Record Details

Title Towards a 3D velocity model deduced from 2D seismic processing and interpretation in Northern Alsace (France)
Authors Maurer, V; Perrinel, N; Dalmais, E; Richard, A; Plévy, L; Genter, A
Year 2016
Conference European Geothermal Congress
Keywords Geothermal Project, Seismic Interpretation, Velocity Model, 3D Modeling, Alsace
Abstract Since the last decade, geothermal exploitation activity in the Upper Rhine Graben (URG) has been on-going with several German, Swiss and French deep geothermal sites such as Bruchsal, Bruhl, Groβ Gerau, Insheim, Landau for Germany, Basel, Riehen for Switzerland and Soultz-sous-Forêts, Rittershoffen for France, which are active from exploration to exploitation. All these projects deal with deep fractured geothermal reservoirs located within Triassic-sediments and/or crystalline basement. Since 2011, Electricity of Strasbourg is the holder or co-holder of several exclusive lease for the exploration of high temperature geothermal fields (>150°C) in the Northern Alsace (France). This paper is part of an exploration phase, where we attempt to combine different stratigraphic models realized for four exclusive licenses (Soultz-sous-Forêts, Rittershoffen, Wissembourg, and Lauterbourg) using a modeling software. In a first step, this paper aims to harmonize reprocessed seismic sections interpretation derived from several acquisitions through time within a unique model in order to compile each unique interpretation of the four licenses within a same Northern Upper Rhine Graben 3D model. In a second step, velocity data acquired during drilling campaigns have been used to estimate the local interval velocity of major interpreted geological formations. This time-depth relationships data allowing a conversion from a time based model to a depth based model. Such an outcome has various geothermal applications. For example, it allows the location of induced seismicity in 3D structures representing a significant improvement of events location or it can be used to constrain interpretation of results obtained by other geophysical methods, such as potential methods.
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