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Koldor Graben

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Journal Article
Published: 01 December 2002
Russ. Geol. Geophys. (2002) 43 (12): 1099–1106.
... kilometers across. Most of normal faults cut the sides of the Teletsk and the adjacent Kamga and Koldor grabens, where the neotectonic vertical offset reaches its maximum of 400–1200 m (against <100–300 m in other grabens). Tectonic control of the surface topography in the region is evident from long V...
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Journal Article
Published: 01 February 2002
Russ. Geol. Geophys. (2002) 43 (2): 114–128.
...B. Dehandschutter; B.A. Bobrov; R. Hus; N.E. Astakhov; N.B. Androsova; Yu.P. Popov Lake Teletskoye, a major neotectonic unit of Gorny Altai, is a complexly structured graben formed during reactivation of Late Paleozoic fault zones. The formation of the graben in the northern part of the lake has...
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