Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Citation Map Services Email this article to a friend Similar articles in this journal Similar articles in Web of Science Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via Web of Science (1) Citing Articles via Google Scholar Google Scholar Articles by Melluso, L. Articles by Saccani, E. Search for Related Content GeoRef GeoRef Citation

REPLY TO STOPPA ET AL. 2005

Wollastonite- anorthite- gehlenite-, and fassaite-bearing rocks: Igneous petrological oddity or paralavas?

Leone Melluso^1,*, Sandro Conticelli^2,, Massimo D’Antonio¹, Nicoletta P. Mirco³ and Emilio Saccani⁴

¹ Dipartimento di Scienze della Terra, Università degli Studi di Napoli Federico II, Via Mezzocannone, 8, I-80134, Napoli, Italy
² Dipartimento di Scienze della Terra, Università degli Studi di Firenze, and Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche, Via G. La Pira, 4, I-50121, Firenze, Italy
³ Via V. Monti, 1R, I-50124, Firenze, Italy
⁴ Dipartimento di Scienze della Terra, Università degli Studi di Ferrara, Corso Ercole I d’Este 32, I-44100 Ferrara, Italy

Correspondence: ^* E-mail: melluso{at}unina.it

ABSTRACT

We briefly 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 finding.

This article has been cited by other articles:

				E. Boari, S. Tommasini, M. A. Laurenzi, and S. Conticelli Transition from Ultrapotassic Kamafugitic to Sub-alkaline Magmas: Sr, Nd, and Pb Isotope, Trace Element and 40Ar-39Ar Age Data from the Middle Latin Valley Volcanic Field, Roman Magmatic Province, Central Italy J. Petrology, July 1, 2009; 50(7): 1327 - 1357. [Abstract] [Full Text] [PDF]

				E. Boari and S. Conticelli MINERALOGY AND PETROLOGY OF ASSOCIATED Mg-RICH ULTRAPOTASSIC, SHOSHONITIC, AND CALC-ALKALINE ROCKS: THE MIDDLE LATIN VALLEY MONOGENETIC VOLCANOS, ROMAN MAGMATIC PROVINCE, SOUTHERN ITALY Can Mineral, December 1, 2007; 45(6): 1443 - 1469. [Abstract] [Full Text] [PDF]