1-20 OF 133 RESULTS FOR

Jubaila Formation

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
Well Wadi Laban-1 spudded within the lowermost <b>Jubaila</b> <b>Formation</b> (exposed i...
Published: 01 April 2008
Figure 12: Well Wadi Laban-1 spudded within the lowermost Jubaila Formation (exposed in the cliff behind the rig), Wadi Laban (24°29′01.0″N, 46°35′59.8799″E). Note the recessive, transgressive systems tract associated mud-dominated lower part Ju1 and the resistive, grain-dominated upper part Ju2
Image
The <b>Jubaila</b> <b>Formation</b>, looking south into Wadi Laban, a tributary valley of...
Published: 01 July 2004
Figure 20: The Jubaila Formation, looking south into Wadi Laban, a tributary valley of Wadi Hanifa. Note the well-developed, smooth scree-dominated profile of the lower part, resulting from the less resistive, mud-dominated sediments equated with J1. The upper third of the exposure forms highly
Image
Stromatoporoid cf.  Burgundia  sp. in the upper <b>Jubaila</b> <b>Formation</b>, Wadi Dir...
Published: 01 July 2004
Figure 23: Stromatoporoid cf. Burgundia sp. in the upper Jubaila Formation, Wadi Dirab roadcut, west of Riyadh. Note the well-defined growth laminae. This specimen lies within a stromatoporoid-filled channel and is not in-situ; the apparent way-up position is fortuitous, and is surrounded
Image
The upper <b>Jubaila</b> <b>Formation</b> at Wadi Helwah, Hawtah region (N 23° 28.173’; E...
Published: 01 July 2004
Figure 24: The upper Jubaila Formation at Wadi Helwah, Hawtah region (N 23° 28.173’; E 46°52.101’) displaying in-situ erect coral overlying a bed containing transported stromatoporoids and corals. Note this specimen is located on the same bed as the stromatoporoid in Figure 22 .
Image
Historical evolution of Arab and <b>Jubaila</b> <b>formation</b> lithostratigraphic nomen...
Published: 01 July 1996
Figure 3: Historical evolution of Arab and Jubaila formation lithostratigraphic nomenclature as shown by Powers (1968) .
Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/1215875M88576
EISBN: 9780891813699
... zonation scheme for reservoir management. Arab-D Member of the Arab Formation consists of zone 1, zone 2a, and upper zone 2b, and the remainder of the Arab-D reservoir, consisting of lower zone 2b, zones 3a and 3b, and zone 4, is part of the upper Jubaila Formation ( Meyer et al., 2000 ). The first...
FIGURES | View All (37)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2004
GeoArabia (2004) 9 (3): 79–114.
...Figure 20: The Jubaila Formation, looking south into Wadi Laban, a tributary valley of Wadi Hanifa. Note the well-developed, smooth scree-dominated profile of the lower part, resulting from the less resistive, mud-dominated sediments equated with J1. The upper third of the exposure forms highly...
FIGURES | View All (33)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2015
GeoArabia (2015) 20 (4): 125–180.
... is represented by the Late Oxfordian (Subzone NJT 13b) Najmah Limestone, and is overlain by the Kimmeridgian (Zone NJT 14) Jubaila Formation. Early Kimmeridgian MFS J60 and Late Kimmeridgian MFS J70 are positioned near the base and top of the Jubaila Formation. The positions of Late Jurassic MFS J80, J90...
FIGURES | View All (21)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 1997
GeoArabia (1997) 2 (4): 361–382.
... sequence. The correlation between the Dhruma, Tuwaiq Mountain, Hanifa and Jubaila formations, to their equivalents in other Arabian Gulf countries, requires clearer definitions. (5) The Arab and Hith Anhydrite formations are Tithonian based on their sequence assignment, while the Sulaiy Formation...
FIGURES | View All (13)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 1996
GeoArabia (1996) 1 (3): 417–434.
...Geraint Wyn Hughes ABSTRACT A series of fine-scale biofacies cycles are recognised by the application of semiquantitative micropalaeontological analysis of cores in eight wells from the reservoir carbonates from the Arab-D and upper Jubaila formations in Saudi Arabia. They are of Kimmeridgian...
FIGURES | View All (13)
Series: AAPG Special Publication, AAPG Special Publication
Published: 01 January 1958
DOI: 10.1306/SV18350C52
EISBN: 9781629812434
... and Jubaila formations) of coastal Arabia, originated in and near the rocks in which the oil is now found. The later Jurassic Arab formation (middle or upper Upper Jurassic) shows increased paleogeographic differentiation. During the time of lower Arab deposition an extensive evaporite-depositing lagoon...
Journal Article
Published: 17 July 2013
Petroleum Geoscience (2013) 19 (4): 399–415.
... response of the outcrop lithofacies and their elemental content. The two units of the reservoir (the Upper Jubaila Member of the Jubaila Formation and the Arab-D Member of the Arab Formation) showed distinctive SGR log profiles controlled mainly by their lithofacies associations. The geochemical analysis...
FIGURES | View All (18)
Image
Late Jurassic stratigraphic section including the Hanifa, <b>Jubaila</b> and Arab ...
Published: 17 July 2013
Fig. 1. Late Jurassic stratigraphic section including the Hanifa, Jubaila and Arab formations. The Arab-D reservoir includes both the Upper Jubaila Member of the Jubaila Formation and the Arab-D Member of the Arab Formation ( Cantrell & Hagerty 1999 ).
Image
Late Jurassic stratigraphic section including Hanifa, <b>Jubaila</b>, and Arab for...
Published: 01 April 2014
Figure 1: Late Jurassic stratigraphic section including Hanifa, Jubaila, and Arab formations. The Arab-D reservoir includes both the Upper Jubaila Member of the Jubaila Formation and the Arab-D Member of the Arab Formation (modified from Cantrell and Hagerty, 1999) .
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1959
AAPG Bulletin (1959) 43 (2): 434–454.
... Dar to Haradh. Ghawar oil is Upper Jurassic, occurring in the shallow-water carbonate sediments of the upper Jubaila and lower Arab formations. It is confined above by the lowest of the three anhydrite members of the Arab formation. Only minor shows of oil have been found in higher parts of the Arab...
FIGURES | View All (8)
Image
(a) The upper <b>Jubaila</b> carbonates as exposed in the road section west of Riy...
Published: 01 July 2004
of this exposure marks the top of the Jubaila Formation, but the Arab-D Formation is not preserved at this locality. (b) Close-up of karst feature within the upper Jubaila Formation, showing remains of Thalassinoides burrows. The feature is bed-conformable at its upper surface, but crosses beds in the lower part
Journal Article
Journal: AAPG Bulletin
Published: 01 July 2013
AAPG Bulletin (2013) 97 (7): 1099–1119.
..., and Arab-A. The Arab-D reservoir is the main reservoir in Khurais field, one of the largest onshore oil fields of the Kingdom of Saudi Arabia. In Khurais field, the Arab-D reservoir is composed of the overlying evaporitic Arab-D Member of the Arab Formation and the underlying upper part of the Jubaila...
FIGURES | View All (11)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2008
GeoArabia (2008) 13 (2): 15–46.
...Figure 12: Well Wadi Laban-1 spudded within the lowermost Jubaila Formation (exposed in the cliff behind the rig), Wadi Laban (24°29′01.0″N, 46°35′59.8799″E). Note the recessive, transgressive systems tract associated mud-dominated lower part Ju1 and the resistive, grain-dominated upper part Ju2...
FIGURES | View All (26)
Image
—Schematic stratigraphic reconstruction of upper <b>Jubaila</b> and Arab- D  produ...
Published: 01 February 1959
Fig. 5. —Schematic stratigraphic reconstruction of upper Jubaila and Arab- D producing zones in profile across northern part of Shedgum area. Upper heavy black line is top of Jubaila formation.
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2007
GeoArabia (2007) 12 (3): 15–30.
...Dave L. Cantrell; Abdullah Al-Khammash; Peter D. Jenden ABSTRACT Two different types of calcified dolomite, or dedolomite, occur as stratiform and non-stratiform bodies within the Jurassic (Kimmeridgian) upper Jubaila Formation in the Wadi Nisah area of central Saudi Arabia...
FIGURES | View All (20)