Όρος Πέταλο, Βασιλικό, Άνδρος, Κυκλάδες, Ελλάδα
The Mn-rich rocks are made up of highly oxidized quartzitic schists, quartzites and Mn-rich pyroxenoid and carbonate rocks. The ferromanganoan metasediments in central Andros form part of a volcano-sedimentary sequence that experienced low grade, high pressure metamorphism (P > 1,1 GPa; T = 360°-420°C) followed along the uplift path by a greenschist facies overprint.
References
- Bonazzi P., Menchetti S., Reinecke T. (1996): Solid solution between piemontite and androsite-(La), a new mineral of the epidote group from Andros Island, Greece. Amer. Mineral., 81, 735-742. [
http://www.minsocam.org/MSA/ammin/toc/Articles_Free/1996/Bonazzi_p735-742_96.pdf]
Mineral List
5 entries listed. 5 valid minerals. 1 type locality (valid mineral).
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