Abstract
Comparative hydrogeochemical studies of groundwater in the Ulaanbaatar reservoir and those in the coast of Lake Baikal show significant difference between hydrogeodynamic processes of these areas, the earlier generation of U-isotopic and Si–Na–Li-temperature anomalies in the Ulaanbaatar groundwater reservoir and the later in those of the Baikal coast.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
