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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Terra nova 9 (1997), S. 0 
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: An integrated interpretation of seismicity, fault plane solutions and deep seismic reflection data suggests that the NE–SW to NW–SE trending Rhone–Simplon fault zone and the gently S-dipping basal Penninic thrust separate fundamentally different stress regimes in the western Swiss Alps. North of the Rhone-Simplon fault zone, strike-slip earthquakes on steep-dipping faults within the Helvetic nappes are a consequence of regional NW–SE compression and NE–SW extension. To the south, vertical maximum stress and N–S extension are responsible for normal mechanism earthquakes that occur entirely within the Penninic nappes above the basal Penninic thrust. Such normal faulting likely results from extension associated with southward movements (collapse) of the Penninic nappes and/or continued uplift and relative northward displacements of the underlying Alpine massifs. Geological mapping and fission-track dating suggest that the two distinct stress regimes have controlled tectonism in the western Swiss Alps since at least the Neogene.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2014-06-27
    Description: Sinkhole development created by diverse subsidence mechanisms (suffosion, collapse, sagging) constitutes the main hazard in most karst terrains. Precisely mapping the limits of sinkholes and inferring the subsidence mechanisms are critically important for the effective mitigation of sinkhole risk. Gathering this information commonly requires the application of subsurface investigation methods, such as geophysics or trenching. Here, we analyze the potential of ground-penetrating radar (GPR) for sinkhole characterization in covered karsts. Extensive GPR surveys have been conducted across two buried active sinkholes of contrasting genetic types (collapse vs. sagging) in the mantled evaporite karst of Zaragoza city, NE Spain. Data were acquired with 100 MHz and 50 MHz unshielded antennas and ~180 MHz shielded antennas. Interpretation of the processed GPR profiles allowed us to map reliably the boundaries of the sinkholes, characterize their internal geometries (deformation style), infer the subsidence mechanisms, and estimate subsidence magnitudes. The suitability and limitations of the GPR technique in covered karsts are illustrated considering different sinkhole types and sizes, as well as data acquired with different antennas (shielded versus unshielded and various frequencies).
    Print ISSN: 1078-7275
    Topics: Geosciences
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