Results 131 to 140 of about 240 (174)

Tectonic evolution of the southwestern wall of the Baikal Rift Zone

Doklady Earth Sciences, 2006
Marc De Batist, A P Fedotov, De Batist M   +2 more
exaly   +2 more sources

Cenozoic lithogenesis in the Baikal rift zone

Lithology and Mineral Resources, 2016
New data on the geological history and Cenozoic lithogenesis in depressions of the Baikal rift zone are considered with areas adjacent to Lake Baikal as example. In this region, rifting developed during the plain (Late Oligocene‒Early Pliocene) and orogenic (Late Pliocene‒Holocene) stages and was accompanied by the accumulation of plain coaliferous fan
Yu. G. Tsekhovskii, O. V. Yapaskurt
openaire   +1 more source

The “seismic quiescence” effect in the Baikal Rift Zone

Journal of Volcanology and Seismology, 2008
This paper presents the results from long-term observations of parameters of the Earth’s natural impulsive electromagnetic field (ENIEMF) in the VLF range recorded in the Baikal Rift Zone. We consider the “seismic quiescence” effect and examine possible factors responsible for changes in the daily variations of the magnetic component before earthquakes.
I. B. Naguslaeva, Yu. B. Bashkuev, Yu. P. Malyshkov, D. G. Buyanova   +3 more
openaire   +1 more source

Volcanism of the Baikal rift zone

Tectonophysics, 1987
Abstract The volcanism of the Baikal rift zone is a specific case of intraplate volcanism where the tensional stress field in the lithosphere under the rift zone does not greatly exceed local tension in other volcanic regions of Central Asia in which rifting was not morphologically expressed.
openaire   +1 more source

Seismotectonics of the Baikal rift zone

Tectonophysics, 1978
Abstract High seismicity in the Baikal rift zone is controlled by the development of conjugate rising and subsiding block structures. Many types of seismological phenomena resulting from large earthquakes are manifested in the rift zone and include seismotectonic (regional, zonal and local), gravity-seismotectonic and seismogravitational deformations.
openaire   +1 more source

Faults of the Baikal rift zone

Tectonophysics, 1978
Abstract Baikal rift-zone faults range in magnitude from major through regional to local. The major, transcrustal faults of pre-Cenozoic initiation frame the structural pattern of the rift zone. Rifting causes a rejuvenation of all important faults regardless of their original type, many becoming oblique-slip faults.
openaire   +1 more source

Exploration of magnetic anomalies of the Baikal rift zone

Geomagnetism and Aeronomy, 2011
The paper presents the results of an experimental study of natural magnetic field anomalies in the Baikal rift zone.
R. A. Rakhmatulin, S. Yu. Khomutov, Yu. V. Lipko, V. V. Kharchenko   +3 more
openaire   +1 more source

The kinematics of the Baikal rift zone accommodation structures

Moscow University Geology Bulletin, 2017
Rift systems are composed of a set of heterogeneous tectonic blocks that deform under regional extension concordantly, but individually. Such coordination is achieved due to development of evolving ensembles of deformation structures along the borders of the blocks; these structures accommodate in some way the discrepancies in the structural style ...
A. V. Tevelev, V. S. Fedorovsky
openaire   +1 more source

Problems of the seismicity of the Baikal rift zone

Journal of Geodynamics, 1990
Abstract The results of investigations of the seismicity of the Baikal rift zone are considered on the basis of an instrumental survey of small shocks, macroseismic information on strong earthquakes of the past, and data on paleoseismic dislocations obtained from seismo-geological observations.
openaire   +1 more source

SEISMOHYDROGEOLOGICAL FEATURES OF THE BAIKAL RIFT ZONE

Russian Geology and Geophysics, 1992
A correlation between distribution of hydrotherms and seismic character of different regions of BRZ is considered. The conclusion is made that the deep-circulation waters, a peculiar “grease”, can provoke a gradual discharge of stresses accumulated in the Earth’s ernst to promote earthquake swarms, i.e., to activize seismic environment.
openaire   +1 more source