U-Th stratigraphy of a cold seep carbonate crust
On continental margins, oxidation of methane-rich fluids from the sediment often leads to formation of authigenic carbonate pavements on the seafloor. The biogeochemical processes involved during this carbonate precipitation are increasingly understood, but little is known about the duration or mode...
| Main Authors: | , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2009
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