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Aruma Group

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Series: GCSSEPM
Published: 01 December 2012
DOI: 10.5724/gcs.12.32.0534
EISBN: 978-0-9836097-8-0
... Cretaceous Aruma Group carbonates ( Fig. 2 ). Potential source rocks include the basal Hadhramaut Group shales, intra-Aruma Group shales, organic-rich units in the basinal Jurassic Sahtan Group, and the Infracambrian middle to upper Huqf Super Group. Sealing units for potential traps are provided...
Image
Late Cretaceous time chart for shelf and foreland basin (<b>Aruma</b> <b>Group</b>) in Ce...
in > GeoArabia
Published: 01 April 2007
Figure 4: Late Cretaceous time chart for shelf and foreland basin (Aruma Group) in Central Oman, based on seismic and well data, adapted after Warburton et al. (1990) , showing thrusts cutting into the Fiqa and Juweiza formations during the Late Cretaceous emplacement (stage 1a to 1d). Also
Image
—<b>Aruma</b> <b>Group</b> isopach map. Map omits wells in which thickening due to thrust...
Published: 01 July 1988
Fig. 7. —Aruma Group isopach map. Map omits wells in which thickening due to thrusting is likely.
Series: SEPM Special Publication
Published: 01 January 2000
DOI: 10.2110/pec.00.69.0315
EISBN: 9781565761919
.... Within the three groups of the Lower, middle, and Upper Cretaceous, referred to as the Thamama, Wasia, and Aruma Groups in the Arabian Gulf region, seven major sedimentary cycles are recognized. Three of these cycles or major sequences are attributed to the Lower Cretaceous Thamama Group, and each...
Journal Article
Published: 01 October 1988
Journal of the Geological Society (1988) 145 (5): 831-845.
... occurred after the Turonian-Maastrichtian thin-skinned thrusting of the Oman Mountains was completed. The basal Hagab thrust cuts up-section to the west from at least mid-Permian level up to the late Cretaceous Aruma Group and breached up into the overlying previously allochthonous (Cretaceous) Hawasina...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2002
GeoArabia (2002) 7 (4): 699-718.
...Jean M. Philip; Jack Roger; Denis Vaslet; Fabrizio Cecca; Silvia Gardin; Abdullah M.S. Memesh ABSTRACT The Aruma Formation is a predominantly carbonate lithostratigraphic unit of Late Cretaceous age that crops out in Saudi Arabia. It consists of three members: from base to top they are Khanasir...
FIGURES | View All (14)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2006
GeoArabia (2006) 11 (1): 97-140.
... Maastrichtian to Palaeocene uplift and erosion in excess of 1,000 m, is recorded by truncation of the Aruma Group and Natih Formation, as well as part of the Shu’aiba Formation below the base Cenozoic unconformity. Seismic velocity and porosity anomalies from Lekhwair field in the northwest to the Huqf-Haushi...
FIGURES | View All (46)
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1969
AAPG Bulletin (1969) 53 (3): 626-671.
... on Precambrian rocks to Upper Cretaceous rocks of the Hawasina Group ( Figs. 4 , 5 ). The section is especially important to this study because it shows the sedimentary transition from Campanian neritic shale (Aruma-Muti) into the overlying abyssal sediments of the Hawasina Group and thus clarifies the origin...
FIGURES | View All (32)
Image
Geologic column of northern Oman showing major sedimentary <b>groups</b> (<b>ARUMA</b>) a...
in > GeoArabia
Published: 01 January 2002
Figure 2: Geologic column of northern Oman showing major sedimentary groups (ARUMA) and key formations (Muti), and major tectonic events that have affected the eastern Arabian margin and surrounding region. Modified from Naylor and Spring (2001) and Le Métour, Mitchel et. al. (1995). Arabian
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2009
GeoArabia (2009) 14 (1): 115-142.
... rocks exposed in Jabal Sumeini (Sumeini Group and Hamrat Duru Group) have been emplaced over uppermost Cretaceous Juweiza Formation conglomerates at the highest level of the Aruma foreland basin. These Sumeini D1 structures are abruptly truncated by an unconformity, above which are Middle Maastrichtian...
FIGURES | View All (17)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2010
GeoArabia (2010) 15 (1): 31-44.
... sequences. The older five Shiranish sequences are fourth order and grouped into one third-order sequence, while the sixth and youngest Shiranish Sequence was of third order. This suggests that the studied section was deposited in about 5 million years between ca. 76.0–74.4 and 69.5–69.8 Ma. The correlation...
FIGURES | View All (16)
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1973
AAPG Bulletin (1973) 57 (11): 2263-2279.
... and the Mishrif above, constitutes the upper part of the Wasia Group and is proved to be of middle Cenomanian-Turonian age. The Wasia Group is expanded to include the succession of sandstone and intercalated shaly bands extending from the top of the Buwaib Limestone (= Ratawi Limestone) to the base of the Aruma...
FIGURES | View All (8)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2014
GeoArabia (2014) 19 (1): 143-158.
... basin by thick Aruma and Pabdeh Group sediments. The low gravity is flanked to the west by a series of low-amplitude gravity highs. The highs are located in a region of generally high gravity anomaly that reflects the flexural bulge that flanks the UAE foredeep basin. The western area (salt tectonic...
FIGURES | View All (19)
Journal Article
Published: 01 December 2015
Journal of Sedimentary Research (2015) 85 (12): 1525-1551.
..., obduction of the Semail ophiolites, and formation of the Oman Foreland basin. As a consequence, carbonate sedimentation ended and syntectonic sediments (Aruma Group) were deposited in the subsiding foredeep. In Oligocene to Pliocene times, oceanic spreading in the Red Sea and the Gulf of Aden resulted...
FIGURES | View All (15)
Journal Article
Journal: GSA Bulletin
Published: 01 May 2016
GSA Bulletin (2016) 128 (5-6): 957-972.
... and sandstones of the Nahr Umr Formation; another unconformity separates the latter from the Natih Formation. The upper part of the Natih Formation is eroded and unconformably overlain by the shales and sandstones of the Aruma Group ( Fig. 2 ; e.g., Homewood et al., 2008 ). The Natih Formation, consisting...
FIGURES | View All (16)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 1997
GeoArabia (1997) 2 (1): 65-88.
... generation phase. At well E the Shu’aiba started generating oil during the Eocene (65 Ma) and is currently in the gas window. Unconformities were also accounted for in the burial reconstruction. The paleo-thickness of the partly eroded Aruma and Wasia groups were estimated. In southeast onshore Abu...
FIGURES | View All (27)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2015
GeoArabia (2015) 20 (1): 49-94.
...Hussain Fahad Al-Ajmi; Martin Keller; Matthias Hinderer; Claudio Miro Filomena ABSTRACT The Wajid Group is a Palaeozoic siliciclastic succession of southern Saudi Arabia. In the outcrop belt it is ca. 500 m thick, whereas in the subsurface, the thickness increases to more than 4,500 m...
FIGURES | View All (28)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 1998
GeoArabia (1998) 3 (4): 509-540.
... constructed from the intersection of the outcrop of the top of the Khanasir Member (Aruma Formation) with the detailed topography contours ( Figure 14b ), reveal that the regional slope of the Tertiary Aruma Formation, which is so prominently folded in the north-wall of the Sahba Fault, is left-laterally...
FIGURES | View All (32)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2012
GeoArabia (2012) 17 (2): 121-150.
... (Hawasina Complex) and syn-obduction foredeep sediments (Aruma Group) onto the Arabian continental margin spanned the Late Cretaceous ( Glennie et al., 1973 , 1974 ; Bernoulli and Weissart, 1987 ; Robertson, 1987 ; Béchennec et al., 1990 ; Cooper, 1990 ; Robertson and Searle, 1990 ). Passive margin...
FIGURES | View All (17)
Image
—Stratigraphic cross section of Cretaceous in northwestern Oman. Line of se...
Published: 01 May 1984
Figure 4 —Stratigraphic cross section of Cretaceous in northwestern Oman. Line of section is identical to that for Figure 3 . Eastward thickening of Aruma Group coincides with development and filling of Omani foredeep shown on Figure 1 .