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Shear vs. non-shear components in source mechanisms of microearthquakes induced in hydraulic fracturing experiment at the HDR site Soultz-sous-Forets (Alsace) in 2003
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SYSNO ASEP 0315223 Document Type C - Proceedings Paper (int. conf.) R&D Document Type Conference Paper Title Shear vs. non-shear components in source mechanisms of microearthquakes induced in hydraulic fracturing experiment at the HDR site Soultz-sous-Forets (Alsace) in 2003 Title Střižné versus nestřižné složky zdrojových mechanizmů mikrozemětřesení indukovaných při experimentu hydraulického rozrušování v geotermální oblasti (HDR) Soultz-sous-Forets (Alsasko) v roce 2003 Author(s) Horálek, Josef (GFU-E) ORCID, RID
Jechumtálová, Zuzana (GFU-E) ORCID, RID
Dorbath, L. (FR)
Šílený, Jan (GFU-E) ORCID, RIDSource Title EHDRA scientific conference proceedings. - Soultz-sous-Forets : EHDRA, 2008 Pages s. 1-8 Number of pages 8 s. Action EHDRA scientific conference Event date 24.09.2008-25.09.2008 VEvent location Soultz-sous-Forets Country FR - France Event type EUR Language eng - English Country FR - France Keywords moment tensor ; source mechanisms ; microearthquakes Subject RIV DC - Siesmology, Volcanology, Earth Structure CEZ AV0Z30120515 - GFU-E (2005-2011) Annotation Moment tensor formalism replaced fault-plane solution in contemporary seismology and has become a standard for description of seismic source, both of natural origin and induced by man-made activity. Thanks to that, the question of double-couple (DC) vs. non-DC mechanism of a seismic source became urgent. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2009
Number of the records: 1