Seismic evidence of extensive microbial gas migration and trapping in submarine gas hydrates (Rakhine Basin, Bay of Bengal)
Submarine methane-rich gas hydrates in ocean sediments are a potential atmospheric greenhouse gas and energy source. It is considered that microbial methane is generally autochthonous, produced in situ within the gas hydrate stability zone with low gas flux and pressure, while thermogenic gas is all...
Κύριοι συγγραφείς: | Foschi, M, Etiope, G, Cartwright, JA |
---|---|
Μορφή: | Journal article |
Γλώσσα: | English |
Έκδοση: |
Elsevier
2023
|
Παρόμοια τεκμήρια
Παρόμοια τεκμήρια
-
Pliocene hyperpycnal flow and its sedimentary pattern in D block of Rakhine Basin in Bay of Bengal
ανά: Lihong ZHOU, κ.ά.
Έκδοση: (2020-04-01) -
Sedimentary and reservoir characteristics of Late Pliocene deep-water depositional units in Rakhine Basin in the Bay of Bengal
ανά: Jianan WU, κ.ά.
Έκδοση: (2024-11-01) -
Evidence for massive emission of methane from a deep‐water gas field during the Pliocene
ανά: Foschi, M, κ.ά.
Έκδοση: (2020) -
Submarine Slides and Their Influence on Gas Hydrate and Shallow Gas in the Pearl River Mouth Basin
ανά: Jiapeng Jin, κ.ά.
Έκδοση: (2025-02-01) -
Representation of gas hydrate fracture migration system by seismic
ανά: Ruiyou SONG, κ.ά.
Έκδοση: (2021-01-01)