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Barguzin Fault

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Journal Article
Published: 01 July 2007
Russ. Geol. Geophys. (2007) 48 (7): 581–592.
...A.V. Chipizubov; S.G. Arzhannikov; R.M. Semenov; O.P. Smekalin Abstract We studied fault scarps produced by prehistoric earthquakes in the Barguzin fault zone and estimated the ages and the magnitudes of the scarp-forming events in each scarp segment from their structure, morphology, and scarp...
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<b>Fault</b> scarps produced by prehistoric earthquakes in <b>Barguzin</b> <b>fault</b> (souther...
Published: 01 July 2007
Fig. 1. Fault scarps produced by prehistoric earthquakes in Barguzin fault (southern flank of Shamanka segment). 1 — bedrock; 2 — alluvium and colluvium in alluvial fans and glacial talus; 3, 4 — glacial deposits of terminal moraines of Last Glacial (3) and older glaciations (4) ; 5 — Barguzin
Journal Article
Published: 01 July 2007
Russ. Geol. Geophys. (2007) 48 (7): 598–609.
...O.V. Lunina; A.S. Gladkov Abstract New structural and tectonophysical data, combined with the published geophysical and seismological evidence, were used to map the Late Cenozoic fault pattern and crustal stress in the Barguzin rift. Faults striking in the NE direction are the most abundant...
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Journal Article
Published: 01 July 2007
Russ. Geol. Geophys. (2007) 48 (7): 626–641.
... ) morphologically linked to Lake Baikal and surrounded by mountains ( Fig. 1 , A ). The basin northwestern edge has a fault border with the Barguzin Range, marked by the greatest fault offset. The mountains rise 2200 to 2600 m above sea level. The basin axis is assumed to be shifted notably toward the range foot...
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Journal Article
Published: 01 November 2013
Russ. Geol. Geophys. (2013) 54 (11): 1417–1426.
... in the central Baikal basin. One more transfer zone striking to the northeast, which is a connecting link between the South Baikal and Barguzin basins, is distinguished on the eastern side of the Baikal basin ( Fig. 1 ). The zone includes a series of normal faults bounding the Ust’-Barguzin basin...
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<b>Fault</b> pattern in <b>Barguzin</b> rift and its surroundings.  1 ,  2  — observed ( ...
Published: 01 July 2007
Fig. 2. Fault pattern in Barguzin rift and its surroundings. 1 , 2 — observed ( a ) and inferred ( b ) regional ( 1 ) and local ( 2 ) faults; 3 — normal ( a ) and strike-slip ( b ) faults; 4 — strike and dip of faults. Other symbols are as in Fig. 1 . A–C — rose diagrams of fault
Journal Article
Journal: GSA Bulletin
Published: 01 June 1997
GSA Bulletin (1997) 109 (6): 746–766.
...T. C. Moore, Jr.; K. D. Klitgord; A. J. Golmshtok; E. Weber Abstract Comparison of sedimentation patterns, basement subsidence, and faulting histories in the north and central basins of Lake Baikal aids in developing an interbasinal seismic stratigraphy that reveals the early synrift evolution...
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Maps of Pliocene–Quaternary <b>faults</b> in <b>Barguzin</b> rift basin and its flanking ...
Published: 01 April 2010
Fig. 2. Maps of Pliocene–Quaternary faults in Barguzin rift basin and its flanking mountains. 1–4 , fault activity rating according to cumulative score of indicators: 1 , low (1–5), 2 , medium (6–10), 3 , relatively high (11–20), 4 , and high (21–30); 5 , inferred faults; 6 , basins
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Density of <b>faults</b> in <b>Barguzin</b> rift and its surroundings. Map compiled using...
Published: 01 July 2007
Fig. 7. Density of faults in Barguzin rift and its surroundings. Map compiled using a round sliding window of 1% of surface area. White line contours large lakes and basins with Cenozoic fill.
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Location map of <b>Barguzin</b> basin ( A ):  1  — VES points,  2  — boreholes,  3...
Published: 01 July 2007
Location map of Barguzin basin ( A ): 1 — VES points, 2 — boreholes, 3 — MSE points; and VES profiles and stations ( B–D ), with elements of generalized geology. Symbols in A : 1 — VES stations, 2 — boreholes, 3 — MTS stations. Symbols in B–D : 1 — faults, 2 — boreholes, 3
Journal Article
Published: 01 April 2010
Russ. Geol. Geophys. (2010) 51 (4): 412–422.
...Fig. 2. Maps of Pliocene–Quaternary faults in Barguzin rift basin and its flanking mountains. 1–4 , fault activity rating according to cumulative score of indicators: 1 , low (1–5), 2 , medium (6–10), 3 , relatively high (11–20), 4 , and high (21–30); 5 , inferred faults; 6 , basins...
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Journal Article
Published: 01 January 2008
Journal of the Geological Society (2008) 165 (1): 235–246.
... ages of 507 ± 8 and 498 ± 7 Ma, and magmatic zircons from syntectonic syenite yielded an age of 495 ± 6 Ma. The main metamorphic event occurred at about 500 Ma, and was probably related to collision of the Barguzin microcontinent with the Siberian craton. Ages from 535 to 2750 Ma for detrital zircon...
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Journal Article
Published: 01 January 2007
Russ. Geol. Geophys. (2007) 48 (1): 120–140.
... (283.7±5.3 Ma), and quartz monzonites of the Romanovka massif (278.5±2.4 Ma). The U-Pb and Rb-Sr dates show that the Late Paleozoic magmatism in western Transbaikalia proceeded in two stages: (1) 340–320 Ma, when predominantly mesocratic granites of the Barguzin complex, including autochthonous ones...
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Journal Article
Published: 01 May 2016
Russ. Geol. Geophys. (2016) 57 (5): 790–808.
... of the activity of a low-energy mantle plume with the final stage of the Hercynian orogeny in space and time. At the early stage of magmatism, during the formation of the Barguzin granites, the plume had only a thermal influence on the crustal rocks heated as a result of Hercynian fold–thrust deformations...
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Journal Article
Published: 01 August 2020
Russ. Geol. Geophys. (2020) 61 (8): 858–873.
... of continental salinization, the Barguzin and Gusinoe Ozero–Orongoi depressions. The average mineralization of the lakes reaches 30.8 g/L, pH = 7.90–8.84, the fractional content of sulfate ion is 55.2–81.8% eq, and the fractional content of sodium ion is 59.1–82.1% eq. The paper presents the major-ion and trace...
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Journal Article
Published: 01 January 2007
Russ. Geol. Geophys. (2007) 48 (1): 71–82.
... folded and cut by transverse and lengthwise strike-slip faults of Middle Paleozoic and Mesozoic age. With late deformations taken into account, they can be regarded as a single belt of more than 6000 km long. Supposedly, the Kokchetav, Altai-Mongolian, Tuva-Mongolian, Barguzin and other microcontinents...
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Journal Article
Published: 01 September 2012
Russ. Geol. Geophys. (2012) 53 (9): 936–954.
... to the India–Eurasia collision, and the first rifting pulse originally had other causes. This inference agrees with fission-track apatite thermochronology indicating Cretaceous ages of samples from the Barguzin rift basin in the northeastern flank of the rift system. Rifting developed successively in three...
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Journal Article
Published: 01 May 2010
Russ. Geol. Geophys. (2010) 51 (5): 461–481.
... sediments are metamorphosed to low grades, folded in low-angle folds, densely faulted, and intruded with 288 ±2 Ma granitoids ( Ruzhentsev et al., 2007 ). The Uakit basin in the eastern Barguzin turbidite terrane is filled with Middle–Late Paleozoic terrigenous-carbonate rocks derived from...
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Journal Article
Published: 01 May 2010
Russ. Geol. Geophys. (2010) 51 (5): 447–460.
... active continental margin rocks (island arc–backarc basin system). The backarc basin history possibly began at 840–800 Ma, according to SHRIMP-II U-Pb zircon ages of the Orso gneiss. Many tectonic units in the Olkhon terrane belonged to the active margin of the Barguzin microcontinent which rifted off...
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<b>Fault</b> scarps produced by prehistoric earthquakes in northern Sarankhur segm...
Published: 01 July 2007
Fig. 3. Fault scarps produced by prehistoric earthquakes in northern Sarankhur segment of Barguzin fault. Symbols as in Fig. 1 .