Titlebook: Nisyros Volcano; The Kos - Yali - Nis Volker J?rg Dietrich,Evangelos Lagios Book 2018 Springer International Publishing AG 2018 Dodecanese

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2195-3589 s Plateau Tuff”) in the history of the eastern Mediterranean devastated the Dodecanese islands 161,000 years ago. Although the last volcanic activity on Nisyros dates back at least 20,000 to 25,000 years, it en978-3-319-85667-4978-3-319-55460-0Series ISSN 2195-3589 Series E-ISSN 2195-7029

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Geodynamics and Volcanism in the Kos-Yali-Nisyros Volcanic Field,cover, submarine volcanic features and fault zones within the different basins, troughs and horsts. Geological outlines and maps are given for all volcanic eruptive centers: Kos Island and the distribution of the 161,000 years old Kos Plateau Tuff, Nisyros Volcano, Yali Island, Strongyli Volcano, Av

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Geology of Nisyros Volcano,ive volcanic cycles has been devised using eruptive successions, contact relationships, epiclastic deposits and intercalated paleosols. Volcanic activity started with shallow submarine basaltic-andesitic lavas during the “Early Shield Volcano Cycles” evolving into a subaerial environment with local

Chronological

Petrology and Geochemistry of Lavas and Pyroclastics,s offered. The chapter concludes with a discussion on the petrogenetic evolution of the island, including crustal assimilation, fractional crystallisation, magma mixing and mingling, crystal-retention-liquid-segregation, the probable depth of the magma chamber and models for generating the highly si

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