gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0296gtcrust-437Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSBASIC PRINCIPLES OF STRUCTURAL AND HYDROGEOLOGICAL MAPPING OF THE BAIKAL REGIONBASIC PRINCIPLES OF STRUCTURAL AND HYDROGEOLOGICAL MAPPING OF THE BAIKAL REGIONTugarinaM. A.TugarinaM. A.

Irkutsk

Irkutsk

SeminskyK. Zh.SeminskyK. Zh.

Irkutsk

Irkutsk

Irkutsk National Research Technical UniversityРоссияIrkutsk National Research Technical UniversityRussian FederationInstitute of the Earth’s Crust, Siberian Branch of RASРоссияInstitute of the Earth’s Crust, Siberian Branch of RASRussian Federation20171410201783577579Copyright © Tugarina M.A., Seminsky K.Z., 20172017Tugarina M.A., Seminsky K.Z.Tugarina M.A., Seminsky K.Z.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/437

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.

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.

Russian Foundation for Basic ResearchReferencesSeminsky 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.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.Sherman S.I., Bornyakov S.A., Buddo V.Yu., 1983. Areas of Dynamic Influence of Faults (Results of Modeling). Nauka, Novosibirsk, 112 p.Sherman S.I., Bornyakov S.A., Buddo V.Yu., 1983. Areas of Dynamic Influence of Faults (Results of Modeling). Nauka, Novosibirsk, 112 p.Stepanov V.M., 1980. Hydrogeological Structures of Transbaikalia. Nedra, Moscow, 176 p.Stepanov V.M., 1980. Hydrogeological Structures of Transbaikalia. Nedra, Moscow, 176 p.Stepanov V.M., 1989. Introduction to Structural Hydrogeology. Nedra, Moscow, 229 p.Stepanov V.M., 1989. Introduction to Structural Hydrogeology. Nedra, Moscow, 229 p.

The authors declare that there are no conflicts of interest present.