Saccà, Carmelo and Saccà, Domenica (1992) Composizione mineralogica e chimica di una mineralizzazione a prevalente pirite, affiorante in contrada croce, presso Fiumedinisi (Messina). Accademia Peloritana dei Pericolanti Classe FF.M.NN., 70. pp. 199-210.
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Abstract
A mineralization outcropping in C.da Croce locality (Fiumedinisi area), and mainly consisting of pyrite, has been investigated.
The studied samples belong to the “Mandanici Unit”, which is a low grade metamorphic unit of the northern Peloritan complex.
Results of microscopical investigations revealed a mineral association mainly consisting of quartz, pyrite, magnetite, ilmenite and chalcopyrite.
Both pyrite and quartz show two generations. Quartz has been observed in some fractures.
Chemical investigations revelead 46.41% Fe medium content for pyrite. No significant differences exist between the two pyrite generations.
As regards trace elements, the Co/Ni ratio in pyrite of almost 2 suggests a deposition due to a hydrothermal activity.
| Item Type: | Article |
|---|---|
| Subjects: | M.U.S. - Miscellanea > Atti Accademia Peloritana > Classe di Scienze Fisiche, Matematiche e Naturali > 1992 > 1992 Parte 2 M.U.S. - Miscellanea > Atti Accademia Peloritana > Classe di Scienze Medico-Biologiche > 1992 > 1992 Parte 2 M.U.S. - Miscellanea > Atti Accademia Peloritana > Classe di Scienze Giuridiche, Economiche e Politiche > 1992 > 1992 Parte 2 M.U.S. - Miscellanea > Atti Accademia Peloritana > Classe di Lettere Filosofia e belle Arti > 1992 > 1992 Parte 2 |
| Depositing User: | Dr M P |
| Date Deposited: | 21 Sep 2012 08:35 |
| Last Modified: | 02 Apr 2013 08:20 |
| URI: | http://cab.unime.it/mus/id/eprint/753 |
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