Titlebook: Geophysik I / Geophysics I; J. Bartels Book 1956 Springer-Verlag OHG · Berlin · G?ttingen · Heidelberg 1956 Geophysik.geophysics

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書目名稱Geophysik I / Geophysics I影響因子(影響力)




書目名稱Geophysik I / Geophysics I影響因子(影響力)學科排名




書目名稱Geophysik I / Geophysics I網(wǎng)絡(luò)公開度




書目名稱Geophysik I / Geophysics I網(wǎng)絡(luò)公開度學科排名




書目名稱Geophysik I / Geophysics I被引頻次




書目名稱Geophysik I / Geophysics I被引頻次學科排名




書目名稱Geophysik I / Geophysics I年度引用




書目名稱Geophysik I / Geophysics I年度引用學科排名




書目名稱Geophysik I / Geophysics I讀者反饋




書目名稱Geophysik I / Geophysics I讀者反饋學科排名

神圣將軍

,Séismométrie, par des explosions artificielles, par exemple ceux qui servent à la prospection, on doit enregistrer des périodes encore beaucoup plus courtes, comptées en centièmes ou en millièmes de seconde, tandis que les marées terrestres mettent en jeu des périodes de douze heures et au delà. Nous ne parleron

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Nebulous

CRAFT

0085-140X Overview: 978-3-642-45857-6978-3-642-45855-2Series ISSN 0085-140X Series E-ISSN 2197-4195

和音

https://doi.org/10.1007/978-3-642-56750-6kes or explosions. These waves are of interest to seismologists not only because they form the most prominent features of seismograms but also for their usefulness in determining the structure of the earth’s crust.

和音

,Elektronische St?rstellentheorie,. The existence of this discontinuity has been established by seismic refractions and reflections, which show an abrupt increase in seismic wave speeds to a value which appears to be the same all over the world. The silicic crust is about 5 km. thick under oceans and about 35 km thick under continents.

panorama

,Allgemeines über intermolekulare Mesomerie,surface would be perfectly smooth and exhibit a simple geometrical form. However, everyone knows that the surface of the Earth is not perfectly smooth but exhibits a great number of disturbances. This fact must be the result of forces other than hydrostatic compression in the Earth’s crust and therefore requires a physical explanation.

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Surface waves and guided waves,kes or explosions. These waves are of interest to seismologists not only because they form the most prominent features of seismograms but also for their usefulness in determining the structure of the earth’s crust.