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Proceedings of the International School of Applied Geophysics on title] held March 1987, Erice, Italy. Presents updated seismic techniques for the exploration of the shallower structure of the Earth as well as for the understanding of the dynamic processes taking place in the crust and upper mantle. Also the theoretical background leading to techn
Compte-rendus de NATO Advanced Study Institute tenu Ă Sandefjord, Norway du 22 avr. - 3 mai 1974, sous les auspices de Cransfield Institute NATO Advanced Study Institute on the Exploitation of Seismograph Networks, Sandefjord, Norway, 1974.
Here is unique and comprehensive coverage of modern seismic instrumentation, based on the authors’ practical experience of a quarter-century in seismology and geophysics. Their goal is to provide not only detailed information on the basics of seismic instruments but also to survey equipment on the market, blending this with only the amount of theory needed to understand the basic principles. Seismologists and technicians working with seismological instruments will find here the answers to their practical problems. Instrumentation in Earthquake Seismology is written to be understandable to the broad range of professionals working with seismological instruments and seismic data, whether students, engineers or seismologists. Whether installing seismic stations, networks and arrays, working and calibrating stationary or portable instruments, dealing with response information, or teaching about seismic instruments, professionals and academics now have a practical and authoritative sourcebook. Includes: SEISAN and SEISLOG software systems that are available from http://extras.springer.com and http://www.geo.uib.no/seismo/software/software.html
"Seismograms provide the seismologist the most efficient means of 'looking' into the most inaccessible regions of the Earth--the Earth's interior. Geophysical studies based on seismograms have drawn a vivid picture of a planet that has a solid inner core about 1250-km radius, a fluid outer core about 3470-km radius, a mantle about 2900 km thick, and a crust about 30 km thick. Other studies have pinpointed areas of high earthquake risk, where the buildings in which we live and work must be constructed to resist damaging earthquake motion. Further, the methods devised to describe Earth's internal structure have been used by many others to search for rich deposits of oil and minerals beneath its surface and its oceans"--Introduction.