1-7 OF 7 RESULTS FOR

Ottug-Taiga-Azas fault zone

Results shown limited to content with bounding coordinates.
Save search
Follow your search
Access your saved searches in your account
Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article

PALEOSEISMIC DISLOCATIONS IN THE OTTUG-TAIGA-AZAS FAULT ZONE ( Eastern Tuva )

S. G. Arzhannikov
Published: 01 November 2000
Russ. Geol. Geophys. (2000) 41 (11): 1445–1453.
..., and terminates near the Ulug-Arga Ridge. The Ottug-Taiga system of faults inherits the Azas linear interblock zone dating back to the Cambrian, which was then an area of intense downwarping and accumulation of volcanosedimentary beds of the Tumat-Taiga Formation [ 30 ]. The additional studies I carried...
FIGURES
View PDF for article title, PALEOSEISMIC DISLOCATIONS IN THE <span class="search-highlight">OTTUG</span>-<span class="search-highlight">TAIGA</span>-<span class="search-highlight">AZAS</span> <span class="search-highlight">FAULT</span> <span class="search-highlight">ZONE</span> ( Eastern Tuva )
Purchase
Add to Citation Manager for PALEOSEISMIC DISLOCATIONS IN THE <span class="search-highlight">OTTUG</span>-<span class="search-highlight">TAIGA</span>-<span class="search-highlight">AZAS</span> <span class="search-highlight">FAULT</span> <span class="search-highlight">ZONE</span> ( Eastern Tuva )
Image
Structural model of crustal failure at Sayan–Tuva–Ottug-Taiga–Azas fault junction. I: map of active faults and seismic fault scarps in Central Tuva; II: tentative structural model of compression duplex failure (Logachev, 1991); III: an evolution stage of a shear zone with progressive failure of irregularities and fault links (Ruzhich, 1997); IV: location map of faults with elements of slip geometry in northwestern Akademik Obruchev Range, Sayan–Tuva (1) and Ottug-Taiga–Azas (2) fault junction. 1, active Cenozoic faults: a, regional, b, local, c, presumably active; 2, fault scarps and their numbers; 3, fault numbers; 4, strike-slip faults; 5, thrusts. Faults: 1, Sayan–Tuva; 2, Ottug-Taiga–Azas; 3, Oka–Zhombolok; 4, Main Sayan. Fault scarps: 1, Aldy-Ishkin; 2, Uttug-Durug; 3, Upper Tura; 4, Taskyl; 5, Uzun-Khem; 6, Ustuku–Kara-Sug; 7, Kara-Khol; 8, At-Chol-Dug; 9, Kodura-Khol; 10, Oka I; 11, Oka II.

Structural model of crustal failure at Sayan–Tuva–Ottug-Taiga–Azas fault ju...

Published: 01 February 2010
Fig. 6. Structural model of crustal failure at Sayan–Tuva–Ottug-Taiga–Azas fault junction. I: map of active faults and seismic fault scarps in Central Tuva; II: tentative structural model of compression duplex failure ( Logachev, 1991 ); III: an evolution stage of a shear zone with progressive
Journal Article

The Late Pleistocene–Holocene climate history in the western Todzha basin ( Eastern Tuva )

S.G. Arzhannikov, S.V. Alekseev, A.V. Glyzin, N.V. Kulagina, N.V. Ignatova, L.A. Orlova
Published: 01 February 2010
Russ. Geol. Geophys. (2010) 51 (2): 163–175.
DOI: https://doi.org/10.1016/j.rgg.2009.12.017
...Fig. 6. Structural model of crustal failure at Sayan–Tuva–Ottug-Taiga–Azas fault junction. I: map of active faults and seismic fault scarps in Central Tuva; II: tentative structural model of compression duplex failure ( Logachev, 1991 ); III: an evolution stage of a shear zone with progressive...
FIGURES | View All (10)
View PDF for article title, The Late Pleistocene–Holocene climate history in the western Todzha basin ( Eastern Tuva )
Purchase
Add to Citation Manager for The Late Pleistocene–Holocene climate history in the western Todzha basin ( Eastern Tuva )
Journal Article

Recurrence of strong seismic events in the area of the 2011–2012 Tuva earthquakes according to paleoseismological data

A.N. Ovsyuchenko, Yu.V. Butanaev, A.V. Marakhanov, A.S. Lar’kov, S.S. Novikov, K.S. Kuzhuget
Published: 01 November 2017
Russ. Geol. Geophys. (2017) 58 (11): 1417–1425.
DOI: https://doi.org/10.1016/j.rgg.2017.11.006
... . Paleoseismodislocations in the Ottug–Taiga-Azas fault zone (eastern Tuva) . Geologiya i Geofizika (Russian Geology and Geophysics) 41 ( 11 ), 1501 – 1510 (1445–1453). Arzhannikov , S.G. , Zelenkov , P.Ya. , 1995 . Strong paleoearthquakes of the Academician...
FIGURES | View All (10)
View PDF for article title, Recurrence of strong seismic events in the area of the 2011–2012 Tuva earthquakes according to paleoseismological data
Purchase
Add to Citation Manager for Recurrence of strong seismic events in the area of the 2011–2012 Tuva earthquakes according to paleoseismological data
Image
Scheme of arrangement and internal structure of paleoseismic dislocations in the zone of the Ottug-Taiga–Azas fault. A – Uzun-Khem and Ustuku-Kara-Sug PSD; 1 – seismotectonic escarpment, 2 – detachment walls and landslide masses, 3 – watershed lines of ridges, 4 – parameters: h – height (m), L – length (km), 5 – western, central, and eastern parts of the structure, 6 – seismotectonic structures: I – Uzun-Khem, II – Ustuku-Kara-Sug. B – At-Chol-Dug PSD: 1 – seismotectonic escarpment, 2 – graben-shaped and wedge-like near-fault subsidences, 3 – PSD parameters: h – height (m), d – depth of subsidence (m), L – width of breakage valleys in escarpments (m), 4 – breakage valley in a seismotectonic escarpment and its number, 5 – isohypses laid at 40 m, 6 – extinct lakes, 7 – range of distribution of seismotectonic displacements of paleoearthquakes of different generations. C – Kara-Khol’ PSD: 1–5 – absolute hypsometry of blocks: 1 – 2500–2700 m, 2 – 2300–2500 m, 3 – 2000–2300 m, 4 – 1700–2000 m, 5 – 1400–1700 m, 6 – (I) – fault-block architecture of the region under study, (II) – detailed scheme of the Kara-Khol’ PSD; 7 – numbers of features of the Kara-Khol’ PSD; 8 – faults: a – regional Ottug-Taiga; b – local; 9 – detachment walls; 10–12 – landslide masses of: 10 – first generation, 11 – second generation, 12 – third generation; 13 – landslide blocks of first generation; 14 – isohypses laid at 100 m; 15 – epicentral regions of earthquakes of different generations. D – Kodura-Khol’ PSD: 1 – seismotectonic fracture, 2 – en-echelon system of fractures, 3 – en-echelon micrograbens, 4 – escarpment of 80 m high terrace, 5 – offset watershed nose of 80 m high terrace, 6 – isometric subsidences, occasionally filled with water, 7 – supposedly seismic deformations, 8 – PSD parameters: h – height (m), d – depth of subsidence (m), L – length (m), 9 – relief hypsometry, 10 – valley-like depression, 11 – en-echelon seismotectonic fractures expressed in escarpments.

Scheme of arrangement and internal structure of paleoseismic dislocations i...

Published: 01 November 2000
Fig. 2. Scheme of arrangement and internal structure of paleoseismic dislocations in the zone of the Ottug-Taiga–Azas fault. A – Uzun-Khem and Ustuku-Kara-Sug PSD; 1 – seismotectonic escarpment, 2 – detachment walls and landslide masses, 3 – watershed lines of ridges, 4 – parameters: h
Journal Article

LATE QUATERNARY GEODYNAMICS AND TECTONIC ACTIVITY WITHIN THE KAN FAULT SYSTEM ( southwestern Siberian Platform )

S.G. Arzhannikov, A.S. Gladkov, R.M. Semenov
Published: 01 April 2004
Russ. Geol. Geophys. (2004) 45 (4): 430–442.
.... MOIP. Otd. Geol. , 34 , 5 , 55 – 71 , 1959 . 17. Arzhannikov , S.G. , Paleoseismic dislocation in the Ottug-Taiga-Azas fault zone (Eastern Tuva) , Geologiya i Geofizika (Russian Geology and Geophysics) , 41 , 11 , 1501 – 1510 (1445...
FIGURES | View All (9)
View PDF for article title, LATE QUATERNARY GEODYNAMICS AND TECTONIC ACTIVITY WITHIN THE KAN <span class="search-highlight">FAULT</span> SYSTEM ( southwestern Siberian Platform )
Purchase
Add to Citation Manager for LATE QUATERNARY GEODYNAMICS AND TECTONIC ACTIVITY WITHIN THE KAN <span class="search-highlight">FAULT</span> SYSTEM ( southwestern Siberian Platform )
Journal Article

The Kyzyl–Tashtyg Ore Deposit of Eastern Tuva—A Standard for the Ancient Volcanogenic Formation of Pyrite-Polymetallic Ores

I.V. Gaskov
Published: 01 February 2020
Russ. Geol. Geophys. (2020) 61 (2): 139–154.
DOI: https://doi.org/10.15372/RGG2019075
... ). The Ulugoy zone extends up to ~150 km with a west-east strike, is 30–40 km wide and is bound from the south by the Kaakhem fault and from the north by the Taskyl and Azas faults. Its structure is that of a linear paleodepression filled with mainly bimodal volcanics (basalts, dacites, rhyolites...
FIGURES | View All (10)
View PDF for article title, The Kyzyl–Tashtyg Ore Deposit of Eastern Tuva—A Standard for the Ancient Volcanogenic Formation of Pyrite-Polymetallic Ores
Purchase
Add to Citation Manager for The Kyzyl–Tashtyg Ore Deposit of Eastern Tuva—A Standard for the Ancient Volcanogenic Formation of Pyrite-Polymetallic Ores