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Sulaiman Fault Zone

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Journal Article
Journal: Geology
Published: 01 January 1997
Geology (1997) 25 (1): 23–26.
...-northeast striking Chaman fault zone. It has been observed at oblique margins that the total plate motion is resolved into a component parallel to the margin, accommodated through strike-slip faulting, and a component normal to the margin taken up as contraction. However, the orientations of structures...
Journal Article
Journal: GSA Bulletin
Published: 01 May 1971
GSA Bulletin (1971) 82 (5): 1235–1250.
... the Himalayan arc appears to be affected by gigantic tear faults cutting across the east-west-trending fold and thrust axes. The tectonic pattern suggests that these cross structures are zones of differential lateral movement within the crust related to linear features of sea-floor spreading in the Indian Ocean...
Journal Article
Published: 01 June 1972
Bulletin of the Seismological Society of America (1972) 62 (3): 823–850.
... in eastern Persia, mechanism solutions vary from pure left-lateral strike-slip faulting to pure thrust faulting. Mechanism solutions for earthquakes on the Kirthar-Sulaiman shear zone in West Pakistan show consistent left-lateral strike-slip motion on a fault plane that strikes north-south...
Image
(A) Simplified tectonic map of the potential source terranes: Abbreviations...
Published: 01 September 2016
Figure 2. (A) Simplified tectonic map of the potential source terranes: Abbreviations: CHF—Chaman fault; JD—Jaz Murian depression; KB—Katawaz Basin; MAW—Makran accretionary wedge; MD—Mashkel depression; MF—Minab fault; OOB—Oman ophiolite belt; SFTB—Sulaiman fold-and-thrust belt; Sa-Si-Z—Sanandaj
Image
—Structural cross section of part (Mari pop-up <b>zone</b>) of the central Sulaima...
Published: 01 May 1994
Figure 8 —Structural cross section of part (Mari pop-up zone) of the central Sulaiman fold- and-thrust belt (from Jadoon et al., in press ). Notice pop-ups and associated reverse faults with minor throw of the top Cretaceous, Paleocene, and Eocene. These secondary faults emerging from
Image
—Structural cross section of the southern and central <b>Sulaiman</b> fold- and-th...
Published: 01 May 1994
from the southern zone are related to blind faults at depth. Structure of the central zone is highlighted in Figure 8 . The zone marked PROBLEM in the section represents the space that has to be filled by duplication of strata.
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1994
AAPG Bulletin (1994) 78 (5): 758–774.
...Figure 8 —Structural cross section of part (Mari pop-up zone) of the central Sulaiman fold- and-thrust belt (from Jadoon et al., in press ). Notice pop-ups and associated reverse faults with minor throw of the top Cretaceous, Paleocene, and Eocene. These secondary faults emerging from...
FIGURES | View All (17)
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1933
AAPG Bulletin (1933) 17 (3): 229–240.
... folds of great size. The oil fields are situated in a “foothill” zone of the Zagros arc. The high mountain front lies about 20 miles northeast of Masjid-i-Sulaiman and Haft Kel, and the mountains proper consist of tightly packed folds of Mesozoic and Paleozoic rocks. Still farther northeast...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 05 March 2021
Lithosphere (2021) 2021 (1): 7866954.
.... A. K. Khurshid S. Gravity and tectonic model across the Sulaiman fold belt and the Chaman fault zone in western Pakistan and eastern Afghanistan Tectonophysics 1996 254 1-2 89 109 10.1016/0040-1951(95)00078-X 2-s2.0-0029729977 Hubbard J. Shaw J. H. Klinger Y...
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Journal Article
Published: 01 May 2009
Journal of Micropalaeontology (2009) 28 (1): 7–23.
... foraminiferal and planktonic foraminiferal zones for Paleocene–Eocene stratigraphical units of the Lower Indus Basin. Biostratigraphical data are compiled from various sections of the Sulaiman and Kirthar ranges ( Eames, 1952 ; Nagappa, 1959 ; Shah, 1977 ; Köthe et al ., 1988 ; Weiss, 1993 ; Afzal, 1996...
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Image
—(A) Regional sketch map showing geographic position of Pakistan and tecton...
Published: 01 February 1997
) of the Indian plate relative to the Asian plate (after Jacob and Quittmeyer, 1979 ). AF = Altyn Tagh fault, BD = Bangladesh, CF = Chaman fault, HF = Herat fault, KF = Karakoram fault, MBT = Main Boundary thrust, MCT = Main Central thrust, MR = Murray Ridge, OFZ = Owen fracture zone, SL = Sri Lanka, SRT = Salt
Journal Article
Published: 01 December 2002
Bulletin of the Seismological Society of America (2002) 92 (8): 2893–2910.
... Western Pakistan and eastern Afghanistan Crustal structure from gravity and seismic reflection interpretation 1 21 Jadoon et al. 1996 Sulaiman foldbelt, Pakistan; Chaman fault zone, Pakistan-Afghanistan border Gravity and tectonic model 1 22 Jadoon et al. 1994a Central Sulaiman...
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Journal Article
Published: 01 October 1976
Bulletin of the Seismological Society of America (1976) 66 (5): 1695–1711.
... fault-plane solutions (Molnar et al., 1973). The seismicity in the Kirthar range is relatively diffuse compared to that in the Sulaiman range. At the latter seismicity falls on or near a very sharply defined frontal fault scarp which offsets the range against the eastward extending Indus basin. A zone...
Journal Article
Published: 01 June 2012
Mineralogical Magazine (2012) 76 (3): 717–723.
... across the Sulaiman fold belt and the Chaman fault zone in western Pakistan and eastern Afghanistan . Tectonophysics , 254 , 89 – 109 . Kassi A.M. Kelling G. Kasi A.K. Umar M. Khan A.S. ( 2009 ) Contrasting Late Cretaceous–Palaeocene lithostratigraphic successions...
FIGURES
Journal Article
Published: 01 September 1997
Journal of the Geological Society (1997) 154 (5): 753–756.
.... Khurshid A. Gravity and tectonic model across the Sulaiman fold belt and the Chaman fault zone in western Pakistan and eastern Afghanistan Tectonophysics 1996 254 89 109 Jadoon I.A.K. Lawrence R.D. Lillie R. J. McClay K. Balanced and retrodeformable cross-section from...
Journal Article
Published: 01 March 2011
Journal of the Geological Society (2011) 168 (2): 499–516.
..., Northern Suture; ITSZ, Indus–Tsangpo Suture Zone; TM, Tso Morari. (See Table 6 for main characteristics of these units.) Fig. 2. ( a ) Generalized geological map of the Sulaiman fold and thrust belt (modified from Jadoon et al. 1994 a ). Box shows the location of ( b ). PK, Pirkoh anticline...
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Journal Article
Published: 01 July 2009
Seismological Research Letters (2009) 80 (4): 599–608.
... (< 1.0) typical of a high-stress thrusting regime. However, higher values are seen in the Hazara syntaxis zone as well as to the northwest of the Karakoram fault, suggesting an underlying creeping tectonics. The spatial variations of δb indicate that the estimated b -values to be overall well within...
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Journal Article
Published: 01 June 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (2): 400–409.
... separated by tightly folded anticlines and/or thrust faults. Toward the east of the area, the trend of the fold belt becomes north-northwest to south-southeast. Seismic data from four surveys over the past nine years has demonstrated the presence of a triangle zone-type structure beneath the frontal...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 2004
AAPG Bulletin (2004) 88 (7): 1007–1035.
... Main Limestone. The correlation shows the increased clastic influx toward the northern Sulaiman Range and Jaisalmer basin, absence of Lutetian to Priabonian rocks in Trans-Indus Range, presence of an evaporatic sequence in Kohat, and a predominantly carbonate stratigraphy in Potwar. Formal names have...
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Journal Article
Published: 01 March 2003
Seismological Research Letters (2003) 74 (2): 107–123.
.... The shear displacement accommodated by block rotation is proportional to the aspect ratio of the blocks ( Figure 7 ). Assuming fault lengths of ≈100 km (the approximate width of the zone of faulting in Figure 5 ) and a uniform north-south separation of these faults of 30-50 km, the plate boundary slip rate...
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