Results 181 to 190 of about 21,284 (228)
Some of the next articles are maybe not open access.
Flysch Formations of the Northern Apennines
1964Summary At least a dozen distinct types of flysch occur in the northern Apennines. Two differential processes — resedimentation and tectonic sliding — are invoked to account for their distribution in space and time, and to trace some genetic connections.
openaire +1 more source
Chrysotile within calcite veins from Northern Apennines
2014In the Northern Apennines several olistoliths made up of serpentinites, calpionelle limestones and ophiolitic breccias have been recognized within the Porcellara Complex, Monte Cassio Unit. These olistoliths are frequently crossed by a dense network of centimeter to decimeter veins generally filled by carbonate minerals (e.g.
Giordani, Matteo +2 more
openaire +2 more sources
Thermal evolution of the Northern Apennines
1998This paper uses numerical 2D simulations in studyng subsurface temperatures and heat flow density along a 200 km long transect in the Italian Northern Apennines from Piombino to Ancona.
FEDERICO, Costanzo, PAUSELLI, Cristina
openaire +1 more source
Structure of the Northern Apennines
Nature, 1961EDWARD BAILEY, W. J. McCALLIEN
openaire +1 more source
Landscape dynamics risk management in Northern Apennines
2002The Riomaggiore catchment is a sub-watershed of the Reno river basin, located in the Northern Apennines between Florence and Bologna. The whole area shows complex interactions between the environment and human activities: hillslope processes, mainly soil erosion and landsliding, are very widespread and overlap in many cases with settlements and ...
Bianchi F., CATANI, FILIPPO
openaire +1 more source
Thermal-topographic modeling of the Northern Apennines
2004Geomorphology can have a strong influence on thermochronometer. In particular, the closure isotherm will tend to form a smoothed version of the surface topography, with greater topographic relief producing larger deflections of the isotherm. Also, erosion rate will influence the mean closure depth given that the faster erosion causes isotherms to ...
ZATTIN, MASSIMILIANO +4 more
openaire +1 more source
The northern Apennine, Italy: Geological structure and traspressive evolution.
2004At the boundary between the European and Adria plates, the Northern Apennine represents a polyorogenic belt, resulted from the Oligocene-Pliocene eastward progressive overthrusting of the Ligurides on the detached sedimentary cover of the Adria plate continental margin (Foredeep Units).
Cerrina Feroni A, Ottria G, Ellero A
openaire +3 more sources