By P. Giese, C. Prodehl, A. Stein (auth.), Prof. Dr. Peter Giese, Dr. Claus Prodehl, Dr. Albert Stein (eds.)

The choice of crustal constitution by way of explo­ sion seismology has been one of many significant pursuits of the eu Seismological fee (ESC) over the last twenty-five years. It was once determined your time in the past to submit the result of local crustal investigations in Europe in a sequence of monographs. This booklet entitled "Ex­ plosion Seismology in primary Europe - info and effects" is quantity 1 in a chain of guides facing the crustal constitution in Europe. the eu seismologists are indebted to the German Geo­ actual Society (Deutsche Geophysikalische Gesellschaft) for taking the initiative to put up this e-book. thank you are as a result of the German study Society (Deutsche Forschungs­ gemeinschaft) for delivering beneficiant monetary help of the sphere measurements and information review. it really is was hoping that this e-book will stimulate a continuation of in­ vestigations of the earth's lithosphere for you to eluci­ date the main points that are nonetheless no longer absolutely understood.

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Explosion Seismology in Central Europe: Data and Results

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On the other hand these considerations con- 20 tribute essentially to an interpretation of seismic results in petrological terms. 1 Investigation of Seismic Noise in the Federal Republic of Germany M. 3 Hz was recorded on magnetic tape by a mobile seismic station over a period of four years. The recordings generally extend over a period of at least 24 h. At some stations the recordings were repeated after half a year or more. ). The spectral density functions, correlation functions, directional characteristics and ground-particle movements were computed from the recordings.

Messungen mit maxichapter. These methods have the admalen Elektrodenentfernungen zwischen 20 und vantage that the initial form of the 150 km wurden in verschiedenen Gegenden field is known and one has them thereDeutschlands durchgefuhrt. Das Problem der fore mathematically better "in hand". Anisotropie, das anhand aller vorliegender The classical procedure for determinMessungen studiert werden konnte, kornrnt bei ing the conductivity of a horizontalder Interpretation ultratiefer Sondierungen ly stratified subsurface is the geoeine einschneidende Bedeutung zu.

Ultra-deep sounding curve of the Rhine Graben 28 500 l00km Cm 10' 7 - - l,S rr- rr3 • . . 0 • • 0· 0 . , o. • 0 . • 0 ~ ~ 0" I! 0 • 0 MEASURING GRAPH THEORETICAL CALCULATED GRAPH 0 ~ I WAMBERGSATTEL ABh I I I II I I I I I 10m I 100m 7 300 0 0 Qo 1m ••• ! ••• I 300 1500 I I I lk'1' I 9000 I I I I I I I 10km 7000 I I I I I I II 100 km Om Fig, 3. Ultra-deep sounding curve of the Wamberger anticline The results of the above test were used for the preparation of the largescale test with AB max = 150 km along the Rhine Graben between Karlsruhe and Badenweiler in Autumn 1967.

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