The anoxic facies of the Lower Toarcian of Central Italy have been studied in order to define they depositional environment and they potentiality as source rock.

The Early Toarcian anoxic event and shale gas potential: the case history of the Marne del Monte Serrone Formation (Central Italy)

CIRILLI, Simonetta;
2012

Abstract

The anoxic facies of the Lower Toarcian of Central Italy have been studied in order to define they depositional environment and they potentiality as source rock.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11391/1224424
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