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- W2023396005 abstract "The pre-Neogene basement of the Vienna Basin comprises, among others, the late TriassicHauptdolomit, which serves as a gas reservoir below the Neogene silicilastic sediments. Both Alpinenappe stacking and the formation of the pull-apart basin in the Miocene affected this rock after itsdeposition. This polyphase deformation resulted in the generation of a dense fracture network, presentfrom nano-scale (microfractures) to map-scale (thrusts and strike-slip faults). The assessment ofpetrophysical properties, especially porosity and permeability, is, however, a non-trivial task in thiskind of fractured reservoir. Clearly, the scale of observation of well logging, even for advancedtechniques like Formation Micro Imager (FMI) logging, does not cover the whole range of relevantfracture distribution. In particular, fractures of only a few micrometers width may contributesignificantly to the fracture volume (and therefore to the reservoir storage capacity), as they are inmany cases closely spaced (some few millimetres) and intersect in a dense fracture network." @default.
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- W2023396005 date "2011-05-27" @default.
- W2023396005 modified "2023-09-23" @default.
- W2023396005 title "Quantifying Porosity and Calculating Permeability in Reservoir Rocks of the Vienna Basin" @default.
- W2023396005 doi "https://doi.org/10.3997/2214-4609.20144746" @default.
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