basile C. Mascle J. Mascle G. Equanaute Scientific Party La marge transformante de Côte d’Ivoire-Ghana: premières donneés thermo-chronologiques (cam-pagne Equanaute, 1992) Comptes Rendus de l’Acadamie des Sciences Paris 1994 318 1365 1370...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1985
AAPG Bulletin (1985) 69 (1): 39–52.
... ). These facies changes represent a local variation in depositional setting across the platform margin. To the east and west of the Marada trough the Paleocene section changes laterally to a predominantly shelf carbonate facies—Satal carbonate on the Dahra platform to the west and Sabil carbonates on the Zeiten...
FIGURES | View All (14)
Series: AAPG Memoir
Published: 01 January 2001
DOI: 10.1306/M74775C22
EISBN: 9781629810621
.... Approximate location of the Paleocene Upper Sabil carbonate shelf edge, Ajdabiya trough—a zone of potential reef and shoal development. Shelf slope pinnacle reef oil fields are shown. Seals. —Etel shale and anhydrite at the Sirt unconformity provide an effective seal for the Nubian sandstone...
FIGURES | View All (21)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 2008
AAPG Bulletin (2008) 92 (8): 993–1027.
... grade into platform carbonates along the shelf (Upper Satal, Defa, and Lower Sabil). Synrift 2 Kalash (Lower Satal and Waha) Limestones, predominantly argillaceous calcilutite, with dark gray calcareous shale beds. The depositional environment is open marine, probably neritic, as suggested by Barr...
FIGURES | View All (16)
Journal Article
Published: 01 October 2023
Geochemical Perspectives (2023) 12 (2): 240–310.
... – 311 . Sabil , K.M. , Azmi , N. , Mukhtar , H. ( 2011 ) A review on carbon dioxide hydrate potential in Technological Applications . Journal of Applied Sciences 11 , 3534 – 3540 . Saldi , G. , Kohler , S.J. , Marty , N. , Oelkers , E.H. ( 2007 ) Dissolution...
FIGURES | View All (47)
Journal Article
Journal: GSA Bulletin
Published: 01 November 2003
GSA Bulletin (2003) 115 (11): 1425–1440.
.... The Valaisan units ( Fig. 2 ) are derived from the more external North Penninic (or Valais) oceanic basin ( Trümpy, 1955 ; Frisch, 1979 ). Two different domains have been distinguished ( Fügenschuh et al., 1999 ; Loprieno, 2001 ). The external Valaisan represents an eroded carbonate platform unconformably...
FIGURES | View All (11)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 1999
GeoArabia (1999) 4 (4): 503–542.
... siliciclastics and carbonates of the lower Miocene Tayran group, unconformable on the Proterozoic basement. The Tayran group is unconformably overlain by the deep-marine lower Miocene Burqan formation that, in turn, is overlain by marine mudstones, carbonates, and evaporites of the middle Miocene Maqna group...
FIGURES | View All (35)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2015
GeoArabia (2015) 20 (1): 99–156.
... and half-graben settings, and possible northwest-trending bounding faults similar to the Najd basins in Saudi Arabia. Again, in contrast to the outcrop areas to the west, the upper part of the Araba Complex, hereabouts, consists of fine-grained, in part carbonate-cemented sandstone and claystone, together...
FIGURES | View All (40)
Journal Article
Published: 01 September 1988
Bulletin of Canadian Petroleum Geology (1988) 36 (3): 311–332.
... to Devonian platform carbonates and Middle to Upper Devonian foredeep siliciclastic formations that lie uncon- formably on deformed and eroded Proterozoic strata. This same stratigraphic succession is involved in the latest Devonian to earliest Carboniferous foreland deformation of the Franklinian Mobile Belt...
Journal Article
Published: 08 May 2015
Geochemistry: Exploration, Environment, Analysis (2015) 15 (4): 273–291.
... (and sometimes sulphosalts) in broad silicified zones or quartz carbonate veins bounded by sericite or chlorite schist ( Boyle 1961 ; Ellis & Hearn 1990 ). Ore shoots typically contained less than 10% sulphide content and more often less than 5%, although up to 15% sulphide has been reported ( Coleman 1957...
FIGURES | View All (10)
Series: AAPG Studies in Geology
Published: 01 January 2002
DOI: 10.1306/St48794C14
EISBN: 9781629810591
... ); magnetic-mineral genesis ( Donovan et al., 1979 , 1986; Foote, 1987 ); oxidized soil carbonate “salts” ( Duchscherer, 1981 , 1988 ); efflorescence of petroleum-eating bacteria ( Beghtel et al., 1987 ); natural earth gamma radiation ( Fisher, 1985 ; Tedesco, 1988 ); and trace-metal or elemental-soil...
FIGURES | View All (15)
Series: Geological Society, London, Special Publications
Published: 01 January 2003
DOI: 10.1144/GSL.SP.2003.207.11
EISBN: 9781862394551
.... Tagrifet Formation-Intisar (!) petroleum system. The main play in the southern part of the Agedabia Trough is for Paleocene (Upper Sabil Formation) carbonates, within large reefal build-ups (Intisar pinnacle reefs) and smaller carbonate build-ups and structural traps. Reservoir development...
FIGURES | View All (29)