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...
Những tác giả chính: | Foschi, M, Etiope, G, Cartwright, JA |
---|---|
Định dạng: | Journal article |
Ngôn ngữ: | English |
Được phát hành: |
Elsevier
2023
|
Những quyển sách tương tự
-
Sedimentary and reservoir characteristics of Late Pliocene deep-water depositional units in Rakhine Basin in the Bay of Bengal
Bằng: Jianan WU, et al.
Được phát hành: (2024-11-01) -
Evidence for massive emission of methane from a deep‐water gas field during the Pliocene
Bằng: Foschi, M, et al.
Được phát hành: (2020) -
Submarine Slides and Their Influence on Gas Hydrate and Shallow Gas in the Pearl River Mouth Basin
Bằng: Jiapeng Jin, et al.
Được phát hành: (2025-02-01) -
Representation of gas hydrate fracture migration system by seismic
Bằng: Ruiyou SONG, et al.
Được phát hành: (2021-01-01) -
Application of Reverse Time Migration to Faults Imaging in Rakhine Basin, Myanmar
Bằng: Seonghyung Jang, et al.
Được phát hành: (2022-01-01)