Figure 12 - uploaded by Magda Patyniak
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Exposed scarp in the west trench-wall of the Belek site. South dipping faults are highlighted by red lines with arrows indicating the compared with the hanging-wall collapse fault scarp model modified after (Philip et al., 1992)
Source publication
This work presents an extended paleoseismic analysis of the Issyk-Ata fault scarp at the Belek site, northern Central Tien Shan, Kyrgyzstan. The Issyk-Ata fault is situated along the northern deformation margin of the Kyrgyz Range and south of Bishkek, the capital city of Kyrgyzstan. In the 20th century, a sequence of large magnitude earthquakes (≥...
