Add to ORKGIrace Andrea, Clari Pier Angelo, Dela Pierre Francesco, Bicchi Erica, Cavagna Simona, Festa Andrea. The Moncucco quarry : a key area to understand the Messinian evolution of the Torino Hill, tertiary Piemonte Basin, NW-Italy. In: Documents des Laboratoires de Géologie, Lyon, n°156, 2002. STRATI 2002. 3ème congrès français de stratigraphie. Lyon, 8-10 juillet 2002. pp. 131-132
In the NE Simbruini Mountains, the “Brecce della Renga Fm.” is a clastic unit documenting sedimentat...
The upper Messinian succession of the coastal area of Northern Marche can be subdivided into two lit...
The Montello hill is an uplifting anticline structure located in the front of the Neogene- Quaternar...
Cavagna Simona, Clari Pier Angelo, Dela Pierre Francesco, Irace Andrea, Festa Andrea. Petrographical...
An ash layer, about 1 cm thick, has been found during a reinvestigation of the upper Messinian-Zancl...
Along the Ligurian coast (NW Italy), Alpine-folded and slightly metamorphosed rocks experienced fluv...
<p>The study area is located in the Alpi Apuane (Tuscany, Italy), and extends between N 44°0′49.883″...
The Barga Basin, located between the Apuane Alps and the Northern Apennines, was the site of a fines...
In the Tertiary Basin of Piedmont (Northern Italy) an important Messinian sedimentary succession cro...
Abstract. – Integrated biostratigraphic and palaeoenvironmental analyses of foraminiferal, ostracod ...
The Central portion of the Periadriatic Basin is a N-S oriented foreland basin system associated to ...
The metamorphic evolution of metapelites from the eastern part of the Monte Rosa nappe and the Camug...
The early Messinian Laga Formation represents a turbidite complex deposited in the Late Neogene fore...
This paper and the associated 1:50,000 geological map are devoted to describe the geological feature...
L\u2019evoluzione tettonica del Monferrato \ue8 ben conosciuta a partire dagli episodi deformativi o...
In the NE Simbruini Mountains, the “Brecce della Renga Fm.” is a clastic unit documenting sedimentat...
The upper Messinian succession of the coastal area of Northern Marche can be subdivided into two lit...
The Montello hill is an uplifting anticline structure located in the front of the Neogene- Quaternar...
Cavagna Simona, Clari Pier Angelo, Dela Pierre Francesco, Irace Andrea, Festa Andrea. Petrographical...
An ash layer, about 1 cm thick, has been found during a reinvestigation of the upper Messinian-Zancl...
Along the Ligurian coast (NW Italy), Alpine-folded and slightly metamorphosed rocks experienced fluv...
<p>The study area is located in the Alpi Apuane (Tuscany, Italy), and extends between N 44°0′49.883″...
The Barga Basin, located between the Apuane Alps and the Northern Apennines, was the site of a fines...
In the Tertiary Basin of Piedmont (Northern Italy) an important Messinian sedimentary succession cro...
Abstract. – Integrated biostratigraphic and palaeoenvironmental analyses of foraminiferal, ostracod ...
The Central portion of the Periadriatic Basin is a N-S oriented foreland basin system associated to ...
The metamorphic evolution of metapelites from the eastern part of the Monte Rosa nappe and the Camug...
The early Messinian Laga Formation represents a turbidite complex deposited in the Late Neogene fore...
This paper and the associated 1:50,000 geological map are devoted to describe the geological feature...
L\u2019evoluzione tettonica del Monferrato \ue8 ben conosciuta a partire dagli episodi deformativi o...
In the NE Simbruini Mountains, the “Brecce della Renga Fm.” is a clastic unit documenting sedimentat...
The upper Messinian succession of the coastal area of Northern Marche can be subdivided into two lit...
The Montello hill is an uplifting anticline structure located in the front of the Neogene- Quaternar...