New manual of seismological observatory practice (NMSOP)
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Examination of the Storfjorden aftershock sequence. The Storfjorden, Svalbard, aftershock sequence: Seismotectonics in a polar environment. IS PD Emil Wiechert — Mitteilungen der Deutschen Geophysikalischen Gesellschaft. Continent-ocean-transition across a trans-tensional margin segment: off Bear Island, Barents Sea. Modelling of seafloor multiples observed in OBS data from the North Atlantic - new seismic tool for oceanography?.
Polish Polar Research. A probabilistic seismic model for the European Arctic.
Journal of Geophysical Research - Solid Earth. Application of array-based waveform cross-correlation techniques to aftershock sequences: the Lefkada Island, Greece, case. Spatial noise-field characteristics of a three-component small aperture test array in central Italy. An empirical procedure for rapid magnitude estimation in Italy.
Publications | IASPEI
Comparison of location procedures: The Kara Sea event of 16 August Crustal root beneath the highlands of southern Norway resolved by teleseismic receiver functions. How can the ISC location procedures be improved?. Physics of the Earth and Planetary Interiors. Results from the temporary installation of a small aperture seismic array in the Central Apennines and its merits for local event detection and location capabilities.
Annals of Geophysics.
Dahm, Torsten; Hainzl, S. Predicting size and occurrence time of coseismic rupture using a single fault stick slip model: examples from the Fimbul ice shelf, Antarctica. Geophysical Research Abstracts.
Rebuild of the Bulletin of the International Seismological Centre (ISC), part 1: 1964–1979
Location and depth estimation of the North Sea earthquake 30 June On 11 February , Prof. Peter Bormann passed away at the age of 75 after a period of serious illness. We have lost not only a precious colleague and friend but also an outstanding geoscientist. With all his strength and personality, he had dedicated his professional life to seismology, has made significant research contributions in this field, rendered excellent services to the international bodies and the scientific community and has trained young seismologists from all over the world.
We know Peter as someone who always walked through life with keen eyes and made interesting discoveries in many areas of life. Far beyond seismology, he also took an interest in other fields of science, in literature, art, photography and last not least in people. After two years of interim work at the United Nations in New York — , fostering the use of Remote Sensing in developing countries, he came back to Potsdam and took the position of the deputy director of CIPE in , which he held until Peter Bormann has not only brought his profound knowledge of seismology into these courses but also his fascinating dedication to the scientific matter.
His unique ability to impart knowledge has been invaluable and a great support for education and professional career development of generations of seismologists, particularly in developing areas. It was translated completely into Chinese and partly into several other languages such as Bahsa Indonesia, Russian and Turkish.
January 26, Gujarat, India Earthquake Mw7. Mori 9. Mori Period WavelengthBody waves 0. Note thedetailed interpretation of secondary phase onsets. Structure in the Earth results in complicated paths Lowrie, , fig 3. Wysession Courtesy R. MereuCourtesy J. Courtesy J.
Stacked broadbandseismograms for shallowearthquakes. Therefore unlike magnitudeintensity is not a singlenumber. Natural Vibrations of the Earth Shearer Ch. You just clipped your first slide!
- Commission on Seismological Observation and Interpretation (CoSOI) | IASPEI!
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