IGB

Connexion

(Article of periodic en Anglais - 2005)

Document title

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

Authors(s) and Affiliation(s)

VESCOVI P. ;

Abstract

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)

Source

Article of periodic

published at : Bollettino della Società geologica italiana / ISSN 0037-8763 / CODEN BOGIAT

Editor : Società geologica italiana, Roma - ITALIE (1882- 2008)

Millesime : 2005, vol. 124, no1 [pp. 53-63]

Bibliographic references : 67 ref.

Language

Anglais

INIST-CNRS, Cote INIST : 5205

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2006.
Refdoc record number (ud4) : 18261957 : Permanent link - XML version
Powered by Pxxo