Abstract
Hydrous pyrolysis of an immature (Ro ¡Ö 0.25%) sulphur-rich marl from the Gessoso-solfifera Formation (Messinian) in the Vena del Gesso Basin was carried out at 160¡ãC ¡Ü T ¡Ü330¡ãC for 72 h, to study the effect of progressive diagenesis and early catagenesis on the abundance and distribution of sulphur-containing and
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