By Nicholas Rast
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The target of the publication is to offer a range from the papers, which summarize a number of very important effects received in the framework of the József Hatvany Doctoral institution working on the collage of Miskolc, Hungary. in response to the 3 major examine parts of the Doctoral university demonstrated for info technological know-how, Engineering and expertise, the papers could be categorized into 3 teams.
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Extra resources for Applied Geophysics U.S.S.R.
9). But as we can show, these assumptions are not so important. If for example we make the comparison at a distance r comparable with then the intensity of the head waves will increase still more rapidly as the discontinuity in longitudinal velocities at the reflecting boundary diminishes than at fairly great distances from TQ. 9. If the longitudinal velocity alone varies in the nth layer ^ on the boundary of which the wave under consideration is formed, while the transverse velocity renudns constant, then, as can be seen from Fig, 4, the diminution in the discontinuity in longitudinal velocities at this boundary will be accompanied by a still more rapid increase in the intensity of the head waves formed at it than in the case we considered above, where we assumed that the ratio Vf^s|v^^p remained constant.
Head waves along the profile do not alter the form of the trace. ANALYSIS OF THE INTENSITY OF REFLECTED WAVES A Two-Layered Medium (a) Single Reflected Waves—The intensity of single reflected waves above the shot point is equal to the quantity QOVO,p-QiVi,p 4π(Αο + 2//ο)νο,ρ QoVo,p +Qi^i^p * The index sd signifies the shot depth. 2hQ-hsd* 38 V . P . GORBATOVA This increases in proportion to the difference in the acoustic rigidities at the interface, in inverse proportion to the bedding depth and in direct proportion to h^^.
We thus obtain three points belonging to the parallel. These points are sufficient to enable us to construct the whole parallel. The meridianal stereograpliic net constructed through 2° for a sphere J? = 10 cm, was first introduced into crystallography by Vul'f (2) and bears his name (normally as Wulff in English) (See Fig. 2). Operations with a Wulff Net The Wulff net is a transparent sheet by which any construction can be transferred to transparent paper (wax paper or ordinary tracing paper) without the use of compasses or a ruler.
Applied Geophysics U.S.S.R. by Nicholas Rast