Quaternary faulting in the Upper Rhine Graben revealed by high-resolution multi-channel reflection seismic

2006 ◽  
Vol 338 (8) ◽  
pp. 574-580 ◽  
Author(s):  
Guillaume Bertrand ◽  
Philippe Elsass ◽  
Gunther Wirsing ◽  
Alex Luz
2009 ◽  
Vol 57 (3/4) ◽  
pp. 338-366 ◽  
Author(s):  
Hermann Buness ◽  
Gerald Gabriel ◽  
Dietrich Ellwanger

Abstract. Currently, the Heidelberg Basin is under investigation by new cored research boreholes to enhance the understanding concerning the control on Pliocene and Quaternary sedimentation by (neo)tectonics and climate. The Heidelberg Basin is expected to serve as a key location for an improved correlation of parameters that characterise the climate evolution in North Europe and the Alpine region. The recovery of sediment successions of high temporal resolution that are complete with respect to the deposition of Pleistocene glacials and interglacials in superposition is of special importance. Prior to the new research boreholes in Viernheim and Heidelberg geophysical pre-site surveys were performed to identify borehole locations that best achieve these requirements. In the area of the Heidelberg Basin the strongest negative gravity anomaly of the entire Upper Rhine Graben is observed (apart from the Alps), hinting at anomalously thick sediment deposits. However, especially reflection seismic profiles contributed significantly to the decision about the borehole locations. In the city of Heidelberg for the first time, the depocentre of the Heidelberg Basin, as indicated by additional subsidence compared to its surroundings, was mapped. In this area, sediments dip towards the eastern margin of the Upper Rhine Graben. This is interpreted to represent a rollover structure related to the maximum subsidence of the Upper Rhine Graben in this region. At the Viernheim borehole location the seismic survey revealed several faults. Although these faults are mainly restricted to depths greater than 225 m, the borehole location was fi nally adjusted with respect to this information.


2021 ◽  
Author(s):  
Matthis Frey ◽  
Sebastian Weinert ◽  
Kristian Bär ◽  
Jeroen van der Vaart ◽  
Chrystel Dezayes ◽  
...  

<p>The crystalline basement of the Upper Rhine Graben presents an attractive target for deep geothermal projects due to its favourable temperatures and its high potential as a fractured and faulted reservoir system. It is already exploited at several sites, e.g. Soultz-sous-Forêts or Landau, and further projects are currently planned or under development. The crystalline units are furthermore the main source of radiogenic heat production and thus, together with the shallow Moho depth and convective heat transport along large fault zones, significantly contributing to the crustal temperature field. For these reasons, we developed the most detailed 3D geological model of the basement in the northern Upper Rhine Graben to date within the Interreg NWE DGE-ROLLOUT and Hesse 3D 2.0 projects. Due to the small number of very deep boreholes as well as seismic profiles reaching the basement beneath the locally more than 5 km thick sedimentary cover, we additionally used high-resolution magnetic and gravity datasets. In contrast to common deterministic modelling approaches, we performed a stochastic joint inversion of the geophysical data by applying a Monte Carlo Markov Chain algorithm. This method generates a large set of random but valid models, which enables a statistical evaluation of the results, e.g. concerning the model uncertainties. For a realistic attribution of the model, we used existing petrophysical databases of the region and measured the magnetic susceptibility of more than 430 rock samples. As a result of the inversion, high-resolution voxel models of the density and susceptibility distribution were generated, allowing conclusions about the composition and structure of the crystalline crust, which leads to a reduction of uncertainties and risks associated with deep geothermal drillings in the northern Upper Rhine Graben. Furthermore, our model will serve as a basis for realistic simulations of heat transport processes in the fractured basement and a meaningful assessment of the deep geothermal potential in the future.</p>


2015 ◽  
Vol 203 (1) ◽  
pp. 614-631 ◽  
Author(s):  
T. Fuhrmann ◽  
M. Caro Cuenca ◽  
A. Knöpfler ◽  
F.J. van Leijen ◽  
M. Mayer ◽  
...  

PalZ ◽  
2007 ◽  
Vol 81 (4) ◽  
pp. 365-375 ◽  
Author(s):  
Bettina Reichenbacher München ◽  
Jean Gaudant Paris ◽  
Thomas W. Griessemer

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