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Kos Plateau Tuff

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Journal Article
Published: 21 April 2020
Geological Magazine (2020) 157 (12): 2021–2032.
...David J.W. Piper; Georgia Pe-Piper Abstract The 161-ka Kos Plateau Tuff (KPT) eruption deposited widespread unwelded ignimbrites, but the Dikeos and Sympetro mountains on the SE of Kos Island blocked all but the most energetic pyroclastic flows. KPT remnants north of Sympetro mountain comprise...
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Journal Article
Journal: Geology
Published: 01 January 2007
Geology (2007) 35 (1): 73–76.
...O. Bachmann; B.L.A. Charlier; J.B. Lowenstern Abstract In contrast to most large-volume silicic magmas in continental arcs, which are thought to evolve as open systems with significant assimilation of preexisting crust, the Kos Plateau Tuff magma formed dominantly by crystal fractionation of mafic...
FIGURES
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The <span class="search-highlight">Kos</span> <span class="search-highlight">Plateau</span> <span class="search-highlight">Tuff</span> (KPT); location shown on  F igure  1 . ( L eft  ) Gene...
Published: 01 June 2019
Figure 2. The Kos Plateau Tuff (KPT); location shown on F igure 1 . ( L eft ) Generalized stratigraphic log of the Kos Plateau Tuff (KPT). Four eruptive phases (1–4) generated six major stratigraphic units: unit A is at the base, unit F is at the top. Phase 1 comprises Units A and B; phase 2
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Isochron slopes and age distributions of zircons from <span class="search-highlight">Kos</span> <span class="search-highlight">Plateau</span> <span class="search-highlight">Tuff</span>, Gre...
Published: 01 January 2008
Figure 13. Isochron slopes and age distributions of zircons from Kos Plateau Tuff, Greece, showing presence of continuous age distributions. A) Model isochron slopes and corresponding 238 U- 230 Th age distributions for granitoid xenoliths (top) and pumices (bottom). B) 238 U- 206 Pb age
Journal Article
Journal: Elements
Published: 01 June 2019
Elements (2019) 15 (3): 191–196.
...Figure 2. The Kos Plateau Tuff (KPT); location shown on F igure 1 . ( L eft ) Generalized stratigraphic log of the Kos Plateau Tuff (KPT). Four eruptive phases (1–4) generated six major stratigraphic units: unit A is at the base, unit F is at the top. Phase 1 comprises Units A and B; phase 2...
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Journal Article
Journal: Geology
Published: 03 February 2022
Geology (2022) 50 (4): 481–485.
... increasing economic importance, the behavior of lithium (Li) in such environments remains poorly known. We illustrate how compositionally unusual biotites from the rhyolitic Bishop Tuff (California, USA) and Kos Plateau Tuff (Greece) may contain a magmatic volatile phase trapped between layers of biotite...
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Journal Article
Journal: Geosphere
Published: 01 October 2010
Geosphere (2010) 6 (5): 470–481.
... compared to lab measurements of pumices produced by the Kos Plateau Tuff eruption to validate the method. New permeability data for pumices from other silicic volcanic deposits is presented, and an empirical model for permeability is tested using geometrical and topological data, i.e., tortuosity, specific...
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Lithium contents of biotites and coexisting groundmass glasses. (A) Biotite...
Published: 03 February 2022
Figure 2. Lithium contents of biotites and coexisting groundmass glasses. (A) Biotite compositions from low-total biotites (LTBs) showing highly enriched Li contents (note logarithmic scale). Campi Flegrei (Italy) data are from this study and Forni et al. (2018) . KPT—Kos Plateau Tuff. (B
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Biotite compositional and structural data. (A) Analytical totals of biotite...
Published: 03 February 2022
; Bachmann, 2010 ) systems are shown for comparison in pale colors. NTB—normal-total biotite; LTB—low-total biotite; KPT—Kos Plateau Tuff. (B,C) Appearance of biotites from Astroni pyroclastics (Campi Flegrei, Italy) (NTB) and Kos Plateau Tuff (LTB) deposits illustrating different textures observed
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