Abstract
The hypothesis of subsurface subaquamarine runoff as a cause of formation of gas-hydrate accu- mulations on the continental slope and the shelf of continents and large islands is discussed. According to this hypothesis, large natural accumulations of hydrocarbons are a product of circulation of mobile carbon of the biosphere through land surface with the participation of waters of climatic cycle.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: 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.