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Traditional methods to identify the geological structure of the rock mass are based mainly on the analysis of cores from boreholes. Today, more and more often geophysical methods are introduced to support classical methods or completely replace them. One of the major advantages of this type of measurement is non-invasive analysis of the rock mass. Due to the nature of this type of geophysical measurements...
The Dębowiecki conglomerate is a coarse-grained Miocene sediment, which occurs in the western part of the Carpathian Foredeep between Cieszyn, Jastrzębie and Bielsko (Poland). This unit includes varigrained conglomerates and coarse-grained sandstones. The thickness of the unit may reach up to 260 m. The Dębowiecki conglomerate was mentioned for the first time by Petrascheck (see Konior 1965). However,...
Middle Miocene marine sediments in the Vienna Basin provide opportunities for analyses of spatial and temporal variation in the composition of molluscan communities, especially across the Badenian/Sarmatian boundary. In this study, we describe variation in composition of molluscan assemblages with multivariate analyses (cluster and ordination analyses). In ongoing analyses, we test whether Badenian...
Microseismic monitoring is usually used to map hydraulic fracture or stress changes in the reservoir, which is stimulated (Maxwell et al. 2010, Duncan & Eisner 2010). Examining the wave traveling through the reservoir can provide many important information on medium properties (Grechka et al. 2011) and can be used either to assess the stimulated reservoir or improve microseismic imagining. Microseismic...
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