1-20 OF 52 RESULTS FOR

Qeshm Island

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Image
Podocallichirus masoomi (Tirmizi, 1970), Qeshm Island, Persian Gulf, Iran, deposited under number NHMW 24990. 1, major left cheliped from lateral view; 2, major left cheliped (merus and carpus) from mesial view. Note the shape of meral blade and tuberculation on both, lateral and mesial, surfaces.
Published: 01 July 2012
F igure 3 Podocallichirus masoomi ( Tirmizi, 1970 ), Qeshm Island, Persian Gulf, Iran, deposited under number NHMW 24990. 1 , major left cheliped from lateral view; 2 , major left cheliped (merus and carpus) from mesial view. Note the shape of meral blade and tuberculation on both, lateral
Journal Article
Published: 01 May 2009
Journal of the Geological Society (2009) 166 (3): 387–391.
... at the end of the 15th century, suggests that this 1483 event was a moderate magnitude earthquake in the vicinity of Qeshm Island that has been misassociated with a second, later, earthquake. This interpretation removes from the earthquake catalogue any evidence for major earthquake activity along...
FIGURES
Image
Shaded relief map of the southeastern ZFTB. The solid boxes indicate Envisat and PALSAR (ALOS) image footprints used in this study. The locations of the Anguru salt diapir, Bandar-Abbas City and the Qeshm Island are labelled An, BA and QI, respectively. The inset shows the study area in Iran; the ZFTB is highlighted in green.
Published: 08 June 2021
Fig. 1. Shaded relief map of the southeastern ZFTB. The solid boxes indicate Envisat and PALSAR (ALOS) image footprints used in this study. The locations of the Anguru salt diapir, Bandar-Abbas City and the Qeshm Island are labelled An, BA and QI, respectively. The inset shows the study area
Image
Suffosion, soil loss and collapse in action, exposed in the side of a large dropout sinkhole on an exposed salt dome on Qeshm Island, Iran. Because the bedrock, visible below the dark red soil, is salt (halite), dissolution is very rapid and the karst is developing far more rapidly than in limestone, although the processes are essentially the same in both.
Published: 09 February 2016
Fig. 6. Suffosion, soil loss and collapse in action, exposed in the side of a large dropout sinkhole on an exposed salt dome on Qeshm Island, Iran. Because the bedrock, visible below the dark red soil, is salt (halite), dissolution is very rapid and the karst is developing far more rapidly than
Journal Article
Published: 01 April 1978
Bulletin of the Seismological Society of America (1978) 68 (2): 411–428.
... Belt. Previous earthquakes of the Bandar Abbas region The seismic history of the Bandar Abbas region is briefly presented here. For references see Berberian and Tchalenko (1976). Qeshm Island earthquake, 1360-1 Destructive. Strait of Hormoz, 1482-1483: A damaging shock at Hormoz and Oman. 414 M...
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1980
AAPG Bulletin (1980) 64 (12): 2095–2107.
.... This formation is a subsurface unit which extends throughout much of the southeastern Persian Gulf as well as the western part of Qeshm Island ( Fig. 1 ). The name Qeshm Formation is taken from Qeshm Island in the Persian Gulf. The formation has been drilled in various parts of the Persian Gulf. Figures 11...
FIGURES | View All (15)
Journal Article
Published: 15 April 2015
Seismological Research Letters (2015) 86 (3): 775–782.
.... Bayer R. Tavakoli F. , et al. ( 2003 ). GPS network monitors the Arabia–Eurasia collision deformation in Iran , J. Geod. 77 , nos.  7/8 , 411 – 422 . Nissen E. Ghorashi M. Jackson J. Parsons B. Talebian M. ( 2007 ). The 2005 Qeshm Island earthquake (Iran...
FIGURES
Journal Article
Published: 20 June 2017
Bulletin of the Seismological Society of America (2017) 107 (4): 1625–1641.
... of the Arabian and Eurasian plates ( Jackson and McKenzie, 1988 ), implying that aseismic shortening is significant in the Zagros. For the 2005 M w  5.8 Qeshm Island earthquake, the InSAR‐derived moment is double the estimate from body‐wave modeling ( Nissen et al. , 2010 ), and for the 2006 Fin...
FIGURES | View All (7)
Journal Article
Published: 08 January 2020
Seismological Research Letters (2020) 91 (2A): 758–769.
... , doi: 10.1016/j.jseaes.2018.02.009 . Lohman R. B. , and Barnhart W. D. 2010 . Evaluation of earthquake triggering during the 2005‐2008 earthquake sequence on Qeshm Island, Iran , J. Geophys. Res. 115 , no.  B12 , doi: 10.1029/2010JB007710 . Lohman R. B. Simons M...
FIGURES | View All (7)
Journal Article
Journal: Geology
Published: 07 October 2024
Geology (2025) 53 (1): 61–66.
... of geological structure in fold-thrust belts : Journal of Geophysical Research: Solid Earth , v. 126 , https://doi.org/10.1029/2021JB022045 . Nissen , E. , Ghorashi , M. , Jackson , J. , Parsons , B. , and Talebian , M. , 2007 , The 2005 Qeshm Island earthquake (Iran)—a link...
FIGURES | View All (4)
Journal Article
Journal: Geology
Published: 01 September 2011
Geology (2011) 39 (9): 815–818.
.... Yamini-Fard F. Tatar M. Gholamzadeh A. Bergman E. Elliott J.R. Jackson J.A. Parsons B. , 2010 , The vertical separation of mainshock rupture and microseismicity at Qeshm island in the Zagros fold-and-thrust belt, Iran : Earth and Planetary Science Letters , v. 296 , p. 181...
FIGURES | View All (4)
Journal Article
Published: 01 February 2011
Petroleum Geoscience (2011) 17 (1): 101–107.
..., such as the Gaversin diapir in the Qeshm Island to the west of the study area ( Figs 1 , 4 ), comprise generally circular domes above buried Hormuz salt. Type B diapirs, such as the Pol diapir, the one closest to the study area ( Fig. 4 ), are exposed at the surface with a high relief, suggesting recent emergence...
FIGURES | View All (9)
Journal Article
Published: 01 October 2018
Jour. Geol. Soc. India (2018) 92 (4): 491–497.
... processing with petro physical data will be dealt with ( Sadegi, 2009 ). Hengam field is located in Hormozgan Province and Strait of Hormuz, 40 km south of Qeshm island and 30 km south of Hengam island. Iran and Oman share Hengam oil field, while 80% of the filed lies in Iran’s coastal waters. Hengam...
FIGURES | View All (10)
Journal Article
Journal: Geophysics
Published: 23 October 2014
Geophysics (2014) 79 (6): KS43–KS49.
... receiver functions : Geophysical Journal International , 165 , 969–980 , doi: 10.1111/j.1365-246X.2006.02981.x . GJINEA 0956-540X Zarean A. Farrokhi M. Chaychizadeh S. , 2008 , Attenuation of high frequency P and S waves in Qeshm Island, Iran : Presented at 14th World Conference...
FIGURES | View All (9)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 1998
GeoArabia (1998) 3 (4): 509–540.
... Fault still further eastward across the Gulf floor from the southern end of Qatar to Qeshm Island at the coast of Iran. The Gulfward extension of the Nisah-Sahba Fault is named here the Trans-Arabian Gulf Fault. Qeshm Island is cored by a southwest-northeast trending anticline of Asmari Limestone...
FIGURES | View All (32)
Journal Article
Journal: Geology
Published: 16 July 2019
Geology (2019) 47 (9): 862–866.
... , https://doi.org/10.2205/2002ES000106 . Nissen , E. , Yamini-Fard , F. , Tatar , M. , Gholamzadeh , A. , Bergman , E. , Elliott , J.R. , Jackson , J.A. , and Parsons , B. , 2010 , The vertical separation of mainshock and microseismicity at Qeshm island...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1972
AAPG Bulletin (1972) 56 (10): 1965–1974.
... overlies the Asmari limestone except in Qeshm Island, where Pabdeh marl replaces the Asmari and directly underlies the evaporites ( Fig. 2 ). The last major period of marine deposition in the Zagros ended in the Oligo-Miocene, when the trough had developed into a broad, shallow foreland basin...
FIGURES | View All (12)
Journal Article
Published: 01 November 2011
Seismological Research Letters (2011) 82 (6): 815–823.
... 45 ( 6 ), 1,529 – 1,558 ; doi: 10.1109/TGRS.2006.888937 . Lohman , R. B. , and W. D. Barnhart ( 2010 ). Evaluation of earthquake triggering during the 2005–2008 earthquake sequence on Qeshm Island, Iran . Journal of Geophysical Research 115 ; doi: 201010.1029/2010JB007710...
FIGURES | View All (5)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1969
AAPG Bulletin (1969) 53 (8): 1764–1788.
... Ganoweh and Kharg Island. At Kharg the expansion will be completed during 1969. Table 9. Iran-IOEPC, Rigs. Active 12/31/68 Type of Well No. Rigs Active Total Exploration   3  Lab-e-Safid 1    Qeshm (Gevarzin) 1    Sardarabad 1 (Rigging up)   Development   3...
FIGURES | View All (5)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1962
AAPG Bulletin (1962) 46 (7): 1241–1280.
... continues. Khalafabad 1 .—Was drilled to 8,995 ft. in 1961 and reached the Asmari at 8,980 ft. Drilling continues. Three wells were drilled on Qeshm Island prior to 1951 but without finding oil. Qeshm 4 .—Was drilled to 5,116 ft. in 1961. Drilling continues. Fig. 7. —Iraq Petroleum...
FIGURES | View All (21)