Titlebook: Geomechanical Controls on Fracture Development in Chalk and Marl in the Danish North Sea; Understanding and Pr Michael John Welch,Mikael Lü

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Christine Bescherer,Andrea Hoffkamphrow faults seen from seismic amplitude sections. In plan view on stratigraphic horizons, sets of parallel or near-parallel lineations can be seen, with individual segments often linked together to form 200–1000 m long segments. At connecting junctions, the eXchroma. ant-tracked data shows highest v

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https://doi.org/10.34157/9783648158128. This is combined with mechanical property data from Amour et al. (this volume), and strain data from Petersen et al. (this volume) and Welch et al. (in .. Springer Nature Switzerland AG, 2020), to run a series of sensitivity models on a small area of Kraka. The results of these models are compared

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https://doi.org/10.1007/978-3-658-09692-2ural fractures. The sedimentological subdivision of the reservoir correlates with mechanical variations within the different layers, and core studies have shown that the characteristics of the natural fractures vary according to the sedimentary facies. The three reservoir units therefore form the ba

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Formen digitalen Krisenmanagements,se data are typically of varying quality and scales, creating an issue of non-uniqueness in the description of subsurface reservoirs used for e.g. energy and water production. The inclusion of onshore data from geological outcrops can increase the accuracy of 3D digital models used for subsurface ch

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Christine Bescherer,Andrea HoffkampXchroma. Petrel plug-in) and ant-tracking leading to higher vertical resolution than wavelet-based methods. The reason is that only seismic amplitude differences between adjacent time slices matter, rather than trace similarity, and thus leans on the concept of seismic detectability rather than reso