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by Donato_VA in science-technology
Buco del Piombo Cave - Alpe del viceré complex - Southern alps - Lombardy - Italy Cave Deposits with flattened and imbricated pebbles in a fine matrix. The sedimentary wreck is protected and resting on a fault plane characterized by kinematic indicators such as grooves, steps and calcitic mineralizations. The fault plane, in low angle and concordant with bedding, can be ascribed to flexural sliding in a simple shear system in agreement with regional tectonics.