Abstract
The potential and limits of monitoring induced seismicity by surface-based mini arrays was evaluated for the hydraulic stimulation of the Basel Deep Heat Mining Project. This project aimed at the exploitation of geothermal heat from a depth of about 4,630 m. As reference for our results, a network of borehole stations by Geothermal Explorers Ltd. provided ground truth information. We utilized array processing, sonogram event detection and outlier-resistant, graphical jackknife location procedures to compensate for the decrease in signal-to-noise ratio at the surface. We could correctly resolve the NNW–SSE striking fault plane by relative master event locations. Statistical analysis of our catalog data resulted in M L 0.36 as completeness magnitude, but with significant day-to-night dependency. To compare to the performance of borehole data with M W 0.9 as completeness magnitude, we applied two methods for converting M L to M W which raised our M C to M W in the range of 0.99–1.13. Further, the b value for the duration of our measurement was calculated to 1.14 (related to M L), respectively 1.66 (related to M W), but changes over time could not be resolved from the error bars.
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References
Bachmann CE, Wiemer S, Woessner J, Hainzl S (2011) Statistical analysis of the induced Basel 2006 earthquake sequence: introducing a probability-based monitoring approach for Enhanced Geothermal Systems. Geophys J Int 186. doi:10.1111/j.1365-246X.2011.05068.x
Bethmann F, Deichmann N, Mai PM (2011) Scaling relations of local magnitude versus moment magnitude for sequences of similar earthquakes in Switzerland. Bull Seism Soc Am 101(2):515–534
Deichmann N, Giardini D (2009) Earthquakes induced by the stimulation of an enhanced geothermal system below Basel (Switzerland). Seismo Res Lett 80:784–798
Dyer BC, Schanz U, Spillmann T, Ladner F, Häring MO (2010) Application of microseismic multiplet analysis to the Basel geothermal reservoir stimulation events. Geophys Prosp 58:791–807
Fäh D, Giardini D, Bay F, Bernardi F, Braunmiller J, Deichmann N, Furrer M, Gantner L, Gisler M, Isenegger D, Jimenez MJ, Kästli P, Koglin R, Masciadri V, Rutz M, Scheidegger C, Schibler R, Schorlemmer D, Schwarz-Zanetti G, Steimen S, Sellami S, Wiemer S, Wössner J (2003) Earthquake Catalogue of Switzerland (ECOS) and the related macroseismic database. Eclogae Geol Helv 96:219–236
Fäh D, Giardini D, Kästli P, Deichmann N, Gisler M, Schwarz-Zanetti G, Alvarez-Rubio S, Sellami S, Edwards B, Allmann B, Bethmann F, Wössner J, Gassner-Stamm G, Fritsche S, Eberhard D (2011) ECOS-09 Earthquake Catalogue of Switzerland release 2011 report and database. Public catalogue, 17.4.2011. Swiss Seismological Service ETH Zurich, report SED/RISK/R/001/20110417
Gutenberg B, Richter CF (1944) Frequency of earthquakes in California. Bull Seismol Soc Am 34:185–188
Häge M, Joswig M (2009a) Spatiotemporal distribution of aftershocks of the 2004 December 5 M L = 5.4 Waldkirch (Germany) earthquake. Geophys J Int 178:1523–1532
Häge M, Joswig M (2009b) Mapping local microseismicity using short-term tripartite small array installations—case study: Coy region (SE Spain). Tectonophys 471:225–231
Häge M, Joswig M (2011) Untersuchung der Lokalisierungsgenauigkeit von Kleinarrays anhand induzierter Seismizität während der Stimulationsphase des Deep-Heat-Mining-Projektes in Basel. DGG Mitteilungen 1:24–30
Häring MO, Schanz U, Ladner F, Dyer BC (2008) Characterisation of the Basel 1 enhanced geothermal system. Geothermics 37:469–495
Husen S, Kissling E, Deichmann N, Wiemer S, Giardini D, Baer M (2003) Probabilistic earthquake location in complex three-dimensional velocity models: application to Switzerland. J Geophys Res 108(B2):2077
Illies J (1972) The Rhine graben rift system-plate tectonics and transform faulting. Surv Geophys 1:27–60
Ishimoto M, Iida K (1939) Observation of earthquakes registered with the microseismograph constructed recently. Bull Earthq Res Inst Univ Tokyo 17:443–478
Joswig M (1990) Pattern recognition for earthquake detection. Bull Seismol Soc Am 80:170–186
Joswig M (1995) Automated classification of the local earthquake data in the BUG small array. Geophys J Int 120:262–286
Joswig M (2008) Nanoseismic monitoring fills the gap between microseismic networks and passive seismic. First Break 26:121–128
Kahn D (2008) Hydro-fractured reservoirs: a study using double-difference location Techniques. Dissertation, Duke University
Labak P, Villagran M, Haege M (2009) Seismic aftershock monitoring during an OSI—experience and results from Field Exercise in Kazakhstan. OSI-05/B, International Scientific Studies Conference, Vienna, Austria
Pirli M, Voulgaris N, Chira A, Makropoulos K (2007) The March 2004 Kalamata seismic sequence: a case of efficient seismicity monitoring in the area of Peloponnese, southern Greece, by the Tripoli Seismic Array. J Seismol 11:59–72
Tester JW, Anderson BJ, Batchelor AS, Blackwell DD, DiPippo R, Drake EM, Garnish J, Livesay B, Moore MC, Nichols K, Petty S, Toksoz MN, Veatch RW, Baria R, Augustine C, Murphy E, Negraru P, Richards M (2007) Impact of enhanced geothermal systems on US energy supply in the twenty-first century. Phil Trans R Soc A 365:1057–1094
Ustaszewski K, Schmid SM (2007) Latest Pliocene to recent thick-skinned tectonics at the Upper Rhine Graben—Jura Mountains junction. Swiss J Geosci 100:293–312
Valley B, Evans KF (2009) Stress orientation to 5 km depth in the basement below Basel (Switzerland) from borehole failure analysis. Swiss J Geosci 102(3):467–480
Wiemer S (2001) A software package to analyse seismicity: ZMAP. Seismol Res Lett 72(2):374–383
Woessner J, Wiemer S (2005) Assessing the quality of earthquake catalogs: estimating the magnitude of completeness and its uncertainty. Bull Seismol Soc Am 95(2):684–698
Wust-Bloch GH, Joswig M (2006) Pre-collapse identification of sinkholes in unconsolidated media at Dead Sea area by ‘nanoseismic monitoring’ (graphical jackknife location of weak sources by few, low-SNR records). Geophys J Int 167:1220–1232
Acknowledgments
The authors would like to thank Nicolas Deichmann and Dan Kahn for providing their results. We also thank Gregor Mokelke for assisting in data analysis. Marco Walter is acknowledged for field assistance. Guest editor S. Cesca and two anonymous reviewers are acknowledged for critical and useful comments which improved the paper. Figures 1, 3 and 4 have been published in similar form in Häge and Joswig (2011).
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Häge, M., Blascheck, P. & Joswig, M. EGS hydraulic stimulation monitoring by surface arrays - location accuracy and completeness magnitude: the Basel Deep Heat Mining Project case study. J Seismol 17, 51–61 (2013). https://doi.org/10.1007/s10950-012-9312-9
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DOI: https://doi.org/10.1007/s10950-012-9312-9