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DISS 3.2.GreDaSS: Seismogenic Source GRCS070 - Amyndeo | ![]() |
Source Info Summary | Commentary | Pictures | References |
Geologcal sketches showing the stepping pattern of the Quaternary Petron-Xino Nero-Nymfeon fault. (a) General sketch of fault structure in Petron area. 1, Basement's Triassic-Jurassic limestones. 2, Plio-Quaternary sediments. 3, Alluvial. (b) Detailed sketch of one of the small Quaternary faults (25°/78° W) near Petron springs, where the dipping of the hangingwall formations is in between 25° and 30° NNW. 1, Neogene sediments. 2, Quaternary conglomerates. 3, Alluvials
[from Pavlides (1985)].
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