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- W2384570086 abstract "Gas hydrates as an important agent for climate change occur worldwide on the continental slopes and in permafrost regions.Based upon the study of the geology and geochemistry of the great geologic transitions,the dissociation of gas hydrates has been considered to probably result in global catastrophic events in the geological history.This idea is supported by global and relatively short-lived negative carbon isotope excursions,methane-derived carbon isotope values(especially δ13C-40‰) in carbonate sediments,carbonate dissolution,the biomarkers indicative of methane release,high accumulation rates of biogenic barite,an unusual suite of sedimentary structures and textures similar to those of cold seep carbonates,submarine sediment failures and crystal fans(e.g.aragonite).However,thehypothesisremains controversial and the proposed evidence has their limitations;therefore,we need further research." @default.
- W2384570086 created "2016-06-24" @default.
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- W2384570086 date "2010-01-01" @default.
- W2384570086 modified "2023-09-26" @default.
- W2384570086 title "Geological and Geochemical Evidence for Massive Dissociation of Gas Hydrate in the Geological History" @default.
- W2384570086 hasPublicationYear "2010" @default.
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