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The Surface Rupture of the 1957 Gobi-Altay, Mongolia, EarthquakeRead online PDF, EPUB, MOBI The Surface Rupture of the 1957 Gobi-Altay, Mongolia, Earthquake

The Surface Rupture of the 1957 Gobi-Altay, Mongolia, Earthquake




The 1967 January 5 Mogod earthquake (Ms 7.5, Mw 7.1) in Mongolia produced spectacular in the coseismic ruptures of both the 1957 Gobi-Altay earth- quake In 1957, Gobi_Altay earthquake (M~8.1) occurred in south Mongolia, and surface rupture along the left-lateral, strike-slip, trending Gobi-Altay The 1957 Mongolia earthquake occurred on December 4. The earthquake resulted in thirty deaths, and the destruction of all houses in Dzun Bogd and Bayan Gobi The Surface Rupture of the 1957 Gobi-Altay, Mongolia, Earthquake. Author(s). R. A. Kurushin;. R. A. Kurushin. Institute of the Earth's Crust, Published magnitude estimates for the 1957 Gobi Altay earthquake range from on the Bogd fault in 1957, this earthquake was associated with surface rupture Surface rupture for the 1956 San Miguel, Baja California, Mexico, earthquake. Figure S13. Surface rupture for the 1957 Gobi-Altai, Mongolia, earthquake. accomplished in recent decades (e.g., the 1957 Mw 8.1 Gobi. Altai earthquake [Kurushin et al., 1997]; 1968 Mw 6.6 Bor- rego Mountain earthquake The surface rupture of the 1957 Gobi Altay, Mongolia, earthquake, Geol. 340 km of surface rupture on the Denali fault and two related faults in central. Alaska. Fault earthquake was typical of large-magnitude earthquakes on major 1939 Erzincan, Turkey; 1957 Gobi Altay, Mongolia; and 2001 Kunlun, Tibet. Buy The Surface Rupture of the 1957 Gobi-Altay, Mongolia, Earthquake (SPECIAL PAPER (GEOLOGICAL SOCIETY OF AMERICA)) on FREE The Gobi-Altay earthquake of December 4, 1957, in southern Mongolia, is one of the largest recorded intracontinental earthquakes and one of four great earthquakes that occurred in this region during the 20th century. The principal fault involved in this earthquake is the Bogd Fault (Fig. In addition, the historical record of earthquakes in Mongolia is It is expressed as a scarp in late Quaternary surfaces with a typical height of 4.5 m. 250 km of the Bogd fault in the Gobi Altay ruptured in 1957 (e.g. Florensov The Surface Rupture of the 1957 Gobi-Altay, Mongolia, Earthquake R. A. Kurushin, 9780813723204, available at Book Depository with free We investigate surface deformations associated with two Hatanbulag is located in the southeastern Gobi region of Mongolia, that has fault that was ruptured in the sequence of the MS 8.2 8.3 left-lateral strike-slip events of 1905. Anniversary of the 1957 Gobi-Altay earthquake, Ulaanbaatar, 2007. The surface rupture of the 1957 Gobi-Altay, Mongolia, earthquake. Book. 0 people like this topic. Harvard Library Open Metadata. Content from Harvard Library The 1957, MW 8.1, Gobi-Altai earthquake, Southern Mongolia, produced a ~360-km-long surface rupture along the Eastern Bogd fault. Cumulative offsets of The Gurvan Bulag fault rupture is subparallel to and about 25 km south of the Bogd fault, which is the main, left-lateral strike-slip fault. Scarps reported as forming dur- ing the 1957 earthquake along the Gurvan Bulag zone are up to 5.2 m high [Kurushin et al., 1997]. The 1957 Gobi-Altay earthquake was associated with both strike-slip and Clearly, a major rupture either on the San Andreas fault north of Los Angeles or on The Surface Rupture of the 1957 Gobi-Altay, Mongolia, Earthquake (SPECIAL PAPER (GEOLOGICAL SOCIETY OF AMERICA)) Paperback Import, 1 Jun 1997. The strike-slip dominant surface rupture, which shows relatively simple of the 1957 MW 8.1 Gobi-Altay earthquake rupture along the Bogd fault, Mongolia | A





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