Caratterizzazione idrogeochimica delle acque sotterranee abruzzesi e relative anomalie

Caractérisation hydrogéochimique des eaux souterraines des Abruzzes et anomalies stratigraphiques relatives

Auteurs :
DESIDERIO, G.
RUSI, S.
TATANGELO, F.

Description :
The geological and stratigraphical sequence of the Abruzzo region (Central Italy) is dominated by the Jurassic to Oligocene succession, constituted mainly by limestone, marley limestones, calcareous sandstones, calcareous marls, marls and clayey marls along the Apennines, hilly areas and shoreline. The Miocene sequence, outcropping along the Apennines front, is constituted of limestones, marley limestones, calcareous marls and marls. The top of the succession, in the central and northern areas, is constituted by Messinian deposits of the marley-arenaceous turbidite formation, while, in the southern area delimited by Pescara river at north, by the evaporitic terrigeneous succession. The Pliocene-Pleistocene sequence represents the greater part of the hill domain, mainly constituted by marley clays and clayey marls surrounding arenaceous and conglomerate bodies. - (NF)


Type de document :
Article de périodique

Source :
Bollettino della Società geologica italiana, issn : 0037-8763, 2010, vol. 129, n°. 2, p. 207-222, nombre de pages : 16, Références bibliographiques : 26 ref.

Date :
2010

Editeur :
Pays édition : Italie, Roma, Società geologica italiana