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precursor seismic monitoring system protection Civil Montebelluna

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you want an excerpt from the report card geostructural Modenese Apennines (Bettelli, Sandwiches, Capitani, 2002) inherent in the subject area.

The

site is located south of the Faeto.

From the image we see an alignment of planar surfaces with a triangular shape in some cases, poorly preserved and replanted. The triangular and trapezoidal surfaces are an example of the model by exogenous processes corresponding to a fault in the map shown below (Bettelli, Sandwiches, Capitani, 2002):

The triangular facets and rejuvenation of the band who finds himself half-height for most of the side can give information on the likely activity of the fault. This activity occurred in the country would observe the evventuale rejuvenation along the surface of the fault.

Our "Shovel" (and all the side) of tectonic origin, is currently shaped by processes of degradation of the surface layers of debris that form at the foot of the slope.
morphogenetic model which describes the genesis of this side is the "model denudazionale for recession straight with variation of the slope (

Brancaccio et al., 1978 ). The slope was modeled by a series of processes of chemical weathering and physical erosion, in correspondence with the main tectonic structure of the slope leading all'arretramento and / or a reduction of slope.

You can compare the shape of the pyramid

morfostruttura Vesallo

Reggiano Apennines.

the Geological Map of Italy with 50,000 shows the tectonic contact between Flysh Monte Cassio (MCS - Creataceo-Eocene) and Shales palombini (APA - dark green), and Varicolori Cassius Clay (AVV - Light Green).

stratigraphically belong to both and, more specifically Liguride CHAMBERS and APA are all those lithologies that in the 70s were defined as "undifferentiated chaos". Since the 80 / 90 have distinguished different lithologies mostly with clay matrix in which are found lithoid blocks (app. Modena). In other areas are kept well stratigraphy strongly deformed by tectonic (app. Parma). These formations are also known as pre-Flysh

Above are the Flysh and Monte Cassio tectonic contact with

Bibliography: BETTELLA G., F. PANINI, Captain M. (2002), Geological Map - Structural Emiliano Apennines East. From: Proceedings of the third workshop on the geological mapping.
BRANCACCIO L., CINQUE A., Sgrosso I (1978), Morphological analysis of the slopes as a tool for Reconstruction of neotectonic events. Mem Soc Geol lt, 19, pp. 621-626.

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