The possible impact of gas-bearing fluids on sediment in the arch Fedynskogo (Barents sea)

Abstract

A comparative analysis of facies and composition of precipitation on the bottom areas where the discharge of methane fluid occurs rapidly or not registered. Effect of gaseous fluids on postsedimentary transformation of clay minerals not found. Possible local manifestation of the fluid can be lithogenesis authigenic carbonate formation.

Keywords

• подводная мерзлота
• метаноносные флюиды
• флюидный литогенез