The middle Miocene Mt. Ventasso-Mt Cimone arcuate structure of the Emilia Apennines.

Auteur :
VESCOVI, P.

Description :
In the sector NW of the Secchia Valley (Northern Apennines), SW-NE trending folds involve Epiligurian, Subligurian and Modino Units ; these are unconformably overlain by late Langhian Epiligurian deposits and seem to be bounded to the SE by displaced Triassic evaporites outcropping northeastward from the Cerreto Pass zone. An interpretation of the tectonic evolution which places both the NE-trending folds and the current position of the Triasic evaporites within a single setting, is proposed in this paper. - (NF)


Type de document :
Article de périodique

Source :
Bollettino della Società geologica italiana, issn : 0037-8763, 2005, vol. 124, n°. 1, p. 53-63, nombre de pages : 11, Références bibliographiques : 67 ref.

Date :
2005

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