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 scapolite term, containing and OH as essential constituents, Cl and as trace. The relationships between physical data and composition are quite satisfactory.
@article{RLINA_1979_8_66_5_423_0,
author = {Noris Morandi and M. Carla Nannetti and Rossana Pirani},
title = {Ritrovamento di scapolite in un'area di contatto dei M.ti Monzoni (Toal della Traverselliti). II. Spettroscopia I.R. e studio roentgenografico},
journal = {Atti della Accademia Nazionale dei Lincei. Classe di Scienze Fisiche, Matematiche e Naturali. Rendiconti},
volume = {66},
year = {1979},
pages = {423-428},
language = {it},
url = {http://dml.mathdoc.fr/item/RLINA_1979_8_66_5_423_0}
}
Morandi, Noris; Nannetti, M. Carla; Pirani, Rossana. Ritrovamento di scapolite in un'area di contatto dei M.ti Monzoni (Toal della Traverselliti). II. Spettroscopia I.R. e studio roentgenografico. Atti della Accademia Nazionale dei Lincei. Classe di Scienze Fisiche, Matematiche e Naturali. Rendiconti, Tome 66 (1979) pp. 423-428. http://gdmltest.u-ga.fr/item/RLINA_1979_8_66_5_423_0/
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