BASIC PRINCIPLES OF STRUCTURAL AND HYDROGEOLOGICAL MAPPING OF THE BAIKAL REGION
https://doi.org/10.5800/GT-2017-8-3-0296
Abstract
Structural and hydrogeological zonation of the Baikal region is based on allocation of hydrogeological structures within the large tectonic complexes differing in development history. It is a southeast part of the Siberian platform, the Sayan-Baikalian folded belt and the western part of the Transbaikal folded region. The Cenozoic activation of the region which has led to emergence of the Baikal rift and movements on a series of large fault zones in Transbaikalia has substantially influenced on formation of collecting properties of rocks.
About the Authors
M. A. Tugarina
Irkutsk National Research Technical University
Russian Federation
Irkutsk
Russian Federation
Irkutsk
K. Zh. Seminsky
Institute of the Earth’s Crust, Siberian Branch of RAS
Russian Federation
Irkutsk
Russian Federation
Irkutsk
References
1. Seminsky K.Zh., 2003. Internal Structure of Continental Fault Zones. Tectophysical Aspect. Siberian Branch of the Russian Academy of Science, Publishing House Branch “Geo”, Novosibirsk, 244 p.
2. Sherman S.I., Bornyakov S.A., Buddo V.Yu., 1983. Areas of Dynamic Influence of Faults (Results of Modeling). Nauka, Novosibirsk, 112 p.
3. Stepanov V.M., 1980. Hydrogeological Structures of Transbaikalia. Nedra, Moscow, 176 p.
4. Stepanov V.M., 1989. Introduction to Structural Hydrogeology. Nedra, Moscow, 229 p.
Review
For citations:
Tugarina M.A., Seminsky K.Zh. BASIC PRINCIPLES OF STRUCTURAL AND HYDROGEOLOGICAL MAPPING OF THE BAIKAL REGION. Geodynamics & Tectonophysics. 2017;8(3):577-579. https://doi.org/10.5800/GT-2017-8-3-0296
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