Аннотация
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.
| Язык оригинала | Английский |
|---|---|
| Название основной публикации | International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM |
| Издатель | International Multidisciplinary Scientific Geoconference |
| Страницы | 347-354 |
| Число страниц | 8 |
| Том | 1 |
| Издание | 3 |
| Состояние | Опубликовано - 2015 |
| Событие | 15th International Multidisciplinary Scientific Geoconference and EXPO, SGEM 2015 - Albena, Болгария Продолжительность: 18 июн 2015 → 24 июн 2015 |
Другое
| Другое | 15th International Multidisciplinary Scientific Geoconference and EXPO, SGEM 2015 |
|---|---|
| Страна | Болгария |
| Город | Albena |
| Период | 18.6.15 → 24.6.15 |
ASJC Scopus subject areas
- Geology
- Geotechnical Engineering and Engineering Geology
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Цитировать
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). В International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM (3 ред., Том 1, стр. 347-354). International Multidisciplinary Scientific Geoconference.