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Montecatini Val di Cecina

Montecatini Val di Cecina 4.1 - Minette neck with high-silica lamproitic composition, permeated by leucocratic veins. [Pg.19]

Moderate evolutionary modification of mafic melts during emplacement, with some fractional crystallisation, crustal assimilation (e.g. at Torre Alfina) and unmixing of felsic residual melts at Montecatini Val di Cecina. [Pg.42]

See other pages where Montecatini Val di Cecina is mentioned: [Pg.31]    [Pg.32]   
See also in sourсe #XX -- [ Pg.19 , Pg.32 ]



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