the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 08 Mar 2022
The analysis of slip tendency of major tectonic faults in Germany
Abstract. Seismic hazard during subsurface operations is often related to the reactivation of pre-existing tectonic faults. The analysis of the slip tendency, i.e. the ratio of shear to normal stress acting on the fault plane, allows an assessment of the reactivation potential of faults. We use the total stresses that result from a large-scale 3D geomechanical-numerical model of Germany and adjacent areas to calculate the slip tendency for three 3D fault geometry sets with increasing complexity. This allows to draw general conclusions about the influence of the fault geometry on the reactivation potential.
In general, the fault reactivation potential is higher in Germany for faults that strike NW-SE and NNE-SSW. Due to the prevailing normal stress regime in the geomechanical-numerical model results, faults dipping at an angle of about 60° generally show higher slip tendencies in comparison to steeper or shallower dipping faults. Faults implemented with a straight geometry show higher slip tendencies than those represented with a more complex, uneven geometry. Pore pressure has been assumed as hydrostatic and has shown to have a major influence on the calculated slip tendencies. Compared to slip tendency values calculated without pore pressure, the consideration of pore pressure leads to an increase of slip tendency of up to 50 %. The qualitative comparison of the slip tendency with the occurrence of seismic events with moment magnitudes Mw > 3.5 shows an overall good spatial correlation between areas of elevated slip tendencies and seismic activity for one of the investigated fault sets.
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
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Journal article(s) based on this preprint
Interactive discussion
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RC1: 'Comment on egusphere-2022-26', David Ferrill, 06 Apr 2022
Review of “The analysis of slip tendency of major tectonic faults in Germany” by Luisa Röckel, Steffen Ahlers, Birgit Müller, Karsten Reiter, Oliver Heidbach, Andreas Henk, Tobias Hergert, Frank Schilling.
Review by David A. Ferrill
GENERAL
The manuscript provides new slip tendency analyses to constrain the potential for fault activity in Germany, which is important for assessing seismic hazard as well as other fault related processes such as energy extraction and subsurface disposal or storage activities. This is a very interesting manuscript – the material should be of interest to a broad readership, and make a very nice contribution to Solid Earth.
My greatest concern with the article is that, for the article to stand alone and be easily understood, it needs to illustrate the regional stress field and provide representative slip tendency plots. Lacking this information, the slip tendency fault maps are difficult to understand and the related description is rather abstract.
A second concern is related to the justification for the assumption of a vertical fault set. This vertical-fault assumption needs to be (i) justified by providing the geological basis for assuming the faults are vertical, or (ii) explained with appropriate caveats provided regarding impacts of an incorrect assumption on slip tendency results for the stress fields of Germany.
Below are several specific comments and suggestions that could help improve the manuscript. Additional editorial comments are marked in an annotated pdf that will also be provided with this review.
SPECIFIC COMMENTS
Description and illustration of stress states and slip tendency plots for study area (Section 2.1, 3D Stress State):
What are the stress regimes in Germany? This section should summarize the stress state of the study area in terms of stress regimes (e.g., normal faulting, strike-slip faulting, thrust faulting), maximum horizontal stress directions, and variation as a function of depth. In present form, the paper relies on Ahlers et al. (2021), and discusses the stress analysis methodology of Ahlers et al. (2021) but not the result of that analysis which is a primary input for the slip tendency analysis in this paper.
The manuscript would be greatly improved by illustrating the stress states by providing a map with representative slip tendency plots for subregions. Specifically, I recommend a map similar to figure 7 in Morris et al. (2021). Such a map would convey not only stress orientations, but also stress regime (cf. figure 1 in Morris and Ferrill, 2009, The importance of the intermediate principal effective stress (σ'2) to fault slip patterns. Journal of Structural Geology 31, 950-959). Because of the variation in regime as a function of depth indicated by figure 11 of Ahlers et al. (2021, Solid Earth), it may be necessary to provide maps with representative slip tendency plots at two depths.
Assumption of “Vertical fault set” (Section 2.2):
Is there a technical basis for the “vertical” assumption, or is this just a matter of convenience? This assumption has major impact on slip tendency, and results are highly sensitive to stress regime. Please provide (i) a geological basis for assuming the faults are vertical rather than some other dip angle, and/or (ii) a rationale for making the assumption, with acknowledgement that -- if wrong -- this assumption can introduce large error in slip tendency calculation. Vertical faults may be ideally oriented for slip in a strike-slip stress regime, whereas vertical faults are never ideally oriented for slip in normal faulting or thrust (reverse) faulting Andersonian stress regimes. Therefore, the vertical-fault assumption will tend to skew slip tendencies lower values for stress regimes other than strike-slip regime.
Results Section 3.1 – Vertical fault set:
Manuscript states that “Results near surface are visualized” (Line 115): What depth, and why near surface? Earthquakes tend to nucleate at significant depth rather than near the surface.
As noted earlier, if not correct, the vertical fault assumption is problematic and may artificially skew slip tendencies lower for stress regimes other than strike-slip regime where vertical faults are ideally oriented for slip. It would be good to acknowledge this in this results section
Subscripting for slip tendency symbols:
In all figures and throughout article, need to be consistent with subscripting of Ts, Tsnorm, Tseff, and Tsnormeff for consistency with text.
Referencing:
Although cited in the text, Morris et al. (1996) is missing from the reference list:
- Morris, A.P., Ferrill, D.A., Henderson, D.B., 1996. Slip tendency analysis and fault reactivation. Geology 24, 275–278.
Recommend citing the following paper in the Introduction (Line 41) as a very careful example of regional slip tendency analysis of 3D faults:
- Morris A.P., Hennings, P.H., Horne E.A., Smye, K.M., 2021. Stability of basement-rooted faults in the Delaware Basin of Texas and New Mexico, USA. Journal of Structural Geology 149, 104360.
- AC1: 'Reply on RC1', Luisa Röckel, 18 May 2022
-
RC2: 'Review of “The analysis of slip tendency of major tectonic faults in Germany” by Röckel et al.', Stephen Hicks, 12 Apr 2022
Review of “The analysis of slip tendency of major tectonic faults in Germany” by Röckel et al.
Stephen Hicks, Imperial College London
(1) Overview of the manuscript
RoÌckel et al. provide a detailed analysis of slip tendency for mapped faults in Germany using a variety of subsurface datasets. Although local slip tendency studies exist for Germany (e.g., Northeast German Basin - Moeck et al., 2009, J. Struct. Geol.; Roer Valley Rift - Worum et al., 2004, J. Geophys. Res.), this manuscript presents the first national-scale attempt to my knowledge. The computed slip tendency values are based on regional stress tensor information from an already-published 3D numerical geomechanical model (Ahlers et al., 2021). The main findings from this study are that (1) roughly northwest-southeast striking faults have a higher slip tendency in the regional stress field, and (2) there is a reported good spatial correlation between higher slip tendency and seismicity. I congratulate the authors for writing a manuscript with well-grounded objectives and sound, well-described methods. It is refreshing to see these vital fault analyses considered over a large regional scale. The manuscript is detailed, easy to follow, and well-written. Although the methods, data and results appear sound, I have two moderate-to-minor level comments on the comparison with seismicity and the presentation of the regional tectonic context, as detailed below.
I look forward to seeing this excellent work appearing in print soon!
(2) General comments
(2-a) Regional tectonic context and past studies on slip tendency
Although the Introduction reads very well, I feel that it could be improved by including a better description regional tectonic/geological context, especially for a reader who is not familiar with the geology of Germany (like me). Specifically, what are the broad spatial patterns in the regional stress of Germany? What are the main fault structures? What is known about seismicity in Germany and the types of faults that get reactivated? How much of the seismicity in Germany is induced, and what might be the role of high pore fluid pressures in some of these cases? In particular, I feel the article could benefit from having a new figure that comes before all existing figures to present a regional map that highlights and labels specific regions of interest mentioned in the Introduction and throughout the paper (e.g., Roer Graben, Upper Rhine Graben). This map should also show how the stress regime varies across Germany (e.g., by showing indicative SHmax orientations and stress regimes).
Whilst localised slip tendency studies in Germany have been cited (e.g., Moeck et al., 2009; Worum et al., 2004), it would be helpful to compare the results of these studies with the new slip tendency data from this manuscript.
(2-b) Comparison with seismicity
I am not yet entirely convinced by the comparison between slip tendency and seismicity, which is described in Section 4.5 and illustrated in Figure 11, one of the main conclusions of this study. This concern arises for several reasons, which I describe below, and I try to provide some hopefully helpful suggestions to improve confidence in this conclusion.
(2-b-i) The seismicity catalogue used
Slip tendency is compared with earthquakes based on the GruÌnthal und WahlstroÌm (2012) seismicity catalogue. This catalogue runs until 2006, and locations of the more historical earthquakes are likely to be inaccurate, so I wonder whether this dataset could at least be supplemented with additional earthquakes since 2006 using modern operational catalogues (e.g., EMSC; GFZ-GEOFON; BGR)? Widening the earthquake dataset may help produce more confident correlations with slip tendency. Perhaps if one of these instrumental catalogues were considered on their own, then a lower magnitude threshold could be used, e.g., Mw 2.5-3.0?
(2-b-ii) Comparing small earthquakes and large faults
Given that the best correlation between seismicity and slip tendency is reported for the Andersonian fault dataset, I am curious about the rationale behind selecting a minimum fault length of 250 km for this dataset? Earthquakes down to Mw 3.5 are considered in this analysis, but earthquakes this small would typically rupture a fault length down to tens of metres (e.g., by extrapolating earthquake scaling relations of (Wells & Coppersmith, 1994) rather than hundreds of kilometres. Earthquakes in Germany do not typically exceed Mw~5. So I wonder whether some of the small earthquakes may occur on more minor faults than currently considered and that may have an orientation not represented by the larger-scale faults. I realise that it is challenging to map every minor fault. Still, I would like to see how the reported slip tendency - seismicity correlation holds up if a more diverse fault dataset encompassing smaller-length faults (e.g., tens of km) is considered instead?
(2-b-iii) Associating earthquakes with faults
As mentioned above, the premise of the reported correlation relies on the implicit assumption that earthquakes are associated with either one of the fault structures considered or a minor fault whose orientation is represented by larger structures. I, therefore, wonder whether any focal mechanism data exists for Germany, from either operational catalogues or existing published studies, that can be used to state whether one of the nodal planes is parallel to the implicitly identified causative fault? I realise that focal mechanism data may be reasonably sparse for an aseismic region like Germany. Yet a quick look at the GFZ-GEOFON catalogue yields a handful of moment tensors for the study area, which could still at least be briefly presented and discussed. But perhaps there are more detailed focal mechanism datasets from local studies across Germany?
(2-b-iv) Presentation of the seismicity – slip tendency correlation
By visually looking at Figure 11, I am not entirely convinced that a spatial correlation exists, so it would be good to quantify the correlation numerically. One idea to consider is to discretise the study area into a grid. Then assign each grid point where a fault and associated slip tendency value exists to its average and/or maximum value and a seismicity parameter (e.g., log of total seismic moment, number of earthquakes, a binary choice of earthquake occurrence within x km radius). This approach would then allow a scatter plot of points to be shown with an associated correlation coefficient value.
(3) Specific, minor comments
(3a) In Figure 2, I find it hard to work out the dip direction of the fault. Could a solid line be possibly added to the fault surface to show the reader where the top of the fault is?
(3b) For Figure 3, the locations of these vertical sections should ideally be shown on a map somewhere – either a previous map or a sub-panel of this figure. Also, the horizontal and vertical scales could benefit from fully labelled axes with a greater frequency of labels and ticks.
(3c) Figure 8 – even though it is implicitly shown in the axis orientation sketch, the caption should also clarify that the map in (a) is from an oblique/perspective viewpoint.
(4) Technical comments
(4a) Line 161 – possibly a word or punctuation missing between “fault set” and “additional histograms”. Maybe a “, with” is needed here?
Citation: https://doi.org/10.5194/egusphere-2022-26-RC2 - AC2: 'Reply on RC2', Luisa Röckel, 18 May 2022
Interactive discussion
Status: closed
-
RC1: 'Comment on egusphere-2022-26', David Ferrill, 06 Apr 2022
Review of “The analysis of slip tendency of major tectonic faults in Germany” by Luisa Röckel, Steffen Ahlers, Birgit Müller, Karsten Reiter, Oliver Heidbach, Andreas Henk, Tobias Hergert, Frank Schilling.
Review by David A. Ferrill
GENERAL
The manuscript provides new slip tendency analyses to constrain the potential for fault activity in Germany, which is important for assessing seismic hazard as well as other fault related processes such as energy extraction and subsurface disposal or storage activities. This is a very interesting manuscript – the material should be of interest to a broad readership, and make a very nice contribution to Solid Earth.
My greatest concern with the article is that, for the article to stand alone and be easily understood, it needs to illustrate the regional stress field and provide representative slip tendency plots. Lacking this information, the slip tendency fault maps are difficult to understand and the related description is rather abstract.
A second concern is related to the justification for the assumption of a vertical fault set. This vertical-fault assumption needs to be (i) justified by providing the geological basis for assuming the faults are vertical, or (ii) explained with appropriate caveats provided regarding impacts of an incorrect assumption on slip tendency results for the stress fields of Germany.
Below are several specific comments and suggestions that could help improve the manuscript. Additional editorial comments are marked in an annotated pdf that will also be provided with this review.
SPECIFIC COMMENTS
Description and illustration of stress states and slip tendency plots for study area (Section 2.1, 3D Stress State):
What are the stress regimes in Germany? This section should summarize the stress state of the study area in terms of stress regimes (e.g., normal faulting, strike-slip faulting, thrust faulting), maximum horizontal stress directions, and variation as a function of depth. In present form, the paper relies on Ahlers et al. (2021), and discusses the stress analysis methodology of Ahlers et al. (2021) but not the result of that analysis which is a primary input for the slip tendency analysis in this paper.
The manuscript would be greatly improved by illustrating the stress states by providing a map with representative slip tendency plots for subregions. Specifically, I recommend a map similar to figure 7 in Morris et al. (2021). Such a map would convey not only stress orientations, but also stress regime (cf. figure 1 in Morris and Ferrill, 2009, The importance of the intermediate principal effective stress (σ'2) to fault slip patterns. Journal of Structural Geology 31, 950-959). Because of the variation in regime as a function of depth indicated by figure 11 of Ahlers et al. (2021, Solid Earth), it may be necessary to provide maps with representative slip tendency plots at two depths.
Assumption of “Vertical fault set” (Section 2.2):
Is there a technical basis for the “vertical” assumption, or is this just a matter of convenience? This assumption has major impact on slip tendency, and results are highly sensitive to stress regime. Please provide (i) a geological basis for assuming the faults are vertical rather than some other dip angle, and/or (ii) a rationale for making the assumption, with acknowledgement that -- if wrong -- this assumption can introduce large error in slip tendency calculation. Vertical faults may be ideally oriented for slip in a strike-slip stress regime, whereas vertical faults are never ideally oriented for slip in normal faulting or thrust (reverse) faulting Andersonian stress regimes. Therefore, the vertical-fault assumption will tend to skew slip tendencies lower values for stress regimes other than strike-slip regime.
Results Section 3.1 – Vertical fault set:
Manuscript states that “Results near surface are visualized” (Line 115): What depth, and why near surface? Earthquakes tend to nucleate at significant depth rather than near the surface.
As noted earlier, if not correct, the vertical fault assumption is problematic and may artificially skew slip tendencies lower for stress regimes other than strike-slip regime where vertical faults are ideally oriented for slip. It would be good to acknowledge this in this results section
Subscripting for slip tendency symbols:
In all figures and throughout article, need to be consistent with subscripting of Ts, Tsnorm, Tseff, and Tsnormeff for consistency with text.
Referencing:
Although cited in the text, Morris et al. (1996) is missing from the reference list:
- Morris, A.P., Ferrill, D.A., Henderson, D.B., 1996. Slip tendency analysis and fault reactivation. Geology 24, 275–278.
Recommend citing the following paper in the Introduction (Line 41) as a very careful example of regional slip tendency analysis of 3D faults:
- Morris A.P., Hennings, P.H., Horne E.A., Smye, K.M., 2021. Stability of basement-rooted faults in the Delaware Basin of Texas and New Mexico, USA. Journal of Structural Geology 149, 104360.
- AC1: 'Reply on RC1', Luisa Röckel, 18 May 2022
-
RC2: 'Review of “The analysis of slip tendency of major tectonic faults in Germany” by Röckel et al.', Stephen Hicks, 12 Apr 2022
Review of “The analysis of slip tendency of major tectonic faults in Germany” by Röckel et al.
Stephen Hicks, Imperial College London
(1) Overview of the manuscript
RoÌckel et al. provide a detailed analysis of slip tendency for mapped faults in Germany using a variety of subsurface datasets. Although local slip tendency studies exist for Germany (e.g., Northeast German Basin - Moeck et al., 2009, J. Struct. Geol.; Roer Valley Rift - Worum et al., 2004, J. Geophys. Res.), this manuscript presents the first national-scale attempt to my knowledge. The computed slip tendency values are based on regional stress tensor information from an already-published 3D numerical geomechanical model (Ahlers et al., 2021). The main findings from this study are that (1) roughly northwest-southeast striking faults have a higher slip tendency in the regional stress field, and (2) there is a reported good spatial correlation between higher slip tendency and seismicity. I congratulate the authors for writing a manuscript with well-grounded objectives and sound, well-described methods. It is refreshing to see these vital fault analyses considered over a large regional scale. The manuscript is detailed, easy to follow, and well-written. Although the methods, data and results appear sound, I have two moderate-to-minor level comments on the comparison with seismicity and the presentation of the regional tectonic context, as detailed below.
I look forward to seeing this excellent work appearing in print soon!
(2) General comments
(2-a) Regional tectonic context and past studies on slip tendency
Although the Introduction reads very well, I feel that it could be improved by including a better description regional tectonic/geological context, especially for a reader who is not familiar with the geology of Germany (like me). Specifically, what are the broad spatial patterns in the regional stress of Germany? What are the main fault structures? What is known about seismicity in Germany and the types of faults that get reactivated? How much of the seismicity in Germany is induced, and what might be the role of high pore fluid pressures in some of these cases? In particular, I feel the article could benefit from having a new figure that comes before all existing figures to present a regional map that highlights and labels specific regions of interest mentioned in the Introduction and throughout the paper (e.g., Roer Graben, Upper Rhine Graben). This map should also show how the stress regime varies across Germany (e.g., by showing indicative SHmax orientations and stress regimes).
Whilst localised slip tendency studies in Germany have been cited (e.g., Moeck et al., 2009; Worum et al., 2004), it would be helpful to compare the results of these studies with the new slip tendency data from this manuscript.
(2-b) Comparison with seismicity
I am not yet entirely convinced by the comparison between slip tendency and seismicity, which is described in Section 4.5 and illustrated in Figure 11, one of the main conclusions of this study. This concern arises for several reasons, which I describe below, and I try to provide some hopefully helpful suggestions to improve confidence in this conclusion.
(2-b-i) The seismicity catalogue used
Slip tendency is compared with earthquakes based on the GruÌnthal und WahlstroÌm (2012) seismicity catalogue. This catalogue runs until 2006, and locations of the more historical earthquakes are likely to be inaccurate, so I wonder whether this dataset could at least be supplemented with additional earthquakes since 2006 using modern operational catalogues (e.g., EMSC; GFZ-GEOFON; BGR)? Widening the earthquake dataset may help produce more confident correlations with slip tendency. Perhaps if one of these instrumental catalogues were considered on their own, then a lower magnitude threshold could be used, e.g., Mw 2.5-3.0?
(2-b-ii) Comparing small earthquakes and large faults
Given that the best correlation between seismicity and slip tendency is reported for the Andersonian fault dataset, I am curious about the rationale behind selecting a minimum fault length of 250 km for this dataset? Earthquakes down to Mw 3.5 are considered in this analysis, but earthquakes this small would typically rupture a fault length down to tens of metres (e.g., by extrapolating earthquake scaling relations of (Wells & Coppersmith, 1994) rather than hundreds of kilometres. Earthquakes in Germany do not typically exceed Mw~5. So I wonder whether some of the small earthquakes may occur on more minor faults than currently considered and that may have an orientation not represented by the larger-scale faults. I realise that it is challenging to map every minor fault. Still, I would like to see how the reported slip tendency - seismicity correlation holds up if a more diverse fault dataset encompassing smaller-length faults (e.g., tens of km) is considered instead?
(2-b-iii) Associating earthquakes with faults
As mentioned above, the premise of the reported correlation relies on the implicit assumption that earthquakes are associated with either one of the fault structures considered or a minor fault whose orientation is represented by larger structures. I, therefore, wonder whether any focal mechanism data exists for Germany, from either operational catalogues or existing published studies, that can be used to state whether one of the nodal planes is parallel to the implicitly identified causative fault? I realise that focal mechanism data may be reasonably sparse for an aseismic region like Germany. Yet a quick look at the GFZ-GEOFON catalogue yields a handful of moment tensors for the study area, which could still at least be briefly presented and discussed. But perhaps there are more detailed focal mechanism datasets from local studies across Germany?
(2-b-iv) Presentation of the seismicity – slip tendency correlation
By visually looking at Figure 11, I am not entirely convinced that a spatial correlation exists, so it would be good to quantify the correlation numerically. One idea to consider is to discretise the study area into a grid. Then assign each grid point where a fault and associated slip tendency value exists to its average and/or maximum value and a seismicity parameter (e.g., log of total seismic moment, number of earthquakes, a binary choice of earthquake occurrence within x km radius). This approach would then allow a scatter plot of points to be shown with an associated correlation coefficient value.
(3) Specific, minor comments
(3a) In Figure 2, I find it hard to work out the dip direction of the fault. Could a solid line be possibly added to the fault surface to show the reader where the top of the fault is?
(3b) For Figure 3, the locations of these vertical sections should ideally be shown on a map somewhere – either a previous map or a sub-panel of this figure. Also, the horizontal and vertical scales could benefit from fully labelled axes with a greater frequency of labels and ticks.
(3c) Figure 8 – even though it is implicitly shown in the axis orientation sketch, the caption should also clarify that the map in (a) is from an oblique/perspective viewpoint.
(4) Technical comments
(4a) Line 161 – possibly a word or punctuation missing between “fault set” and “additional histograms”. Maybe a “, with” is needed here?
Citation: https://doi.org/10.5194/egusphere-2022-26-RC2 - AC2: 'Reply on RC2', Luisa Röckel, 18 May 2022
Peer review completion
Journal article(s) based on this preprint
Data sets
3D fault sets of Germany and adjacent areas Röckel, Luisa; Müller, Birgit I. R.; Ahlers, Steffen; Reiter, Karsten; Hergert, Tobias; Henk, Andreas; Heidbach, Oliver; Schilling, Frank https://bwdatadiss.kit.edu/dataset/415
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Steffen Ahlers
Birgit Müller
Karsten Reiter
Oliver Heidbach
Andreas Henk
Tobias Hergert
Frank Schilling
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
(2506 KB) - Metadata XML
-
Supplement
(2148 KB) - BibTeX
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- Final revised paper