To study what had actually happened, two seismic profiles were done in the sliding area, by the method of refracted and surface waves, using geophones that accept vertical and horizontal oscillations. For the identification of the geological and tectonic construction of the study area, mainly the seismic works performed for the search of hydrocarbons have been used, through which tectonic faults with very large amplitude up to those with small amplitude of several tens of meters have been identified. This region is part of the Molasses basin of the Peri-Adriatic Depression area. The study area is included in the Peri-Adriatic Depression, Synej region, where on Maa landslide occurred, which completely destroyed 9 houses. For this purpose, refracted and surface seismic waves, artificially generated (active seismic), and natural (passive seismic) were used. Although such techniques are well established for the laboratory and field scale, the potential of current (Hyperion) and upcoming spaceborne sensors such as EnMAP for quantitative mineralogical and salt spectral mapping is still to be demonstrated.Active and passive seismic methods have been widely used for the study of landslides. In these wavelength regions major chemical components of the soil interact with the electromagnetic radiation and produce characteristic absorption features that can be used to derive the properties of interest. High spectral resolution remote sensing can estimate evaporite content and mineralogy of soils based on the analyses of the surface reflectance properties within the Visible-Near InfraRed (VNIR 400-1000 nm) and Short-Wave InfraRed (SWIR 1000-2500 nm) regions. Furthermore, the dynamic of the salt pans, especially the formation of evaporites, is still uncertain and poorly understood. Up to now the soil composition of salt pans in this area have been only assessed mono-temporally and on a coarse regional scale. They are very sensitive to environmental conditions, and as thus hydrological, mineralogical and ecological responses to climatic variations can be analysed. In this context the Kalahari salt pans (also known as playas or sabkhas) and their peripheral saline and alkaline habitats are an ecosystem of major interest.
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