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Tanjero Formation

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Journal Article
Published: 01 July 1986
Micropaleontology (1986) 32 (3): 215-231.
Journal Article
Published: 08 July 2011
Geological Magazine (2011) 148 (5-6): 925-939.
... unconformity exists between Lower Cretaceous and Paleocene–Eocene rocks and the second between the Campanian Shiranish Formation and the Maastrichtian Tanjero Formation. Each of these unconformities is found in two different localities in the Zagros Imbricate Zone (i.e. the highly deformed zone immediately SW...
Image
The contact between the interfingering interval of the Aqra–<b>Tanjero</b> formati...
Published: 24 January 2014
Figure 4. The contact between the interfingering interval of the Aqra–Tanjero formations and the overlying red beds, Mawat–Chwarta area (Sorakalat section). (a) Limestone bed (L) overlain by olive mudstone dipping 35° NE in the upper Tanjero Formation
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2008
GeoArabia (2008) 13 (1): 39-54.
.... In the type section it has a thickness of 315 m (1,033.2 ft), but away from this area the formation wedges out relatively rapidly and (mainly towards the southeast) it forms tongues of relatively small thickness within the Shiranish and Tanjero formations ( Buday, 1980 ). Lithology: R. Wetzel (1950...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2010
GeoArabia (2010) 15 (1): 31-44.
... Formation, Jib’ab Marl), fore- or back-reef limestones (Bekhme, Aqra and obsolete “Pilsener” formations) and clastics (Tanjero Formation) ( Dunnington, 1958-2005 ; van Bellen et al., 1959 -2005; Jassim and Goff, 2006 ; Al-Mutwali et al., 2008 ). These formations can pass below, above or inter-tongue...
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Journal Article
Published: 01 May 2013
Petroleum Geoscience (2013) 19 (2): 139-155.
.... 1959 ; Sadooni 1996 ). The upper boundary of the Shiranish Formation is conformable and gradational towards the overlying Tanjero Formation ( Jassim & Goff 2006 ). The Tanjero Formation is believed to have shed more clastics into the marly upper succession of the Shiranish Formation...
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Book Chapter

Series: AAPG Memoir
Published: 01 January 2014
DOI: 10.1036/13431863M1063618
EISBN: 9781629812663
... and gas occurs in reservoirs of Cenozoic and Cretaceous age. The largest reserves occur in: 1) carbonate rocks of the Kirkuk Group (Lower Miocene–Oligocene), in fields within the Zagros foldbelt of northeastern Iraq, the largest being Kirkuk field; 2) carbonate rocks of the Mishrif Formation (Turonian...
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Image
Geological context for the Azmer (1) and Dokan (2) sections of the Kometan ...
Published: 01 July 2015
is located about 15 km to the NE of Sulaimani city. Small black rectangle on inset map represents study area. The map distribution of the Shiranish Formation is conjoined with the overlying Tanjero Formation based on the original figure by Sissakian (2000) . Without a new geological survey the boundary
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2012
GeoArabia (2012) 17 (2): 81-116.
... the systematic joint sets described above. Bituminous surfaces can even be found in the more ductile marls of the Shiranish Formation ( Figures 13a and 13b ). It is remarkable that in the Bekhme Gorge the Tanjero Formation above the Shiranish marl does not contain shows, and the Shiranish shows are solely...
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Journal Article
Published: 01 July 2015
Journal of Micropalaeontology (2015) 34 (2): 105-138.
... is located about 15 km to the NE of Sulaimani city. Small black rectangle on inset map represents study area. The map distribution of the Shiranish Formation is conjoined with the overlying Tanjero Formation based on the original figure by Sissakian (2000) . Without a new geological survey the boundary...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2015
GeoArabia (2015) 20 (3): 99-140.
..., Tanuma, Sadi, Kometan, Hartha, Shiranish, Aqra/Bekhme, Tanjero Formations Surgah, Ilam, Gurpi, Amiran Formations Reservoir Limestone (shaly) 90–59.8 13–0 12.2 AP8 Albian to Lower Turonian Mauddud, Rutbah, Ahmadi, Rumaila, Kifl, Balambo Formations Sarvak Formation Reservoir Limestone...
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Journal Article
Published: 24 January 2014
Geological Magazine (2014) 151 (6): 1034-1050.
...Figure 4. The contact between the interfingering interval of the Aqra–Tanjero formations and the overlying red beds, Mawat–Chwarta area (Sorakalat section). (a) Limestone bed (L) overlain by olive mudstone dipping 35° NE in the upper Tanjero Formation...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2014
GeoArabia (2014) 19 (1): 161-180.
... deposits of the Tanjero Formation (Late Maastrichtian) ( Figure 2 ). van Bellen et al. (1959-2005) informally subdivided the Shiranish Formation into a ‘lower unit’, characterised by alternating foraminifer-rich marly limestone and calcareous marlstone, and an ‘upper unit’ that is dominated by blue...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2011
GeoArabia (2011) 16 (1): 151-203.
... sections (Qamchuqa, Dokan, Smaqwly and Safin), and correlated with oil wells (Taq-Taq and Chemchemal). The sequence consists of the Qamchuqa, Dokan, Gulneri, Kometan, Shiranish and Tanjero formations, which were deposited in a pre-foreland and foreland basin between the Barremian to the Late Maastrichtian...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2012
GeoArabia (2012) 17 (4): 109-156.
... along the Balambo and Azmur anticlines ( Ibrahim, 2009 ). The more competent Balambo and Kometan formations were thrusted along the fault over the low-elevated incompetent rocks of the Shiranish and Tanjero formations. The fault has been displaced dextrally as in the Halabja-Said Sadiq area due...
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Series: AAPG Memoir
Published: 01 January 2019
DOI: 10.1306/13642165M1183798
EISBN: 9781629812823
... and thickness of these systems is another key task for the explorationist. Known important reservoirs and seals include the Early Triassic Sudair, the Middle Jurassic Dhruma, and the Cretaceous Zubair, Gadvan, Burgan, Nahr Umr, Ahmadi, Tuwayil, and Tanjero formations. All of these formations exhibit marked...
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Journal Article
Published: 01 January 2011
Journal of the Geological Society (2011) 168 (1): 235-250.
.... From internal to external areas, time lines cross the formation boundaries from continental Kashkan red beds to Taleh Zang mixed clastic–carbonate platforms, Amiran slope deposits and basinal Gurpi–Pabdeh shales and marls. The foreland basin depocentres show a progressive migration from the Campanian...
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Journal Article
Published: 11 July 2011
Geological Magazine (2011) 148 (5-6): 819-837.
... components to the mantle wedge relied heavily on the composition of the sedimentary inputs. These vary considerably with time from the relatively deepwater hemipelagic sediments (Qulqula Radiolarite Formation) to platform carbonate sediments (Balambo limestone). The trace element signatures of the GQR...
Series: AAPG Memoir
Published: 01 January 2014
DOI: 10.1036/13431862M1063612
EISBN: 9781629812663
... Formation ( Mouty, 1997a , b). In Syria the Levant fault delimits the Coastal range to the east. This N-S 1200 km (745 mi) long left-lateral strike-slip fault accommodates about 105 km (65 mi) of displacement since Miocene between the Arabian and Nubian plates (e.g., Quennel, 1958 ; Freund et al., 1970...
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Image
Structural features associated to major folding. (a) Crestal collapse in th...
in > GeoArabia
Published: 01 April 2012
Figure 8: Structural features associated to major folding. (a) Crestal collapse in the core of Bekhme Anticline, uninterpreted. (b) Same, interpreted. Note small offset normal faults (red lines) in well-layered Qamchuqa Formation (Bekhme Gorge, NW face). (c) Smaller internal thrusts in the core