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Publications by [Pomoni - Papaioannou F.]

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<p>The Triassic Breccias of the Ionian zone are typical evaporite dissolution collapse breccias. Several features indicate the pre-existence of evaporites, while alternation of dolomites and evaporites consist a very cornmon association in the subsurface. ...
Filed under: Geology -  Economic Geology
Reference: Carbonates & Evaporites, v. 13, no. 2, 1998, no. 207-218.