Cartographic geological and structural data collected in the field and managed by GIS technology can be used for 3D reconstruction of complex geological bodies. Using a link between GIS tools and gOcad, stratigraphic and tectonic surfaces can be reconstructed taking into account any geometrical constraints deriving from field observations. Complex surfaces can be reconstructed using large data sets analyzed by suitable geometrical techniques. Three main typologies of geometric features and related attributes are exported from a GISgeodatabase: 1) topographic data as points from a digital elevation model, 2) stratigraphic and tectonic boundaries, and linear features as 2D polylines, 3) structural data as points. After having imported the available information into gOcad, the following steps should be performed: 1) construction of the topographic surface by interpolation of points; 2) 3D mapping of the linear geological boundaries and linear features by vertical projection on the reconstructed topographic surface; 3) definition of geometrical constraints from planar and linear outcrop data; 4) construction of a network of cross-sections based on field observations and geometrical constraints; 5) creation of 3D surfaces, closed volumes and grids from the constructed objects. Three examples of the reconstruction of complex geological bodies from the Italian Alps are presented here. The methodology demonstrates that although only outcrop data were available, 3D modeling has allowed to check the geometrical consistency of the interpretative 2D sections and of the field geology, through a 3D visualisation of geometrical models. Application of a 3D geometrical model to the case-studies can be very useful in geo-mechanical modeling for slopestability or resources evaluation.

3D reconstruction of complex geological bodies: examples from the Alps

Zanchi A;Sterlacchini S;
2009

Abstract

Cartographic geological and structural data collected in the field and managed by GIS technology can be used for 3D reconstruction of complex geological bodies. Using a link between GIS tools and gOcad, stratigraphic and tectonic surfaces can be reconstructed taking into account any geometrical constraints deriving from field observations. Complex surfaces can be reconstructed using large data sets analyzed by suitable geometrical techniques. Three main typologies of geometric features and related attributes are exported from a GISgeodatabase: 1) topographic data as points from a digital elevation model, 2) stratigraphic and tectonic boundaries, and linear features as 2D polylines, 3) structural data as points. After having imported the available information into gOcad, the following steps should be performed: 1) construction of the topographic surface by interpolation of points; 2) 3D mapping of the linear geological boundaries and linear features by vertical projection on the reconstructed topographic surface; 3) definition of geometrical constraints from planar and linear outcrop data; 4) construction of a network of cross-sections based on field observations and geometrical constraints; 5) creation of 3D surfaces, closed volumes and grids from the constructed objects. Three examples of the reconstruction of complex geological bodies from the Italian Alps are presented here. The methodology demonstrates that although only outcrop data were available, 3D modeling has allowed to check the geometrical consistency of the interpretative 2D sections and of the field geology, through a 3D visualisation of geometrical models. Application of a 3D geometrical model to the case-studies can be very useful in geo-mechanical modeling for slopestability or resources evaluation.
2009
Istituto per la Dinamica dei Processi Ambientali - IDPA - Sede Venezia
Istituto di Geologia Ambientale e Geoingegneria - IGAG
3D modeling
field mapping
structural geology
Alps
GOCAD
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/48177
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