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Taq Taq Field

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Journal Article
Published: 02 May 2013
Petroleum Geoscience (2013) 19 (2): 139–155.
...A.H. Awdal; A. Braathen; O.P. Wennberg; G.H. Sherwani Abstract The Zagros Fold and Thrust Belt of NE Iraq hosts a prolific hydrocarbon system. Reservoirs are commonly found in fractured Cretaceous carbonates (Shiranish Formation) such as in the Taq Taq Field located in the Kirkuk Embayment...
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Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2010
DOI: 10.1144/0070801
EISBN: 9781862394131
... by the presence of oil. Fig. 6. ( a ) 2D seismic dip line across Taq Taq field. ( b ) The same line showing stratigraphic units and structural interpretation. The Taq Taq anticline is a response to shortening along a deep thrust plane lying below the base of the seismic section. Reverse faulting within...
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Series: Geological Society, London, Special Publications
Published: 01 January 2012
DOI: 10.1144/SP370.7
EISBN: 9781862396180
... Abstract Outcrop studies integrated with subsurface data of core, cuttings and different well logs were used to investigate reservoir characteristics of the Middle–Late Eocene Pila Spi Formation at Taq Taq oil field of Kurdistan Region of northeastern Iraq. Reservoir studies include...
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Image
(a) Geological map of the study area. The red dots indicate outcrop locations around the Bina Bawi and Taq Taq anticlines. The white dots are well locations in the Taq Taq Field. Note the proximity of the Bina Bawi and Taq Taq anticlines. The geological map is modified from Sissakian (1997). (b) Schematic cross-section of the study area across the Taq Taq and Bina Bawi anticlines. The thrust faults interpreted on a seismic section in a previous study (Garland et al. 2010) are bounded by the top Shiranish Formation. (c) Top Shiranish depth structure map, which shows the faults and location of the cross-section in (b). This structure map based on 2D seismic interpretation. (After TTOPCO 2006.)
Published: 02 May 2013
Fig. 2. ( a ) Geological map of the study area. The red dots indicate outcrop locations around the Bina Bawi and Taq Taq anticlines. The white dots are well locations in the Taq Taq Field. Note the proximity of the Bina Bawi and Taq Taq anticlines. The geological map is modified from Sissakian
Image
Rose diagrams of the strike of all fractures and faults interpreted in the XRMI image logs in wells: (a) TT-04; (b) TT-05; and (c) TT-06 in the Taq Taq Field.
Published: 02 May 2013
Fig. 16. Rose diagrams of the strike of all fractures and faults interpreted in the XRMI image logs in wells: ( a ) TT-04; ( b ) TT-05; and ( c ) TT-06 in the Taq Taq Field.
Image
Stereograms and rose diagrams of fractures in well TT-04 interpreted from XRMI image logs. (a) Conductive fractures, (b) induced fractures, and (c) fracture frequency in XRMI image logs for reservoir units in the Taq Taq Field.
Published: 02 May 2013
Fig. 17. Stereograms and rose diagrams of fractures in well TT-04 interpreted from XRMI image logs. ( a ) Conductive fractures, ( b ) induced fractures, and ( c ) fracture frequency in XRMI image logs for reservoir units in the Taq Taq Field.
Image
Seismic sections of selected hydrocarbon accumulations in Kurdistan showing he variety of structural style displayed in three of the significant discoveries in the region: Shaikan Field (courtesy of Gulf Keystone); Taq Taq Field (courtesy of Genel Energy); and Kurdamir Field (courtesy of Western Zagros, see Figure 18). For location see Figure 11.
Published: 01 April 2015
Figure 15: Seismic sections of selected hydrocarbon accumulations in Kurdistan showing he variety of structural style displayed in three of the significant discoveries in the region: Shaikan Field (courtesy of Gulf Keystone); Taq Taq Field (courtesy of Genel Energy); and Kurdamir Field (courtesy
Image
Images of a wide-open fracture with a 3 mm-thick layer of calcite on each fracture surface, detected from (a) an image log and (b) core. The images are from the Shiranish Formation in the Taq Taq Field. The image log and core are 1 m in length and 10 cm in diameter.
Published: 02 May 2013
Fig. 15. Images of a wide-open fracture with a 3 mm-thick layer of calcite on each fracture surface, detected from ( a ) an image log and ( b ) core. The images are from the Shiranish Formation in the Taq Taq Field. The image log and core are 1 m in length and 10 cm in diameter.
Image
(a) Regional tectonic map of the Zagros fold and thrust belt. The red line indicates the Zagros Suture, which extends from NW to SE. The study area is indicated by the yellow rectangular box. (b) Simplified tectonic map of Kurdistan, NE Iraq showing the main tectonic zones of the Zagros fold and thrust belt. Note the locations of the Bina Bawi Anticline (star) and the Taq Taq Field (dot). The study area (black rectangular box) is located 40 km east of Erbil city, and 60 km NE of Kirkuk. Modified from Jassim & Goff (2006).
Published: 02 May 2013
of the Zagros fold and thrust belt. Note the locations of the Bina Bawi Anticline (star) and the Taq Taq Field (dot). The study area (black rectangular box) is located 40 km east of Erbil city, and 60 km NE of Kirkuk. Modified from Jassim & Goff (2006) .
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2015
GeoArabia (2015) 20 (2): 181–220.
...Figure 15: Seismic sections of selected hydrocarbon accumulations in Kurdistan showing he variety of structural style displayed in three of the significant discoveries in the region: Shaikan Field (courtesy of Gulf Keystone); Taq Taq Field (courtesy of Genel Energy); and Kurdamir Field (courtesy...
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Image
(A) Petroleum systems event chart (format modified from Magoon and Dow, 1994) for the Middle–Upper Jurassic (Sargelu–Naokelekan) sourced petroleum system in northern Iraq. The main phase of trap formation in the frontal part of the Zagros fold belt in Iraq occurred during the Late Miocene and Pliocene (e.g., Garland et al., 2010; Bretis et al., 2011; Reif et al., 2011; Csontos et al., 2012), although it is possible that older structural and stratigraphic traps were formed before this. (B) Thermal history curves and oil and kerogen–gas transformation-ratio curves illustrating the timing and extent of petroleum generation at (i) Kirkuk (Baba Dome) field, and (ii) Khashm al-Ahmar field (reproduced from Pitman et al., 2004, by permission of GeoArabia). Within the central Iraqi Zagros, the main phase of oil generation is interpreted to have occurred during the Neogene at the Kirkuk field (Pitman et al., 2004), and in the last 10 m.y. at the Taq Taq field (Al-Ameri and Zumberge, 2012; Al-Ameri et al., 2014). However, the timing of oil generation and expulsion from the Jurassic source rocks will vary across the region in accordance with differing burial histories. For example, further southeast along the Iraqi Zagros, where both the Upper Cretaceous and Cenozoic sections are thicker, oil generation from the Jurassic source rocks is interpreted to have begun in the Late Cretaceous at the Kashm-al-Ahmar field (Pitman et al., 2004). It is worth noting that the thermal history models presented by Pitman et al. (2004) may underestimate the onset of oil generation in northern Iraq on the basis of the high-sulfur contents in the kerogens analyzed in this study (Figure 14; Table 4).
Published: 01 February 2015
at the Kirkuk field ( Pitman et al., 2004 ), and in the last 10 m.y. at the Taq Taq field ( Al-Ameri and Zumberge, 2012 ; Al-Ameri et al., 2014 ). However, the timing of oil generation and expulsion from the Jurassic source rocks will vary across the region in accordance with differing burial histories
Journal Article
Journal: AAPG Bulletin
Published: 01 October 2003
AAPG Bulletin (2003) 87 (10): 1653–1680.
...F. N. Sadooni; A. S. Alsharhan Abstract The Albian–Cenomanian Mauddud Formation extends over most parts of the Arabian basin including north Iraq. The formation consists mainly of Orbitolina -bearing limestone with local basin margin rudist buildups in the offshore North field of Qatar...
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Image
A plot of pristane/n-C17 versus phytane/n-C18 for crude oils can be used to infer oxicity and organic-matter type in the source rock depositional environment (Peters et al., 1999). Increasing biodegradation and thermal maturity displace points toward the upper right and lower left, respectively (Peters et al., 2005). (A) Crude oils hosted in Triassic–Cenozoic reservoirs in northern Iraq and Syria are generally derived from marine algal type II organic matter deposited in a reducing environment. Source rock extracts from Triassic–Cenozoic organic-rich horizons in the same region display a similar composition, with the exception of extracts from the Palaeocene–Eocene Aaliji Formation, which suggest mixed type II/III organic matter deposited in a more oxic environment. (B) A subset of data plotted according to field name and reservoir age illustrates that oils in Cretaceous reservoirs tend to display higher maturity than their Cenozoic equivalents. In addition, the maturity of the Cretaceous-hosted oils varies spatially with the Taq Taq and Kirkuk oils displaying a more mature signature than the Tawke oil (see locations of these fields in Figure 13). Data sources include Abboud et al. (2005); Al-Ahmed (2006); Ahmed (2007); Baban (2008); Mohyaldin (2008); Qadir (2008); Ranyayi (2009); Abdula (2010); Al-Ameri et al. (2011); Al-Ameri and Zumberge (2012).
Published: 01 February 2015
Triassic–Cenozoic organic-rich horizons in the same region display a similar composition, with the exception of extracts from the Palaeocene–Eocene Aaliji Formation, which suggest mixed type II/III organic matter deposited in a more oxic environment. (B) A subset of data plotted according to field name
Journal Article
Published: 01 February 2010
Earthquake Spectra (2010) 26 (1): 309–310.
... negative, and the text is fraught with overstated examples on the perils of reinforced concrete and the insensitivity of the engineering profession. The Indian Building Code recommends using reinforcing steel in the vertical boundaries of masonry panels in taq construction. This, indeed, can...
Journal Article
Published: 01 December 2017
Earthquake Spectra (2017) 33 (1_suppl): 299–319.
... the practices in the region, leading to the complete ban of contemporary construction methods in the preservation field within Nepal. Thus no “contemporary stamp” was allowed on reconstructed or restored historic sites. Based on this law, the use of concrete or steel for structural reinforcement in historic...
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Book Chapter

Author(s)
J. Redfern, J. Craig
Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2010
DOI: 10.1144/0070671
EISBN: 9781862394131
... of the Taq Taq Field, located within an anticline in the gently folded zone of the Zagros mountains, northeastern Iraq. This paper reviews the main reservoirs and the importance of characterizing the pervasive fracture system, which provides the reservoir connectivity and deliverability. The authors describe...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 2015
AAPG Bulletin (2015) 99 (2): 231–272.
... at the Kirkuk field ( Pitman et al., 2004 ), and in the last 10 m.y. at the Taq Taq field ( Al-Ameri and Zumberge, 2012 ; Al-Ameri et al., 2014 ). However, the timing of oil generation and expulsion from the Jurassic source rocks will vary across the region in accordance with differing burial histories...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2004
GeoArabia (2004) 9 (4): 41–72.
..., 1989; PGA, 2000 ). Two samples of source rock from the Naokelekan, one each from Kirkuk and Taq Taq fields, have low HI values and high T max values that are indicative of oil-generation completion at relatively shallow burial depths. The sample from Kirkuk field (Kirkuk 109 well; see Figure 1 ) has...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2015
GeoArabia (2015) 20 (3): 99–140.
... samples in the Sargelu outcrop and in the Jebel Kand-1, Samand-1 and Taq Taq-1 wells represent reduced, oil- to dry-gas mature values ( Table 1 ). The measured TOC values in this region can be as high as 10–16 wt%, especially at Tawke Field ( Abdulla, 2010 ) and in the Ghali Kuh outcrop in Iran ( Ashkan...
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Journal Article
Published: 01 August 1967
Bulletin of the Seismological Society of America (1967) 57 (4): 817–820.
... effect in order to give a very thin and undistorted bright line on the photocell grid. A distorted line would not give sharp pulses and the correction would be impaired. Next to the bulb is a good grade condensing lens, F 3.5, 5 em. F.L. flat field. The purpose of that condenser is to give a brighter...