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USGS · 70162504

The Talas-Fergana Fault, Kirghiz and Kazakh, USSR

Abstract

The great Talas-Fergana fault transects the Soviet republic of Kirghiz in Soviet Central Asia and extends southeastward into China and northwestward into Kazakh SSR (figs. 1 and 2). This great rupture in the Earth's crust rivals the San Andreas fault in California; it is long (approximately 900 kilometers), complex, and possibly has a lateral displacement of hundreds of kilometers similar to that on the San Andreas fault. The Soviet geologist V. S. Burtman suggested that right-lateral offset of 250 kilometers has occurred, citing a shift of Devonian rocks as evidence (fig. 3). By no means do all Soviet geologists agree. Some hold the view that there is no lateral displacement along the Talas-Fergana fault and that the anomalous distribution of Paleozoic rocks is a result of the original position of deposition.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 41.80407814427234° to 50.401515322782366° latitude; 71.630859375° to 92.2412109375° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

R. E. Wallace. 1976. The Talas-Fergana Fault, Kirghiz and Kazakh, USSR. https://pubs.usgs.gov/publication/70162504

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