Image1_Microbial Methane Generation and Implications for Stability of Shallow Sediments on the Upper Slope, U.S. Atlantic Margin.JPEG
Dissociation of methane hydrates in shallow marine sediments due to increasing global temperatures can lead to the venting of methane gas or seafloor destabilization. Along the U.S. Atlantic margin there is a well-documented history of slope failure and numerous gas seeps have been recorded. However...
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Format: | Still Image |
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2022
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Online Access: | https://doi.org/10.3389/feart.2022.835685.s001 https://figshare.com/articles/figure/Image1_Microbial_Methane_Generation_and_Implications_for_Stability_of_Shallow_Sediments_on_the_Upper_Slope_U_S_Atlantic_Margin_JPEG/19730689 |