Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/646
AuthorsMelluso, L.* 
Conticelli, S.* 
D'Antonio, M.* 
Saccani, E.* 
TitleWollastonite- anorthite- gehlenite-, and fassaite-bearing rocks: Igneous petrological oddity or paralavas?
Issue Date2005
Series/Report no.90
DOI10.2138/am.2005.453
URIhttp://hdl.handle.net/2122/646
KeywordsWollastonite
gehlenite
Subject Classification04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology 
04. Solid Earth::04.04. Geology::04.04.07. Rock geochemistry 
AbstractWe brieß y review the petrological and geochemical features, and physical characteristics, of the Colle Fabbri and Ricetto rocks to discuss their possible paramagmatic origin, i.e., derived from complete melting, after devolatilization, of marly protoliths, without any orthomagmatic, ultimately mantle-derived, chemical or thermal input. Contrary to the various comments that have been made, the overall mineralogical, petrological, and geochemical data provided in the literature well agree with this Þ nding.
Appears in Collections:Papers Published / Papers in press

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