1-20 OF 81 RESULTS FOR

Saiq Basin

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
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2013
GeoArabia (2013) 18 (3): 87–98.
...Aymon Baud; Sylvain Richoz This note discusses the lithostratigraphic nomenclature used to characterise the Permian-Triassic transition at outcrop in the Oman Mountains, with emphasis on the position of the boundary between the Saiq and Mahil formations. Two inconsistent criteria for picking...
FIGURES | View All (7)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2010
GeoArabia (2010) 15 (2): 91–156.
..., deeper subtidal setting between fair-weather wave base and storm wave base); LFA 8: Offshoal to basinal (low-energy, deep subtidal setting below storm wave base). The lithofacies types observed on the Saiq Plateau were classified in terms of these lithofacies associations and depositional...
FIGURES | View All (43)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2013
GeoArabia (2013) 18 (3): 135–178.
... that were used for correlation at a subregional scale and to reveal the KS6 stratigraphic architecture. During the initial phase of basin-fill, clastic sediments (“Basal Saiq Clastics”) were deposited in paleolows above the “Sub-Saiq Unconformity”. In contrast to younger Upper Khuff sequences KS4 to KS1...
FIGURES | View All (39)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2013
GeoArabia (2013) 18 (3): 103–130.
..., 18B and 18C), each consisting of 12 stratons. Individual dozons lasted 4.86 Myr and are separated by regional sequence boundaries (SB 19C to SB 17A). In Oman, Khuff Sequence KS6 on the Saiq Plateau is correlated to the subsurface Lower Khuff Member, and both are interpreted to consist of 12...
FIGURES | View All (14)
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/GSL.SP.2007.275.01.15
EISBN: 9781862395237
.... Permian deposits of the Saih Hatat, with a thickness of 1000 m, are part of the Akhdar Group. Shallow-water tropical carbonate deposition started on the Arabian plate after the Permo-Carboniferous glaciation with the Saiq Formation, (see Figs 2 & 3). The oldest Permian limestones have a Wordian age...
FIGURES | View All (10)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2012
GeoArabia (2012) 17 (4): 59–104.
...Bastian Koehrer; Thomas Aigner; Holger Forke; Michael Pöppelreiter ABSTRACT The upper part of the Saiq and lower part of the Mahil formations in the Oman Mountains represent outcrop time-equivalents to the highly prolific, hydrocarbon-bearing subsurface Middle and Upper members of the Khuff...
FIGURES | View All (30)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2015
GeoArabia (2015) 20 (2): 115–142.
... heterogeneities and fluid flow. On the Saiq Plateau in Oman, epeiric carbonate ramp deposits of the Triassic Sudair Formation are well exposed and can be investigated in detail over several kilometers. There, reservoir heterogeneities on different scales have been documented by creating various outcrop wall...
FIGURES | View All (21)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2012
GeoArabia (2012) 17 (1): 181–239.
..., < daniel.bendias@gmail.com ), Thomas Aigner (University of Tübingen), Michael Pöppelreiter (Shell) and Bastian Köhrer (Wintershall) This outcrop analog study of Lower Khuff Sequence KS6 (Saiq Formation) aims to capture lateral reservoir facies distribution during the initial phase of basin-fill...
FIGURES | View All (30)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2013
GeoArabia (2013) 18 (2): 17–62.
...Vladimir I. Davydov; Arefifard Sakineh ABSTRACT The Middle–Upper Permian (Guadalupian–Lopingian) Dalan Basin was part of a very large carbonate ramp/platform along the passive margin of the Arabian Plate, located at mid-latitude Neo-Tethys Ocean. As shown in the modern world the mid-latitudes...
FIGURES | View All (21)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 1998
GeoArabia (1998) 3 (4): 475–490.
...Van S. Mount; Roderick I.S. Crawford; Steven C. Bergman ABSTRACT Three quantitative regional transects across the Saih Hatat and Jebel Akhdar anticlines in the Central and Southern Oman Mountains and the Northern Ghaba Basin have been constructed based on surface, well and seismic data. Interpreted...
FIGURES | View All (14)
Journal Article
Published: 01 March 2002
Geological Magazine (2002) 139 (2): 145–157.
... of the Neotethyan geodynamic evolution. The Batain Exotics bear witness to volcanic activity, sea-level changes, tectonic instability, rifting and oceanization along the Eastern Oman margin during Late Palaeozoic and Mesozoic times. They allow definition of the Batain basin as an aborted Permian branch of Neotethys...
FIGURES | View All (9)
Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2002
DOI: 10.2110/pec.02.72.0339
EISBN: 9781565761940
... Abstract Middle and Late Permian reefs flourished for about 20 million years in the Tethys, the Panthalassan ocean, the Delaware Basin, the Zechstein Basin, and the Northwest Pangean era tonic basin Eight reef types, which were differentiated...
FIGURES | View All (13)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2013
GeoArabia (2013) 18 (2): 141–176.
... at the surface-piercing salt domes of the Ghaba Salt Basin in central Oman. In the absence of unequivocal dating evidence, the regional context suggests the intrusion may be derived from evaporites within the Ediacaran–Early Cambrian Ara Group. These form large deposits in the Fahud and Ghaba salt basins...
FIGURES | View All (32)
Journal Article
Published: 01 December 1994
Journal of the Geological Society (1994) 151 (6): 999–1016.
..., whereas the left hand key represents the autochthonous and parautochthonous basement, shelf and foreland basin units. The Saiq, Mahil, Sahtan and Kahmah units consist of limestones and dolomites. The mafic bodies sampled in this study are labelled a , b and c . Mafic samples from Region I were...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2014
GeoArabia (2014) 19 (1): 143–158.
... to constrain the tectonic elements, major lineation trends and structures of the Neoproterozoic basement of the Arabian Plate and the distribution of infra-Cambrian salt basins. Advanced transformation techniques (including first vertical derivative, total horizontal derivative, tilt derivative and Euler...
FIGURES | View All (19)
Journal Article
Published: 01 January 2000
Geological Magazine (2000) 137 (1): 1–18.
...ADRIAN IMMENHAUSER; GUIDO SCHREURS; EDWIN GNOS; HEIKO W. OTERDOOM; BERNHARD HARTMANN Abstract When the highlands of Arabia were still covered with an ice shield in the latest Carboniferous/Early Permian period, separation of Gondwana started. This led to the creation of the Batain basin (part...
FIGURES | View All (6)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2007
GeoArabia (2007) 12 (2): 99–130.
...Michael P. Searle ABSTRACT The Al Jabal al Akhdar and Saih Hatat culminations in the central Oman Mountains expose the complete mid-Permian to Late Cretaceous (Cenomanian) passive shelf and margin carbonate sequence beneath the allochtonous slope (Sumeini Group), basin (Hawasina complex), distal...
FIGURES | View All (21)
Series: Geological Society, London, Memoirs
Published: 01 March 2021
DOI: 10.1144/M54.5
EISBN: 9781786205254
... of Pangaea and subsequent formation of the Hawasina ocean basin, are recorded in the Southeastern Oman Mountains. As a result, a passive margin formed which existed until the mid-Cretaceous, characterized by deposition of mostly shelfal carbonates. This interval of general tectonic quiescence was interrupted...
FIGURES | View All (25)
Image
Correlation of Middle–Upper Permian (Guadalupian–Lopingian) sections within...
in > GeoArabia
Published: 01 April 2013
, 2003) ; Transcaucasia ( Kotlyar et al., 1989 ; Leven, 1998) ; Abadeh ( Kobayashi and Ishii, 2003a ); Zagros (this paper); Northeast Oman Para-Autochtonous Saiq Basin ( Koehrer et al., 2010 ; Forke et al., 2012) ; Oman “Exotics” (Hawasina and Batain Nappes) ( Baud et al., 2012 ; Blendinger et al
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2012
GeoArabia (2012) 17 (1): 49–98.
...Christopher J. Nicholas; Sophia E.P. Gold ABSTRACT The Ediacaran–Cambrian Ara Group of the South Oman Salt Basin in the Sultanate of Oman is one of the world’s oldest petroleum systems and holds some of the most important hydrocarbon reserves in the country. However, the Ara Group salt and isolated...
FIGURES | View All (29)