1-20 OF 310 RESULTS FOR

Tabas Fault

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
Journal Article
Published: 01 December 1979
Bulletin of the Seismological Society of America (1979) 69 (6): 1861–1887.
...M. Berberian abstract The Tabas-e-Golshan earthquake of magnitude M s = 7.7 occurred in a region of east central Iran known to have been quiescent for at least 11 centuries. The shock was associated with 85 km of discontinuous thrust faulting at the surface along an existing but unrecognized late...
Journal Article
Journal: GSA Bulletin
Published: 01 November 2016
GSA Bulletin (2016) 128 (11-12): 1593–1617.
...Andrzej Konon; Alireza Nadimi; Marek Koprianiuk; Anna Wysocka; Rafał Szaniawski; Michał Wyglądała; Ewa Słaby; Soheyla Beygi; Marcin Barski Abstract The interaction of strike-slip faults in their restraining junctions allowed for the coeval formation of the Tabas and Abdoughi Basins and led...
FIGURES | View All (18)
Image
<span class="search-highlight">Fault</span> pattern in the northern part of the <span class="search-highlight">Tabas</span> block, earthquake distribut...
Published: 01 November 2016
Figure 8. Fault pattern in the northern part of the Tabas block, earthquake distribution, and Harvard Centroid Moment Tensor (CMT) focal mechanisms draped over a shaded-relief Shuttle Radar Topography Mission (SRTM) image. Distribution of earthquake epicenters is from the Iranian Seismological
Journal Article
Published: 01 February 1994
Bulletin of the Seismological Society of America (1994) 84 (1): 31–46.
...) . Quantitative Seismology—Theory and Methods , Vol. 1 , W. H. Freeman , San Francisco, Calif. Berberian M. (1979) . Earthquake faulting and bedding thrust associated with the Tabas-e-Golshan (Iran) earthquake of 16 September 1978 , Bull...
Image
Proposed model of the development of the intracontinental <span class="search-highlight">Tabas</span> and Abdough...
Published: 01 November 2016
Figure 18. Proposed model of the development of the intracontinental Tabas and Abdoughi Basins in the Tabas block. (A) Simplified present-day fault pattern in the Tabas block and Harvard Centroid Moment Tensor (CMT) focal mechanisms draped over a shaded-relief Shuttle Radar Topography Mission
Image
Examples of geomorphic features displaying active deformation in the <span class="search-highlight">Tabas</span> ...
Published: 01 November 2016
Figure 9. Examples of geomorphic features displaying active deformation in the Tabas fold belt marked on a Google Earth image. (A) Location of the Neyestan anticline and Tabas thrust bordering the W Fahalanj anticline. (B) Neyestan anticline cut by strike-slip faults. (C) Quaternary deposits
Image
(a) The original version of the film of the <span class="search-highlight">Tabas</span> acceleration time series ...
Published: 19 May 2021
(GMPEs) developed (for shallow crustal earthquakes) worldwide. The Tabas station was located at a 50 km distance from the earthquake epicenter. It was located three kilometers away from the main rupture of the associated fault. PGA, peak ground acceleration.
Image
Palaeogeography of the northern <span class="search-highlight">Tabas</span> Block in east-central Iran during the...
Published: 06 October 2022
Fig. 17. Palaeogeography of the northern Tabas Block in east-central Iran during the Middle Jurassic (early Bajocian). The meandering river system on the Kalmard sub-block and western part of the northern Tabas Block was sourced from the Yazd Block, grading into shallow-marine lithofacies
Image
Geographical and structural framework. (a) Geographic map of Iran with its ...
Published: 06 October 2022
Fig. 1. Geographical and structural framework. (a) Geographic map of Iran with its major fault systems and geological subdivision based on Shuttle Radar Topography Mission (SRTM) images. The northern Tabas Block area is indicated by a rectangle (faults modified from Konon et al . 2016 ). (b
Journal Article
Published: 06 October 2022
Geological Magazine (2023) 160 (2): 235–259.
...Fig. 17. Palaeogeography of the northern Tabas Block in east-central Iran during the Middle Jurassic (early Bajocian). The meandering river system on the Kalmard sub-block and western part of the northern Tabas Block was sourced from the Yazd Block, grading into shallow-marine lithofacies...
FIGURES | View All (17)
Journal Article
Published: 01 April 1991
Bulletin of the Seismological Society of America (1991) 81 (2): 305–331.
... the inversion runs indicates a complex, multiple source for the Tabas earthquake, with four main source regions over a fault length of 90 km and an average rupture velocity of 2.5 km / sec. 10 8 1990 Copyright © 1991, by the Seismological Society of America References...
Journal Article
Journal: GSA Bulletin
Published: 01 July 2007
GSA Bulletin (2007) 119 (7-8): 961–977.
... ). The Saghand area is in the western part of the central-east Iranian microcontinent, ∼100 km north-northeast of the axis of the Urumieh-Dokhtar arc (Fig. 1) . The central-east Iranian microcontinent is subdivided into three fault-bounded blocks, including (from east to west) the Lut, Tabas, and Yazd blocks...
FIGURES | View All (12)
Journal Article
Published: 01 February 1988
Bulletin of the Seismological Society of America (1988) 78 (1): 142–171.
... S. K. Urey H. C. , Editors Pergamon Press , Oxford, England , 117 - 165 . Berberian M. (1979) . Earthquake faulting and bedding thrust associated with the Tabas-e-Golshan (Iran) earthquake of September 16, 1978 , Bull...
Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP312.15
EISBN: 9781862395602
... not undertaken until the 1990s. Fig. 3. Locality map of the Tabas Block in east-central Iran. Asterisks labelled A–D refer to the approximate positions of lithostratigraphic successions shown in Figure 4. Block-bounding faults are approximately shown. Fig. 4. Lithostratigraphy of the Jurassic...
FIGURES | View All (8)
Image
(A–B) Active WNW-SSE–oriented sinistral strike-slip <span class="search-highlight">fault</span> recognized in the...
Published: 01 November 2016
Figure 11. (A–B) Active WNW-SSE–oriented sinistral strike-slip fault recognized in the northern part of the Tabas Basin. (C) Streams displaced by about several meters by sinistral offset.
Journal Article
Published: 01 December 1979
Bulletin of the Seismological Society of America (1979) 69 (6): 1851–1859.
... (Iran) catastrophic earthquake of 16 September 1978: a preliminary field report , Disaster 2 , 207 - 219 . Berberian M. (1979b) . Earthquake faulting and bedding thrust associated with the Tabas-e-Golshan (Iran) earthquake...
Image
(A) Distribution of Neogene (Ng) folded deposits in the southern part of th...
Published: 01 November 2016
Figure 15. (A) Distribution of Neogene (Ng) folded deposits in the southern part of the Tabas block and location of geomorphic features displaced along the Nayband fault (B) and along the Kuh Banan fault (C). (B) Offset of streams up to several dozen meters along the dextral strike-slip Nayband
Journal Article
Published: 01 February 1999
Bulletin of the Seismological Society of America (1999) 89 (1): 120–139.
... reverse fault systems. The two pairs of earthquakes may have ruptured different faults in each segment, similar to the 1971 and 1994 San Fernando, California, earthquakes. The 1978 Tabas reversefault earthquake was preceded by the 1968 Ferdows earthquake, part of the Dasht-e-Bayaz sequence. The North...
Journal Article
Journal: GSA Bulletin
Published: 01 May 2012
GSA Bulletin (2012) 124 (5-6): 943–956.
.... Paleomagnetic data show that in central Iran, crustal blocks bounded by sets of strike-slip faults are rotated to accommodate NNE-SSW shortening related to Arabia-Eurasia convergence. Counterclockwise rotations of 20°–35° have been measured in the Tabas and Anarak areas, south of the Great Kavir fault...
FIGURES | View All (8)
Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.195.01.10
EISBN: 9781862394438
... the Sanandaj-Sirjan Block of the Zagros, to north of Nikshahr in the east of the Makran. Other metamorphic rocks form the Deyader Complex near Fannuj on the southern margin of the Jaz Murian Depression. These include blueschists, and are thought to form the tip of the Tabas Microcontinental Block, largely...
FIGURES | View All (9)