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- W4322001275 abstract "We present SEISC-3D, an ArcGIS geodatabase for 3D SEIsmic Source Characterization. It integrates multi-scale and multi-depth geological and seismological information in a compressional environment to build a detailed regional-scale, geometric and kinematic, 3D curvilinear fault model suitable for seismic hazard modelers and seismotectonic purposes and geodynamic modeling. This first release focuses on the late Pliocene-to-Quaternary arcuate and eastward convex fold-and-thrust belt still active along the Outer front of the Italian Apennines in eastern Central Italy. The near-surfaces, onshore, and offshore thrust faults represent the hanging-wall structures of a potentially seismogenic regional shear zone, known as Adriatic Basal Thrust, which develops from near-surface to MOHO depths (about 35 km).Three hierarchic levels of structural maps are provided with decreasing details moving from fold-and-thrusts traces, enveloping thrust, and regional thrust alignments.Different datasets (points, lines, surfaces) are unified, compiled, and held in a common ArcGIS file system folder and linked on the basis of relational models.SEISC is composed of:one dataset consisting of fold hinges traces (syncline and anticlines) one dataset consisting of individual fold-related thrust one dataset consisting of enveloping thrusts organized in hierarchic orders one dataset consisting of interconnected curvilinear fault surfaces built along the down-dip projection of the enveloping thrusts, segmented along-strike and along-dip one structural data set containing geometric and kinematic point data (attitude, dip-angle, slip-vector, rake, sense of movement) for the node of each triangulated mesh of each fault surface. A crucial point when dealing with compressional structures is the difficulty in adopting segmentation criteria suitable for a realistic earthquake-fault association. In our methodological approach, the along-strike segmentation is strongly driven by the en-echelon distribution of the fold-related thrusts and by sharp variation in strikes and bending of the enveloping thrusts. On the other hand, the down-dip segmentation is controlled by the mechanical crustal layering derived from earthquake distributions and the rheological investigation." @default.
- W4322001275 created "2023-02-26" @default.
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- W4322001275 date "2023-05-15" @default.
- W4322001275 modified "2023-10-03" @default.
- W4322001275 title "A conceptual 3D fold-and-thrust database for seismic hazard, seismotectonic and geodynamic purposes - a first release from eastern Central Italy" @default.
- W4322001275 doi "https://doi.org/10.5194/egusphere-egu23-11810" @default.
- W4322001275 hasPublicationYear "2023" @default.
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