Tectonic control on laccolith emplacement in the northern Apennines fold-thrust belt: the Gavorrano intrusion (southern Tuscany, Italy)

2004 ◽  
Vol 234 (1) ◽  
pp. 151-161 ◽  
Author(s):  
Francesco Mazzarini ◽  
Giacomo Corti ◽  
Giovanni Musumeci ◽  
Fabrizio Innocenti
1997 ◽  
Vol 40 (3) ◽  
Author(s):  
A. Argnani ◽  
F. Frugoni

Seismic profiles in the Central Adriatic show the presence of a WNW-ESE trending belt (Central Adriatic Deformation Belt, CADB) where broad folds of Quaternary age occur. Seismicity in the Adriatic foreland seems to be localised along the CADB which is interpreted as the result of foreland deformation linked to the Apennine fold-and-thrust belt and possibly due to the presence of an inherited structural discontinuity. Geological arguments indicate that the CADB lineament can continue underneath the Northern Apennines and might have affected its recent evolution, characterised by the rise of a linear orographic front.


Geomorphology ◽  
2016 ◽  
Vol 253 ◽  
pp. 425-437 ◽  
Author(s):  
Mirko Carlini ◽  
Alessandro Chelli ◽  
Paolo Vescovi ◽  
Andrea Artoni ◽  
Luca Clemenzi ◽  
...  

1990 ◽  
Vol 77 (1) ◽  
pp. 3-14 ◽  
Author(s):  
M. Boccaletti ◽  
F. Calamita ◽  
G. Deiana ◽  
R. Gelati ◽  
F. Massari ◽  
...  

Tectonics ◽  
1999 ◽  
Vol 18 (3) ◽  
pp. 559-574 ◽  
Author(s):  
Mike P. Coward ◽  
Mauro De Donatis ◽  
Stefano Mazzoli ◽  
Werter Paltrinieri ◽  
Forese-Carlo Wezel

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