Sluggish and steady focussed flows through fine-grained sediments: The methane-derived cylindrical concretions of the Tertiary Piedmont Basin (NW Italy)
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文摘

Cylindrical concretions developed around ancient fluid conduits.

They record steady, sluggish fluxes of methane-rich fluids through muddy sediments.

They result from microbially-induced dolomite precipitation.

They formed below the seafloor, between the SO4/CH4 and the oxic/anoxic interfaces.

They preserve only the highest part of fluid conduits.

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