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

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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.

About the authors

N P Chamov

Geological Institute of RAS

Email: nchamov@yandex.ru
The laboratory of comparative analysis of sedimentary basins

V V Kostyleva

Geological Institute of RAS

Email: kovikto@yandex.ru
The laboratory of comparative analysis of sedimentary basins

S Yu Sokolov

Geological Institute of RAS

Email: sysokolov@yandex.ru
The laboratory of comparative analysis of sedimentary basins

A E Kotelnikov

eoples’ Friendship University of Russia

Email: aekot@rambler.ru
Department of Mineral Deposits Engineering faculty

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Copyright (c) 2015 Чамов Н.П., Костылева В.В., Соколов С.Ю., Котельников А.Е.

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This work is licensed under a Creative Commons Attribution 4.0 International License.

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