The Cainozoic calcalkaline magmatism of the western Mediterranean and its geodynamic significance

L. Beccaluva; M. Coltorti; B. Galassi; G. Macciotta; F. Siena

The Cainozoic calcalkaline magmatism of the western Mediterranean and its geodynamic significance

L. Beccaluva, M. Coltorti, B. Galassi, G. Macciotta, F. Siena

ARC Centre of Excellence for Core to Crust Fluid Systems (incorporation ARC National Key Centre for Geochemical evolution and Metallogeny of Continents (GEMOC))

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58 Citations (Scopus)

Abstract

Space-time distribution and petrogenetic affinity of the Cainozoic calcalkaline orogenic magmatism from the western Mediterranean (from Provence to Campania) has been reassessed, on the basis of new petrochemical and Sr-Nd isotopic data, for a better understanding of the geodynamic evolution of the area. The calcalkaline magmatism may be subdivided in two main cycles: the older, Oligo-Miocene in age (34-20 Ma in Province, and 32-13 Ma in Sardinia); and the younger, Pliocene-Quaternary in age (Eolian area <2 Ma, Campania ca. 2 Ma, and part of the Tyrrhenian oceanic crust 4-1.6 Ma). -from Authors

Original language	English
Pages (from-to)	293-308
Number of pages	16
Journal	Bollettino di Geofisica Teorica ed Applicata
Volume	36
Issue number	141-144
Publication status	Published - 1994

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title = "The Cainozoic calcalkaline magmatism of the western Mediterranean and its geodynamic significance",

abstract = "Space-time distribution and petrogenetic affinity of the Cainozoic calcalkaline orogenic magmatism from the western Mediterranean (from Provence to Campania) has been reassessed, on the basis of new petrochemical and Sr-Nd isotopic data, for a better understanding of the geodynamic evolution of the area. The calcalkaline magmatism may be subdivided in two main cycles: the older, Oligo-Miocene in age (34-20 Ma in Province, and 32-13 Ma in Sardinia); and the younger, Pliocene-Quaternary in age (Eolian area <2 Ma, Campania ca. 2 Ma, and part of the Tyrrhenian oceanic crust 4-1.6 Ma). -from Authors",

author = "L. Beccaluva and M. Coltorti and B. Galassi and G. Macciotta and F. Siena",

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T1 - The Cainozoic calcalkaline magmatism of the western Mediterranean and its geodynamic significance

AU - Beccaluva, L.

AU - Coltorti, M.

AU - Galassi, B.

AU - Macciotta, G.

AU - Siena, F.

PY - 1994

Y1 - 1994

N2 - Space-time distribution and petrogenetic affinity of the Cainozoic calcalkaline orogenic magmatism from the western Mediterranean (from Provence to Campania) has been reassessed, on the basis of new petrochemical and Sr-Nd isotopic data, for a better understanding of the geodynamic evolution of the area. The calcalkaline magmatism may be subdivided in two main cycles: the older, Oligo-Miocene in age (34-20 Ma in Province, and 32-13 Ma in Sardinia); and the younger, Pliocene-Quaternary in age (Eolian area <2 Ma, Campania ca. 2 Ma, and part of the Tyrrhenian oceanic crust 4-1.6 Ma). -from Authors

AB - Space-time distribution and petrogenetic affinity of the Cainozoic calcalkaline orogenic magmatism from the western Mediterranean (from Provence to Campania) has been reassessed, on the basis of new petrochemical and Sr-Nd isotopic data, for a better understanding of the geodynamic evolution of the area. The calcalkaline magmatism may be subdivided in two main cycles: the older, Oligo-Miocene in age (34-20 Ma in Province, and 32-13 Ma in Sardinia); and the younger, Pliocene-Quaternary in age (Eolian area <2 Ma, Campania ca. 2 Ma, and part of the Tyrrhenian oceanic crust 4-1.6 Ma). -from Authors

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AN - SCOPUS:0028683084

SN - 0006-6729

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JO - Bollettino di Geofisica Teorica ed Applicata

JF - Bollettino di Geofisica Teorica ed Applicata

IS - 141-144

ER -

The Cainozoic calcalkaline magmatism of the western Mediterranean and its geodynamic significance

Abstract

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