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Ritrovamento di epidoto fra i prodotti di trasformazione idrotermale di un monzogabbro (loc. Canzoccoli, Predazzo)

Noris MorandiM. Carla Nannetti — 1979

Atti della Accademia Nazionale dei Lincei. Classe di Scienze Fisiche, Matematiche e Naturali. Rendiconti

Mineralogical and petrographic studies on the epidotized monzogabbro outcrop observed at Canzoccoli (Predazzo) are reported. The clinopyroxenes of the monzogabbro are chloritized, the feldspars are rounded and enclosed in a chlorite-calcite-epidote matrix. The epidote is also enriched in veins or in big lenticular masses. The optical and crystal-chemical study defines the epidote as a Ps = 24% term. The colour of the epidote mineral tends to darker tones the higher the Fe-content. A genetic mechanism...

Ritrovamento di scapolite in un'area di contatto dei M.ti Monzoni (Toal della Traverselliti). II. Spettroscopia I.R. e studio roentgenografico

Noris MorandiM. Carla NannettiRossana Pirani — 1979

Atti della Accademia Nazionale dei Lincei. Classe di Scienze Fisiche, Matematiche e Naturali. Rendiconti

Scapolite occurs as large idiomorphic crystals forming pseudoradiating aggregates in veins in the monzonitic rocks. It is associated with zeolites (analcime, natrolite and scolecite), calcite, ferroan chlorites, K-feldspar, sphene and apatite. The samples were examined by x-ray diffraction and I.R. absorption spectroscopy. The results define the mineral as a M e 36 scapolite term, containing C 0 3 and OH as essential constituents, Cl and S 0 4 as trace. The relationships between physical data and composition...

Ritrovamento di scapolite in un'area di contatto dei M.ti Monzoni (Toal della Traversellite). I. Chimismo e studio ottico

Noris MorandiM. Carla NannettiRossana Pirani — 1979

Atti della Accademia Nazionale dei Lincei. Classe di Scienze Fisiche, Matematiche e Naturali. Rendiconti

Scapolite occurs as large idiomorphic crystals forming pseudoradiating aggregates in veins in the monzonitic rocks. It is associated with zeolites (analcime, natrolite and scolecite), calcite, ferroanchlorites, K-feldspar, sphene and apatite. The samples were examined by optical methods and chemical tests. The results define the mineral as a M e 36 scapolite term, containing C 0 3 and OH as essential constituents and Cl and S O 4 as trace.

Ritrovamento di scapolite in un'area di contatto dei M.ti Monzoni (Toal della Traversellite). III: Comportamento termico

Rossana PiraniNoris MorandiM. Carla Nannetti — 1979

Atti della Accademia Nazionale dei Lincei. Classe di Scienze Fisiche, Matematiche e Naturali. Rendiconti

Research on a K-rich scapolite, containing OH and C 0 3 as anionic constituents was carried out to correlate the thermal behaviour and the heating effects on chemical composition, x-ray and I.R. absorption results. The scapolite-plagioclase stability relations at high temperatures are discussed.

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