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Taurus-Zagros

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Journal Article
Published: 01 November 1991
Geological Magazine (1991) 128 (6): 561–584.
Image
—Regional map showing the position of the Taurus-Zagros large block relative to the major tectonic elements of the area. Stress directions from Jackson and McKenzie (1984).
Published: 01 March 1992
Figure 8 —Regional map showing the position of the Taurus-Zagros large block relative to the major tectonic elements of the area. Stress directions from Jackson and McKenzie (1984) .
Image
—(a) Regional structural subdivisions of the Taurus-Zagros Ranges of northern Iraq. Lines 1–4 indicate the position of the profile sections shown in Figure 4b. (b) A schematic map showing the position of the exposure of the Precambrian basement in the Arabian peninsula.
Published: 01 March 1992
Figure 1 —(a) Regional structural subdivisions of the Taurus-Zagros Ranges of northern Iraq. Lines 1–4 indicate the position of the profile sections shown in Figure 4b . (b) A schematic map showing the position of the exposure of the Precambrian basement in the Arabian peninsula.
Journal Article
Published: 01 June 2009
Russ. Geol. Geophys. (2009) 50 (6): 517–534.
.... Chemical composition of chromian spinels indicates that they are derived from Alpine-type peridotite. The ophiolitic-radiolarite belts of Taurus-Zagros as well as the uplifted Cretaceous and Paleocene strata of north and northeastern Iraq are likely to be the major source of clastics to the Fat’ha–Injana...
FIGURES | View All (17)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1991
AAPG Bulletin (1991) 75 (7): 1215–1232.
.... From the Middle Jurassic to the Late Cretaceous the extensional basin became a passive margin on which clastics alternated cyclically with carbonate platforms. This sequence provided sandstone and carbonate reservoirs sealed by shale and marl. Late Cretaceous convergence along the Taurus-Zagros front...
FIGURES | View All (13)
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1974
AAPG Bulletin (1974) 58 (6): 973–981.
... structure, but this time with northeast-southwest trends. There was no apparent movement on the first-phase fault system during the activity of the second phase of faulting. Following the end of the Cretaceous, the diastrophism reverted again to the epeirogenic style until the Taurus-Zagros orogenic folding...
FIGURES | View All (10)
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1952
AAPG Bulletin (1952) 36 (10): 1885–1901.
...N. E. Baker; F. R. S. Henson ABSTRACT The Middle East geological provinces are: (1) the Arabo-Nubian and Arabo-Somali massifs of pre-Cambrian igneous and metamorphic rocks in western and southern Arabia; (2) the foreland shelf, north and east of the massifs; and (3) the orogenic Taurus-Zagros-Oman...
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Image
A: Sampling locations shown with the background of maximum extent of Lisan at 26 ka in blue. B: Tectonic plates in the Middle East. Dead Sea Transform (DST) transfers the opening motion in the Red Sea to the Taurus-Zagros collision zone. C: Landsat image of sampling region.
Published: 01 April 2010
Figure 1. A: Sampling locations shown with the background of maximum extent of Lisan at 26 ka in blue. B: Tectonic plates in the Middle East. Dead Sea Transform (DST) transfers the opening motion in the Red Sea to the Taurus-Zagros collision zone. C: Landsat image of sampling region.
Image
—Schematic map showing the development of the Mosul and Kirkuk blocks (or subbasins) as parts of the thinning, passive margins, Taurus-Zagros basin of the Afro-Arabian plate. Thinning took place by extensional (longitudinal) faulting (dashed lines) and (transverse) strike-slip faulting (solid lines). The plate positions are based on Dercourt et al. (1986, their Figure 2a).
Published: 01 March 1992
Figure 7 —Schematic map showing the development of the Mosul and Kirkuk blocks (or subbasins) as parts of the thinning, passive margins, Taurus-Zagros basin of the Afro-Arabian plate. Thinning took place by extensional (longitudinal) faulting (dashed lines) and (transverse) strike-slip faulting
Image
(a) Tectonic plates in the Middle East. General tectonic map showing the location of the present Dead Sea Fault (DSF). The Dead Sea Fault transfers the opening motion in the Red Sea to the Taurus–Zagros collision zone. (b) Generalized map showing the maximum extent of Lake Lisan along the Dead Sea Fault at 26 ka. (c) Map of the Dead Sea showing the positions of localities referred to in the text and Table 2.
Published: 01 January 2012
Fig. 1. ( a ) Tectonic plates in the Middle East. General tectonic map showing the location of the present Dead Sea Fault (DSF). The Dead Sea Fault transfers the opening motion in the Red Sea to the TaurusZagros collision zone. ( b ) Generalized map showing the maximum extent of Lake Lisan along
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1992
AAPG Bulletin (1992) 76 (3): 356–370.
...Figure 8 —Regional map showing the position of the Taurus-Zagros large block relative to the major tectonic elements of the area. Stress directions from Jackson and McKenzie (1984) . ...
FIGURES | View All (12)
Image
—(a) The regional basement tectonic pattern of northern Iraq showing the borders (lines 1–8) of the Mosul and Kirkuk blocks and the longitudinal and transverse faults which break the blocks into smaller subblocks (see text for details). Notice that other longitudinal and transverse faults apart from those shown on the map do occur, as evident from Figure 5. (b) Transverse profile sections of depth of sedimentary basin floor in the present Taurus-Zagros basin compared with profiles of the quasibathymetry of the basins of the middle Jurassic to middle Miocene (after Ameen, 1991, his Figure 5). Locations of the profiles are shown in Figure 1.
Published: 01 March 1992
faults apart from those shown on the map do occur, as evident from Figure 5 . (b) Transverse profile sections of depth of sedimentary basin floor in the present Taurus-Zagros basin compared with profiles of the quasibathymetry of the basins of the middle Jurassic to middle Miocene (after Ameen, 1991
Image
—(a) Schematic section in the Zagros-Taurus orogenic belt illustrating the relationship of the geowarping in the sedimentary cover to the differential movement on reverse basement faults or fault stacking (after Ameen, 1991, his Figure 7). (b) Regional map of north Iraq and southwest Iran showing the distribution of productive oil and gas fields. Notice that the majority of the fields are in the downwarped parts of the geowarpings (after Ameen, 1991, his Figure 4).
Published: 01 March 1992
Figure 9 —(a) Schematic section in the Zagros-Taurus orogenic belt illustrating the relationship of the geowarping in the sedimentary cover to the differential movement on reverse basement faults or fault stacking (after Ameen, 1991 , his Figure 7 ). (b) Regional map of north Iraq and southwest
Journal Article
Published: 01 April 1971
Bulletin of the Seismological Society of America (1971) 61 (2): 317–341.
... continuous line of epicenters along the Zagros-Taurus mountains and the Levant fracture zone. The entire series of elongated foothills of the Zagros is a region in which the crustal rocks are contracted by folding, faulting, or a combination of both. The seismic and geological evidence can be explained most...
Book Chapter

Author(s)
Mohammed S. Ameen
Series: EAGE Education Tour Series
Publisher: EAGE
Published: 01 January 2018
EISBN: 9789462824508
... exploration and geotechnical projects, e.g. nuclear waste repositories, strategic gas storage in depleted reservoirs, tunnel stabilities etc. Ameen started his career working as an explorationist by pioneering comprehensive fractures and fold traps characterization across the Taurus-Zagros of Iraq...
FIGURES
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2012
GeoArabia (2012) 17 (2): 81–116.
... encompasses a prominent change in structural orientation of the northern Zagros, from a general NW-SE “Zagros” to an E-W “Taurus” trend. Geological mapping and structural observations, both in the mountains (Mesozoic–Palaeogene) and in the lowlands (Neogene), led to the following conclusions. (1) The oldest...
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Image
A map showing the regional anticlinal structures around the Shaikan Field, in the Taurus and Zagros orogenic trend. It can be seen that the Taurus trend, shown by blue axial hinges, is an east–west trend. The Zagros trend, with red axial hinges, is a more northwesterly–southeasterly trend. The Shaikan anticline resides within the conjunction of these two trends and also forms the starting sequence of en echelon sigmoidal shape folds that overlie a major basement strike-slip fault, the Kochuk–Dohuk Fault (cf. Burberry 2015). Recent seismic activity along this fault suggests the region is critically stressed (Heidbach et al. 2016).
Published: 18 September 2020
Fig. 1. A map showing the regional anticlinal structures around the Shaikan Field, in the Taurus and Zagros orogenic trend. It can be seen that the Taurus trend, shown by blue axial hinges, is an east–west trend. The Zagros trend, with red axial hinges, is a more northwesterly–southeasterly trend
Journal Article
Journal: AAPG Bulletin
Published: 01 January 2010
AAPG Bulletin (2010) 94 (1): 27–60.
... reservoirs. He has published 25 articles on fractures and folds, and has edited three special publications for the Geological Society (London). He conducted the first classic work on the fractures and folds across the Taurus-Zagros Range, Iraq, covering 30 major fold traps. The work is published in the AAPG...
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Journal Article
Published: 18 September 2020
Journal of the Geological Society (2020) 177 (6): 1315–1328.
...Fig. 1. A map showing the regional anticlinal structures around the Shaikan Field, in the Taurus and Zagros orogenic trend. It can be seen that the Taurus trend, shown by blue axial hinges, is an east–west trend. The Zagros trend, with red axial hinges, is a more northwesterly–southeasterly trend...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1967
AAPG Bulletin (1967) 51 (3): 469–470.
...Richard L. Hester The most prolific oil-producing area of the Middle East lies on the southern flank or extension of the ancient Asiatic Tethyan geosyncline and was at least partly subjected to the same tectonic forces which produced the Alpine-Taurus-Himalayan Mountains. The importance...