The Cenozoic CH4-derived carbonates of Monferrato (NW Italy): A solid evidence of fluid circulation in the sedimentary column

Marine Geology

Volumn 265, Issue 3-4, 2009, Pages 167-184

  Clari, P ^a   Dela Pierre, F ^a,b   Martire, L ^a   Cavagna, S ^a  

^a UNIVERSITY OF TURIN   (Italy)

^b CNR   (Italy)

Author keywords

Cenozoic; CH4 derived carbonates; fluid circulation; gas hydrates; mud diapirism; NW Italy

Indexed keywords

CENOZOIC; CH4-DERIVED CARBONATES; FLUID CIRCULATION; MUD DIAPIRISM; NW ITALY;

BEARINGS (STRUCTURAL); CARBONATES; CARBONATION; CEMENTING (SHAFTS); CEMENTS; DEGASSING; FLOW OF FLUIDS; FLUIDS; GAS HYDRATES; HYDRATION; LITHOLOGY; METHANE; ROCKS; SEDIMENTOLOGY; STRATIGRAPHY; VOLCANOES;

LEAKAGE (FLUID);

BIVALVE; BRECCIA; CARBONATE; CENOZOIC; DIKE; GAS HYDRATE; LIMESTONE; LITHOSTRATIGRAPHY; MELANGE; METHANE; MUD VOLCANO; PALEONTOLOGY; SEAFLOOR; SEEPAGE; VEIN (GEOLOGY);

EURASIA; EUROPE; ITALY; MONFERRATO; PIEDMONT [ITALY]; SOUTHERN EUROPE;

BIVALVIA; LUCINA;

EID: 69249220065     PISSN: 00253227     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.margeo.2009.07.007     Document Type: Article

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