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An earthquake catalogue for central, northern and northwestern Europe based on Mw magnitudes

Authors
/persons/resource/ggrue

Grünthal,  Gottfried
2.6 Seismic Hazard and Stress Field , 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;
Scientific Technical Report STR, Deutsches GeoForschungsZentrum;

/persons/resource/rutger

Wahlström,  Rutger
2.6 Seismic Hazard and Stress Field , 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;
Scientific Technical Report STR, Deutsches GeoForschungsZentrum;

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Fulltext (public)

0302.pdf
(Publisher version), 8MB

Supplementary Material (public)

0302_annex.pdf
(Supplementary material), 415KB

Citation

Grünthal, G., Wahlström, R. (2003): An earthquake catalogue for central, northern and northwestern Europe based on Mw magnitudes, (Scientific Technical Report STR ; 03/02), Potsdam : Deutsches GeoForschungsZentrum GFZ, 143 p.
https://doi.org/10.2312/GFZ.b103-030104


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_8599
Abstract
A Databank was created using data from 25 local catalogues and 30 special studies of earthquakes in central, northern and northwestern Europe. Event types were discriminated, fake events and duplets eliminated, and different magnitudes and intensities converted to Mw. The conversions require the establishment of regression equations. The Catalogue contains tectonic events from the Databank within the area 44°N-72°N, 25°W-32°E and the time period 1300-1993 which have Mw magnitudes of 3.50 and larger. The area is covered by different polygons. Within each polygon only data from one or a small number of the local catalogues, supplemented by data from special studies, enter the Catalogue. If there are two or more such catalogues or studies providing a solution for an event, a priority algorithm selects one entry for the Catalogue. Then Mw is calculated from one of the magnitude types, or from macroseismic data, given by the selected entry according to another priority scheme. The origin time, location, Mw magnitude and reference are specified for each entry of the Catalogue. So is the epicentral intensity, I0, if provided by the original source. Following these criteria, a total of about 5,000 earthquakes constitute the Catalogue. Although originally derived for the purpose of seismic hazard calculation within GSHAP, the Catalogue provides a data base for many types of seismicity and seismic hazard studies.