An FT-Raman, Raman and FTIR study of hydrothermally altered volcanic rocks from Kos Island (Southeastern Aegean, Greece)

Author:

Papoulis D.,Tsolis-Katagas P.,Tsikouras B.,Katagas C.

Publisher

Elsevier

Reference30 articles.

1. Reconstruction of a major caldera-forming eruption from pyroclastic deposit characteristics: Kos Plateau Tuff, eastern Aegean Seas;Allen;J. Volc. Geoth. Res.,2001

2. Stratigraphy of the Kos Plateau Tuff: Products of a major Quaternary explosive rhyolitic eruption in the eastern Aegean Sea;Allen;Int. J. Earth Sci.,1999

3. Der jungtertiäre Monzonit von Kos und sein Kontakthof (Ägäis, Griechenland);Altherr;Bull. Soc. Géol. France,1976

4. A late Oligocene/early Miocene high temperature belt in the Attic-Cycladic Crystalline Complex (SE Pelagonian, Greece);Altherr;N. Jb. Geol.,1982

5. Geological and geochronological evidences on the evolution of Kos-Jali-Nisyros eruptive centres, Aegean arc, Greece;Boven;Terra Cognita,1987

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