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Ashkhabad Fault

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A: Quickbird satillite image (GoogleEarth) centered on the Kazandzhik <b>fault</b>...
in > Geology
Published: 01 December 2009
line. C: Simplified structural map of the Kopeh Dagh based on SPOT5 satellite images showing the major faults (white solid lines, simplified after Shabanian et al., 2009 ) and the fold axes (blue lines). D: Structural map of the north-central Kopeh Dagh showing the Ashkhabad fault based on SPOT5
Journal Article
Published: 01 July 1963
Bulletin of the Seismological Society of America (1963) 53 (4): 705–740.
...N. N. Ambraseys Abstract The Buyin-Zara earthquake of 1 September 1962 originated on the Ipak fault and it was felt over most of Northern Iran. This newly named fault and its branches run for 64 miles, from Ipak, about W-05°-N, across the mountains south of Buyin, to Takhrijin, 4 miles west of Ab-i...
Journal Article
Journal: Geology
Published: 01 December 2009
Geology (2009) 37 (12): e197–e198.
... line. C: Simplified structural map of the Kopeh Dagh based on SPOT5 satellite images showing the major faults (white solid lines, simplified after Shabanian et al., 2009 ) and the fold axes (blue lines). D: Structural map of the north-central Kopeh Dagh showing the Ashkhabad fault based on SPOT5...
FIGURES
Journal Article
Published: 01 August 1966
Bulletin of the Seismological Society of America (1966) 56 (4): 899–924.
... microseismicity was observed in areas of recent faulting. A lower level of activity, well above that of aseismic areas however, was observed at other sites in Nevada. Some indication of variation of microearthquake activity with time was obtained. Activity averaged over an interval of about ten hours usually...
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...
Journal Article
Published: 01 July 1962
Bulletin of the Seismological Society of America (1962) 52 (3): 485–505.
.... Gzovsky M. V. 1960 . Physical Theory of Tectonic Fault Origin , Sbornik (collection) “Problems of tectonophysics” , Gosgeoltekhizdat (National Press of Geological Technology) USSR . 34. Gzovsky M. V. 1960 . Principles of Modelling of Tectonic Processes , Sbornik (collection...
Journal Article
Published: 01 May 2007
Russ. Geol. Geophys. (2007) 48 (5): 429–441.
... China ( Kissin, 1988 ; Kissin et al., 1993 ). High-amplitude responses in these zones were recorded at long distances from the causative earthquakes (500 km or more) in the vicinity of large faults along block boundaries. The sensitive zones were noted to be the most changeable elements...
FIGURES | View All (12)
Journal Article
Published: 01 March 2003
Seismological Research Letters (2003) 74 (2): 107–123.
... earthquakes. The historic record in eastern Afghanistan within the Chaman Fault system on Afghanistan's eastern boundary with the Indian Plate is much sparser than in western Afghanistan, with merely three events in the period 800-1800 ( Figure 3 ). Moreover, different plate boundary processes prevail...
FIGURES | View All (7)
Journal Article
Published: 01 February 1978
Quarterly Journal of Engineering Geology and Hydrogeology (1978) 11 (1): 19–32.
... Ambraseys N. Some characteristic features of the Anatolian fault zone Tectonophys. 1970 9 143 165 Ambraseys N. Value of historical records of earthquakes Nature, Lond. 1971 232 5310 375 379 Ambraseys N. Earthquake hazards and emergency planning Bull. International...
Journal Article
Published: 17 March 2021
Russ. Geol. Geophys. (2021)
... ). As a whole, the Lahroud Complex is cut by two fault systems: the Angot Fault complex with a NW–SE trend and the Alahyarlou Fault in the west with a north–south trend ( Fig. 2 ). The younger gabbro in the area is fresher and is largely composed of noncumulate rocks with ophitic textures. It has partly...
FIGURES | View All (10)
Journal Article
Published: 01 August 2002
Bulletin of the Seismological Society of America (2002) 92 (6): 2310–2322.
... by the 1948 Ashkhabad earthquake is 19,800, although a much greater number (119,000) is also suggested; we used the first number. For the 1976 New Guinea earthquakes, the catalog NEIC gives 242 casualties but points out that there were between 5,000 and 9,000 missing people and presumed deaths; we noted 6,000...
FIGURES | View All (7)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1969
AAPG Bulletin (1969) 53 (8): 1649–1699.
... in the Indefatigable and Hewett structural complexes was extended by wells which proved gas in new fault segments. There was no activity in the German sector of the North Sea, and the offshore boundary dispute of Germany with Denmark and The Netherlands was still before the International Court of Justice...
FIGURES | View All (19)
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1977
AAPG Bulletin (1977) 61 (10): 1636–1697.
... holes in previous years. There were 2 new-field discoveries in the eastern Moray Firth basin and 4 in the middle of the North Sea near the median line with Norway. Other discoveries were made on separate fault blocks flanking the Ninian, Thistle, and North Cormorant fields. Confirmation wells were...
FIGURES | View All (30)
Journal Article
Published: 15 February 2017
Quarterly Journal of Engineering Geology and Hydrogeology (2017) 50 (1): 13–52.
... pipeline crossing the north–south grain of the Andes. Figure 1 shows typical pipelining in the region, where challenges included scaling ridges and scarps with up to 2000 m ascents, tropical rainfall up to 5 m a year, turbulent rivers, the main Andean eastern boundary faults close by, little or no level...
FIGURES | View All (24)