Abstract
New data on the neotectonic processes, seismicity, and earth’s interior degassing in the southern part of the Zeya-Bureya artesian basin and their influence on the hydrogeological processes are considered. The helium-measuring and atmochemical methods that were used for defining zones of elevated permeability and channels of the fluid discharge revealed the discrete permeability of fractures and confinement of active “breathing” zones to intersections of faults that border high-order artesian basins and internal hydrogeological massifs. The confinement of discharge sites of different-type mineralized waters to definite structural-tectonic junctions of seismogenic zones is considered. Their description and trace-element composition are reported. The results of long-term helium measurements for understanding the dynamics of the earth’s interior degassing and the fluid regime in the Konstantinovka deposit of mineral chloride sodic waters are presented.
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.
