Shallow gas hydrates off southwest Taiwan and their mechanisms

Yin Sheng Huang, Shu Kun Hsu, Chih Chieh Su, Andrew Tien Shun Lin, Pai Sen Yu, Nathalie Babonneau, Gueorgui Ratzov, Serge Lallemand, Pi Chuen Huang, Shiao Shan Lin, Jing Yi Lin, Kuo Yen Wei, Yuan Pin Chang, Neng Ti Yu, Ching Hui Tsai

研究成果: 雜誌貢獻期刊論文同行評審

5 引文 斯高帕斯(Scopus)

摘要

We have collected two shallow gas hydrate samples at two sites having different geological settings off southwest Taiwan during the cruise MD214 in 2018. The first core site, MD18-3542, is on the South Yuan-An East Ridge at ~ 1200 m water deep, where a structural unconformity covered by fine-silt sediments appears at ~ 5.5 m below the seafloor. The second core site, MD18-3543, is close to the Good-Weather Ridge at ~ 1100 m water deep, where a gas-related pockmark structure and authigenic carbonates are present at shallow strata with fine-silt sediments near the seafloor. Sediment properties of core MD18-3542 are distinctively different above and below the layer corresponding to the unconformity. Both cores show obvious gaps or voids in the lower core halves. The core features could be linked to the dissociated methane upward migrating from deep strata. Core site settings with upwelling methane would favor the formation of shallow gas hydrates. At site MD18-3542, the shallow hydrate could be formed due to high concentration methane kept beneath the unconformity covered by fine-silt sediments. At site MD18-3543, the shallow hydrate could be formed due to an extremely high flux of upwelling methane trapped either beneath the authigenic carbonates or fine-silt sediments.

原文???core.languages.en_GB???
文章編號7
期刊Marine Geophysical Research
42
發行號1
DOIs
出版狀態已出版 - 3月 2021

指紋

深入研究「Shallow gas hydrates off southwest Taiwan and their mechanisms」主題。共同形成了獨特的指紋。

引用此