Abstract
In this study we deal with the results of five-year routine observations of physico-chemical parameters and bulk composition of the local hydrothermal “native sulfur melt - gas-water-rock” system which was created at the bottom of the Bannoe thermal lake in the Uzon caldera after a small phreatic explosion of July 7, 1989.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have