Results 61 to 70 of about 296 (82)
Sea Floor of the Marine Protected Area of the Asinara Island (Sardinia, Italy) [PDF]
, 2022 De Luca, Mario +7 more
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The Atlas‑East Variscan ‑Elbe shear system and its role in the formation of the pull‑apart Late Palaeozoic basins [PDF]
, 2020 Federico, Mantovani +4 more
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Trace element constraints on the evolution and genesis of the Monte Pulchiana Leucogranites, northern Sardinia, Italy [PDF]
, 1999 Ghezzo, C., Poli, G., Tommasini, Simone
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Transtensional Tectonics Played a Key Role During the Variscan Cycle in the Sardinia-Corsica Massif [PDF]
, 2011 Minzoni, Nello
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Geochronological constraints on post-collisional shear belt in the Variscides of Sardinia, Italy [PDF]
, 2012 Carosi, Rodolfo +3 more
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Tectonophysics, 1991
Abstract The genesis of the Corsica-Sardinia batholith (CSB) can be explained in a continental collision setting. During the time of construction of the batholith, which is dated at about 70 Ma, three magmatic associations were emplaced: Mg-K calc-alkaline (U1), composite (mafic-silicic) calc-alkaline (U2) and post-collisional alkaline (U3).
Philippe Rossi, Alain Cocherie
openaire +3 more sources
Abstract The genesis of the Corsica-Sardinia batholith (CSB) can be explained in a continental collision setting. During the time of construction of the batholith, which is dated at about 70 Ma, three magmatic associations were emplaced: Mg-K calc-alkaline (U1), composite (mafic-silicic) calc-alkaline (U2) and post-collisional alkaline (U3).
Philippe Rossi, Alain Cocherie
openaire +3 more sources
Tectonophysics, 2012
The assembly of the Corsica-Sardinia Batholith (C-SB) coincides with final shaping of the Variscan belt and represents a key structure to unravel the feedbacks between partial melting, rheology and the evolution of collisional orogens. This paper presents a model for the genesis of the Arzachena pluton (AZN), one of the major calc-alkaline massifs of ...
L. Casini +4 more
openaire +6 more sources
The assembly of the Corsica-Sardinia Batholith (C-SB) coincides with final shaping of the Variscan belt and represents a key structure to unravel the feedbacks between partial melting, rheology and the evolution of collisional orogens. This paper presents a model for the genesis of the Arzachena pluton (AZN), one of the major calc-alkaline massifs of ...
L. Casini +4 more
openaire +6 more sources
Computers & Geosciences, 2012
Determination of the thermal state of the crust is of fundamental importance to understand the feedbacks between tectonics, rheology and metamorphism. The most important parameters controlling the variation of temperature with depth in the crust are the heat flow across the Moho, the thermal conductivity and the vertical distribution of heat-producing ...
leonardo casini
openaire +4 more sources
Determination of the thermal state of the crust is of fundamental importance to understand the feedbacks between tectonics, rheology and metamorphism. The most important parameters controlling the variation of temperature with depth in the crust are the heat flow across the Moho, the thermal conductivity and the vertical distribution of heat-producing ...
leonardo casini
openaire +4 more sources
2014
Sardinian granites are widely used as tiles, flooring, in columns, or within other architectural elements. The Rosa Beta granite is the most commonly traded variety of these granites and is used worldwide. The aim of this paper is to provide a thorough characterisation of the mineralogy, petrology, physical–mechanical properties and radiological ...
Cuccuru, S., Puccini, A.
openaire +1 more source
Sardinian granites are widely used as tiles, flooring, in columns, or within other architectural elements. The Rosa Beta granite is the most commonly traded variety of these granites and is used worldwide. The aim of this paper is to provide a thorough characterisation of the mineralogy, petrology, physical–mechanical properties and radiological ...
Cuccuru, S., Puccini, A.
openaire +1 more source