BASIC PRINCIPLES OF STRUCTURAL AND HYDROGEOLOGICAL MAPPING OF THE BAIKAL REGION

M. A. Tugarina; K. Zh. Seminsky

doi:10.5800/GT-2017-8-3-0296

BASIC PRINCIPLES OF STRUCTURAL AND HYDROGEOLOGICAL MAPPING OF THE BAIKAL REGION

M. A. Tugarina, K. Zh. Seminsky

https://doi.org/10.5800/GT-2017-8-3-0296

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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
Россия
Irkutsk

K. Zh. Seminsky

Institute of the Earth’s Crust, Siberian Branch of RAS
Россия
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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