Levynes and erionites from Sardinia, Italy
β Scribed by E. Passaglia; E. Galli; R. Rinaldi
- Publisher
- Springer
- Year
- 1974
- Tongue
- English
- Weight
- 825 KB
- Volume
- 43
- Category
- Article
- ISSN
- 0010-7999
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β¦ Synopsis
Three samples of levyne and two of erionite from three different localities of Sardinia are described. In two samples, levyne and erionite are intergrown by epitaxy. The levynes exhibit close chemical compositions with Ca>Na>K; as for their lattice constants, a is very similar in all three samples, while c of one sample is rather smaller than that of the other two. Unit cell dimensions of both erionites and chemical composition of one are also given. In addition, the following data are reported for the levynes: refractive indices for all three samples, density for two and DTA for one. The existence of levyne-erionite intergrowth is emphasized, and support is given to the idea that this intergrowth is much more common than the literature would suggest.
π SIMILAR VOLUMES
The Variscan nappe stack of SE Sardinia originated as a result of several stages of nappe imbrication during the Lower Carboniferous phases of the Variscan orogeny. The crustal shortening caused regional SSWβand Wβdirected thrusting, greenschist facies metamorphism and openβtoβisoclinal polyphase fo