The calc-alkaline Monte Capo Stella dykes in the Ophiolitic Unit of the Elba Island (Italy): Geological setting and compositional characterization

Autor: Pandeli E.[1, Santo A.P.]1, Candido M.R.[1], Petrone C.M.[2], Giusti R.[1]

Publikováno v: Ofioliti (Bologna) 39 (2014): 79–93. doi:10.4454/ofioliti.v39i2.431
info:cnr-pdr/source/autori:Pandeli E.[1,3], Santo A.P.]1,3], Candido M.R.[1], Petrone C.M.[2], Giusti R.[1]/titolo:The calc-alkaline Monte Capo Stella dykes in the Ophiolitic Unit of the Elba Island (Italy): Geological setting and compositional characterization/doi:10.4454%2Fofioliti.v39i2.431/rivista:Ofioliti (Bologna)/anno:2014/pagina_da:79/pagina_a:93/intervallo_pagine:79–93/volume:39

In this paper we studied in detail magmatic dykes filling fractures in the pillow lavas of the Ophiolitic Unit cropping out in the Monte Capo Stella Promontory (southern part of the Elba Island in the Northern Tyrrhenian Sea). The Elba Island is well

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http://www.cnr.it/prodotto/i/350193