Deutsch
 
Datenschutzhinweis Impressum
  DetailsucheBrowse

Datensatz

DATENSATZ AKTIONENEXPORT

Freigegeben

Zeitschriftenartikel

The 2004 Mw 4.4 Rotenburg, Northern Germany, Earthquake and its possible relationship with Gas Recovery

Urheber*innen
/persons/resource/dahm

Dahm,  Torsten
Deutsches GeoForschungsZentrum;

Krüger,  F.
External Organizations;

Stammler,  K.
External Organizations;

Klinge,  K.
External Organizations;

/persons/resource/kind

Kind,  Rainer
2.4 Seismology, 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Wylegalla,  K.
External Organizations;

Grasso,  J.-R.
External Organizations;

Externe Ressourcen
Es sind keine externen Ressourcen hinterlegt
Volltexte (frei zugänglich)
Es sind keine frei zugänglichen Volltexte in GFZpublic verfügbar
Ergänzendes Material (frei zugänglich)
Es sind keine frei zugänglichen Ergänzenden Materialien verfügbar
Zitation

Dahm, T., Krüger, F., Stammler, K., Klinge, K., Kind, R., Wylegalla, K., Grasso, J.-R. (2007): The 2004 Mw 4.4 Rotenburg, Northern Germany, Earthquake and its possible relationship with Gas Recovery. - Bulletin of the Seismological Society of America, 97, 3, 691-704.
https://doi.org/10.1785/0120050149


https://gfzpublic.gfz-potsdam.de/pubman/item/item_235817
Zusammenfassung
We study the 20 October 2004 Mw 4.4 Rotenburg (Wümme)/Neuenkirchen earthquake, located in a previously aseismic region in the northern German sedimentary basin. We constrain the source parameter by using different techniques. A possible relationship between this event, the regional tectonic setting, and local gas recovery is investigated. Different waveform in version and modelling approaches constrain the depth of the mainshock between 5 and 7 km. The source mechanism was oblique normal faulting on planes striking roughly north-south. An inversion for kinematics rupture parameters indicates a unilateral rupture propagation toward the north, consistent with the higher macroseismic intensities found toward the north in the region of Hamburg compared with those at a similar distance toward the south in the region of Hannover. Relocations of the mainshock and three of the largest aftershocks indicate that these events occurred within a few kilometres of three major gas fields and at depth close to gas production intervals. Comparison with seismicity triggered in the northern Netherlands by depletion of similar gas reservoirs in a similar tectonic environment suggests that the Mw 4.4 Rotenburg event may be related to gas recovery.