Faulting style and stress field investigations for swarm earthquakes in NE Baveria/Germany – the transition between Vogtland/NW-Bohemia and the KTB-site
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s10950-005-9008-5.pdf
Reference33 articles.
1. Bohnhoff, M., Baisch, S. and Harjes, H., 2004. Fault mechanisms of induced seismicity at the superdeep German Continental Deep Drilling Program (KTB) borehole and their relation to fault structure and stress field. J. Geophys. Res., 109, B02309, doi:10.1029/2003JB002528.
2. Brudy, M., Zoback, M.D., Fuchs, K., Rummel F., and Baumgärtner, J., 1997. Estimation of the complete stress tensor to 8 km depth in the KTB scientific drill holes: Implications for crustal strength. J. Geophys. Res., 102, No. B8, 453–476.
3. Chen, W-P. and Molnar, P., 1983. Focal depths of intracontinental and intraplate earthquakes and their implications for the thermal and mechanical properties of the lithosphere. J. Geophys. Res. astr. Soc. 88, 4183–4214.
4. Dahlheim, H.-A., Gebrande, H., Schmedes E., and Soffel, H., 1997. Seismicity and stress field in the vicinity of the KTB location, J. Geophys. Res. 102, 18493–18506.
5. Dahm, T., Horálek, J., and Šíleny, J., 2000. Comparison of absolute and relative moment tensor solutions for the January 1997 West Bohemia earthquake swarm. Studia geoph. et geod., 44, 233–250.
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5. Reply to comment of T. Fischer and J. Horálek on “Geodynamic pattern of the West Bohemia region based on permanent GPS measurements” by V. Schenk, Z. Schenková and Z. Jechumtálová;Studia Geophysica et Geodaetica;2009-07
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