Preliminary results of the 3D modeling of the Calcari Grigi carbonate platform (Early Jurassic, Southern Alps, Italy).

M. Franceschi and Matteo Massironi and P. Franceschi and M. Zandonati and V. Picotti. ( 2013 )
in: Proc. 33rd Gocad Meeting, Nancy

Abstract

3D modeling represents a standard procedure in the characterization of large-scale buried geologic bodies. While seismics provides important information about geometries at depth, facies characterization is often less capillary. That is one of the reasons for which outcrop analogues turn out useful, although they normally do not match the scale of subsurface bodies. We present preliminary results in the 3D modeling of the Early Jurassic Calcari Grigi carbonate platform. The platform (size ~100km x 100km, up to 400m thick) consists of several sub-environments (tidal flats, deep lagoons, oolitic shoals), now exhumed in the Southern Alps (Italy), a poorly deformed portion of the Mesozoic passive margin of Adria. Despite some alpine faulting and folding, lateral relationships between Jurassic units are still preserved. During Early Jurassic, the platform was affected by synsedimentary tectonics, testified by exposed structures, controlling sharp variations in the thickness of its units. Excellent outcrop continuity, extensive geological mapping and previous studies provide a great wealth of field data that give the opportunity to produce a 3D model of a seismic-scale carbonate platform. 3D modeling was carried out with SKUA®. Main stratigraphic horizons and geometries of the sedimentary prisms were modeled. Spatial variability of the platform units’ thickness was studied with geostatistics to retrieve information about the arrangement of the Jurassic fault system that drove subsidence during rifting. This helped to estimate the position of main Jurassic faults and revealed an extensive orthorhombic faultnetwork at the platform scale. The 3D model can now be populated with facies information, derived from outcrop data and geologic maps, to evaluate the influence of tectonics on the depositional and diagenetic environments. The model of a carbonate platform of this size potentially represents a useful analogue for carbonate reservoirs and help the understanding of similar buried sedimentary bodies.

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BibTeX Reference

@inproceedings{FranceschiGM2013,
 abstract = { 3D modeling represents a standard procedure in the characterization of large-scale buried geologic bodies. While seismics provides important information about geometries at depth, facies characterization is often less capillary. That is one of the reasons for which outcrop analogues turn out useful, although they normally do not match the scale of subsurface bodies. We present preliminary results in the 3D modeling of the Early Jurassic Calcari Grigi carbonate platform. The platform (size ~100km x 100km, up to 400m thick) consists of several sub-environments (tidal flats, deep lagoons, oolitic shoals), now exhumed in the Southern Alps (Italy), a poorly deformed portion of the Mesozoic passive margin of Adria. Despite some alpine faulting and folding, lateral relationships between Jurassic units are still preserved. During Early Jurassic, the platform was affected by synsedimentary tectonics, testified by exposed structures, controlling sharp variations in the thickness of its units. Excellent outcrop continuity, extensive geological mapping and previous studies provide a great wealth of field data that give the opportunity to produce a 3D model of a seismic-scale carbonate platform. 3D modeling was carried out with SKUA®. Main stratigraphic horizons and geometries of the sedimentary prisms were modeled. Spatial variability of the platform units’ thickness was studied with geostatistics to retrieve information about the arrangement of the Jurassic fault system that drove subsidence during rifting. This helped to estimate the position of main Jurassic faults and revealed an extensive orthorhombic faultnetwork at the platform scale.
The 3D model can now be populated with facies information, derived from outcrop data and geologic maps, to evaluate the influence of tectonics on the depositional and diagenetic environments. The model of a carbonate platform of this size potentially represents a useful analogue for carbonate reservoirs and help the understanding of similar buried sedimentary bodies. },
 author = { Franceschi, M. AND Massironi, Matteo AND Franceschi, P. AND Zandonati, M. AND Picotti, V. },
 booktitle = { Proc. 33rd Gocad Meeting, Nancy },
 title = { Preliminary results of the 3D modeling of the Calcari Grigi carbonate platform (Early Jurassic, Southern Alps, Italy). },
 year = { 2013 }
}