(1998) What does the ice-core record imply concerning the maximum climatic impact of possible gas hydrate release at Termination 1A?, in Gas Hydrates: Relevance to World Margin Stability and Climatic Change. Special Publication, 137. Geological Society of London. 319-326 doi:10.1144/gsl.sp.1998.137.01.25

| Reference Type | Report (article/chapter) | ||
|---|---|---|---|
| Title | What does the ice-core record imply concerning the maximum climatic impact of possible gas hydrate release at Termination 1A? | ||
| Report | Special Publication | ||
| Year | 1998 | Volume | 137 |
| Publisher | Geological Society of London | ||
| DOI | doi:10.1144/gsl.sp.1998.137.01.25Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 428587 | Long-form Identifier | mindat:1:5:428587:2 |
| GUID | 0 | ||
| Full Reference | (1998) What does the ice-core record imply concerning the maximum climatic impact of possible gas hydrate release at Termination 1A?, in Gas Hydrates: Relevance to World Margin Stability and Climatic Change. Special Publication, 137. Geological Society of London. 319-326 doi:10.1144/gsl.sp.1998.137.01.25 | ||
| Plain Text | (1998) What does the ice-core record imply concerning the maximum climatic impact of possible gas hydrate release at Termination 1A?, in Gas Hydrates: Relevance to World Margin Stability and Climatic Change. Special Publication, 137. Geological Society of London. 319-326 doi:10.1144/gsl.sp.1998.137.01.25 | ||
| In | (1998) Gas Hydrates: Relevance to World Margin Stability and Climatic Change. Special Publication Vol. 137. Geological Society of London | ||
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