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Gas hydrates—geological perspective and global change

Kvenvolden, Keith A.·1993·Reviews of Geophysics

Abstract

Natural gas hydrates occur worldwide in polar regions, normally associated with onshore and offshore permafrost, and in sediment of outer continental and insular margins. The total amount of methane in gas hydrates likely exceeds 10 19 g of methane carbon. Three aspects of gas hydrates are important: their fossil fuel resource potential, their role as a submarine geohazard, and their effects on global climate change. Because gas hydrates represent a large amount of methane within 2000 m of the Earth's surface, they are considered to be an unconventional, unproven source of fossil fuel. Because gas hydrates are metastable, changes of pressure and temperature affect their stability. Destabilized gas hydrates beneath the seafloor lead to geologic hazards such as submarine slumps and slides, examples of which are found worldwide. Destabilized gas hydrates may also affect climate through the release of methane, a “greenhouse” gas, which may enhance global warming and be a factor in global climate change.

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Metadata

Authors
Kvenvolden, K. A.
Venue
Reviews of Geophysics
Published
1993-05
Volume
31
Issue
2
Pages
173-187
ISSN
  • 0096-1043 (ISSN-L)
  • 8755-1209
  • 1944-9208
OpenAlex
W2122895208
Cited by
1,533
References
0
FWCI
15.96
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Gas hydrates—geological perspective and global change. https://app.cochat.ai/papers/10.1029/93rg00268
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Kvenvolden, K. A. (1993). Gas hydrates—geological perspective and global change. Reviews of Geophysics. https://doi.org/10.1029/93rg00268

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Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.