Modeling the Mogi magma source centre of the Santorini (Thera) volcano, Aegean Sea, Greece, 1994-1999, based on a numerical-topological approach

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Studia Geophysica et Geodaetica, Vol. 56, Iss. 4, 2012-10 ,pp. : 1037-1062

Springer Publishing Company

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New insights into the initiation and venting of the Bronze-Age eruption of Santorini (Greece), from component analysis

By Druitt T.  

Bulletin of Volcanology, Vol. 76, Iss. 2, 2014-02 ,pp. : 1-21

Springer Publishing Company

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Seismicity rate changes in association with the evolution of the stress field in northern Aegean Sea, Greece

By Leptokaropoulos K. M.   Papadimitriou E. E.   Orlecka-Sikora B.   Karakostas V. G.  

Geophysical Journal International, Vol. 188, Iss. 3, 2012-03 ,pp. : 1322-1338

Oxford University Press

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Upward extrusion and subsequent transpression as a possible mechanism for the exhumation of HP/LT rocks in Evia Island (Aegean Sea, Greece)

By Xypolias P.   Kokkalas S.   Skourlis K.  

Journal of Geodynamics, Vol. 35, Iss. 3, 2003-04 ,pp. : 303-332

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An Upper Pliocene coarse pumice breccia generated by a shallow submarine explosive eruption, Milos, Greece

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Bulletin of Volcanology, Vol. 66, Iss. 1, 2004-01 ,pp. : 15-28

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