Hydrogeochemistry of northern part of kolyvan-tomsk folded zone (South-east of Western Siberia, Russia)

Yuliya V. Kolubaeva, Yulia Grigorievna Kopylova, Stepan L. Shvartsev

Research output: Chapter in Book/Report/Conference proceedingConference contribution

1 Citation (Scopus)

Abstract

The paper is devoted to the study of the geochemistry of natural waters of active water exchange zone in moderately moist climate province using the example of the northern part of the Kolyvan-Tomsk folded zone (Russia, south-east of Western Siberia). It is shown that there is most often founded fresh, neutral and slightly alkaline water of calcium bicarbonate type. It is shown that the chemical composition of groundwater is formed in three stages (atmogenic, biogenic and lithogenic), undergoing at the same time to significant changes from one stage to another.

Original languageEnglish
Title of host publicationInternational Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM
PublisherInternational Multidisciplinary Scientific Geoconference
Pages347-354
Number of pages8
Volume1
Edition3
Publication statusPublished - 2015
Event15th International Multidisciplinary Scientific Geoconference and EXPO, SGEM 2015 - Albena, Bulgaria
Duration: 18 Jun 201524 Jun 2015

Other

Other15th International Multidisciplinary Scientific Geoconference and EXPO, SGEM 2015
CountryBulgaria
CityAlbena
Period18.6.1524.6.15

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Keywords

  • Chemical composition
  • Groundwater
  • Kolyvan-Tomsk folded zone
  • Mineralization

ASJC Scopus subject areas

  • Geology
  • Geotechnical Engineering and Engineering Geology

Cite this

Kolubaeva, Y. V., Kopylova, Y. G., & Shvartsev, S. L. (2015). Hydrogeochemistry of northern part of kolyvan-tomsk folded zone (South-east of Western Siberia, Russia). In International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM (3 ed., Vol. 1, pp. 347-354). International Multidisciplinary Scientific Geoconference.