... (ID-1) occur on the borders of the Teletsk, Kamga, and Koldor grabens, which is represented by the ID-1 maximum in the low elevation domain ( Fig. 4 , A – D ). The surface topography in the region of Lake Teletskoe, typical of a young mountainous terrain, is made up of steep slopes alternating...

... of Vendian-Early Cambrian ophiolites and silicic terrigenous rocks, Late Riphean lavas and sediments, and Early-Middle Cambrian volcanics, tuffa, terrigenous sediments, and carbonates. The Teletsk block in the western side of Lake Teletskoye is composed of Devonian granites (Altyntaus complex) and Late...

... by the formation of the Charysh-Terekta system of right-lateral transforms, followed by left-lateral strike-slip faulting in the Kurai and Kuznetsk-Teletsk-Bashkaus zones. The Siberia/Kazakhstan collision involved left-lateral motion along the Char ophiolite belt and the Irtysh-Kurchum and North East shear zones...

... dashed line shows the study area. ES – East Sayan, GA – Gorny Altai, GSh – Gornaya Shoriya, WS – West Sayan, KA – Kuznetsk Alatau, MA – Mongol-Altai zone, LZ – Lake zone, TV – Tuva. Asterisks show the position of the Abakan massif (1) and migmatites in the Teletsk-Chulyshman block (2). Fig. 5...

... in the Ordovician and a late collisional stage of andalusite-cordierite metamorphism in the Late Silurian–Devonian (about 60 Myr long). The Bashkaus, Chulyshman, Upper Bashkaus, Teletsk–Abakan, and Shapshal andalusite-cordierite schists formed mainly during the late event. These complexes show more evident spatial...

... orogen lying orthogonally to the general strike of Great Altai. On other sides of Great Altai there are relatively stable blocks existing as plainland areas: the West Siberian Plain in the north, the Zaisan and Jonggar basins in the southwest, and the Uvs Nuur basin and the Great Lake Depression...

.... , The Teletskoye Lake young graben , Priroda , 2 , 56 – 64 , 1991 . 2. Buslov , M.M. , and M. Sintubin , Structural evolution of the Teletsk zone, Altai-Sayan Folded Area , Geologiya i Geofizika (Russian Geology and Geophysics) , 36 , 10 , 91 – 98 (81...

... mineralization (the Kaurchak deposit on the left side of Lake Teletskoe in the Teletsk zone) was associated with Middle Cambrian–Early Ordovician accretion and collision . No considerable mineralization has been revealed in the Ordovician–Silurian passive margin setting. The Permian–Triassic event also...

...: Teletsk, Charysh-Terekta, and others, which formed as a result of the collision of the Altai-Mongolian terrane and the Siberian continent. The ratios of regional strike-slip deformations of different ages and orientation are clearly seen in northwestern Gorny Altai ( Fig. 2 ). The basalts have...

... elevated mountains, 2 — moderately and low-elevated mountains; 3 — platform plains composed of Meso-Cenozoic deposits and intermontane depressions with Cenozoic fill; 4 — modern lakes; 5 — territory within which Paleozoic and Cenozoic structural frameworks were compared; 6 — national frontiers...

...: denudatlonal part (Skh1), denudatlonal-accumulatlve part (Skh2), Tarkhatln: denudatlonal part (Tkh1), denudatlonal-accumulatlve part (Tkh2), Bertek (Bt). 9 – 14 — symbols at the block diagreams: 9 — Paleozolc rocks: weakly lithified and loose Cenozoic rocks: 10 — lake-proluvium sediments, experienced...

.... Piper and Paul Karl Link 1217 Massive recrystallization of low-Mg calcite at high temperatures in hydrocarbon source rocks: Implications for organic acids as factors in diagenesis— Ezat Heydari and William J. Wade 1285 Role of sediment composition in trace metal distribution in lake...

... of depressions, undifferentiated ( b ). Altai mobile belt: GrA — Gorny (Russian) Altai, SA — Southern Altai, MA — Mongolian Altai, GA — Gobi Altai; WSn — West Sayan mobile belt; depressions within framing microplates: Zs — Zaisan, Jn — Junggarian (Junggarian microplate), GLB — Great Lakes Basin (Tuvino-Mongolian...

... in the southwest, and the Uvs Nuur basin and the Great Lake Depression in the east ( Fig. 1 ). Fig. 1. Location map of study area in mountain framework of Central Asia. Abbreviations stand for names of mountains and basins: GA — Gorny Altai, MA — Mongolian Altai, H — Hangayn, WS — West Sayan, ES — East...

... ). The basins and ranges typically have rhombic contours, and some consist of smaller rhombic structures. The gravity contrasts are the highest in the Tien Shan and its surroundings (from –300 to +300 mGal) and as high as –250 to +200 mGal around Lake Baikal ( Fig. 1 ). Outside the Cenozoic basins and ranges...

... included in the latter ( Kuznetsov, 1963 ). In the southwest, it is bounded by the Kurai–Teletsk deep fault, whose eastern part breaks into a series of feathering faults. The upper structural level of the East-Altai structural zone is formed by basins composed of terrigenous sedimentary rocks...

... of intrusions: A — plutons intruding unmetamorphosed rocks (Mongolia, east of Lake Dayan-Nuur); B — coarse porphyry granites transient into cataclastic granite and granite gneiss lenses with scalloped boundaries (Mongolia, inner part of Hovd pluton); C — granite gneiss strips and lenses or lenses...

... in the region of earthquake nucleation does increase and can be instrumentally measured. The M s = 6.2 earthquake of 4 November 1986 near Lake Teletskoye was felt at intensities VII in the epicenter, V in the Tashtagol region (∆ = 214 km), and III near Novosibirsk (∆ = 610 km). Altogether Table 3...

... at altitudes from 1000 to 2000 m. The major neotectonic structures are controlled by the Irtysh, Charysh-Terekta, and Kurai fault zones and by the North Sayan, Kurai-Teletsk, Shapshal, and other faults subject to repeated reactivation [ 3 , 6 ]. The geometry of faults and focal mechanisms of earthquakes...