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

保留

Aus der Geschichte des Elektronenmikroskops,t in the neighbourhood of a magnetized sphere of lodestone—a . as he termed it—the magnetic field was directed in a similar manner to the field observed at the surface of the earth. Thus by this simple model experiment . came to his well-known conclusion, “.”.

自傳

,L’agitation microséismique,nt été étudiés par tant d’auteurs professant les opinions les plus contradictoires (468 références dans [.]), qu’il est difficile de voir clairement leurs causes. Décrivons d’abord les phénomènes observés.

lymphedema

Radioactivity and Age of Minerals,adioactivity present in rocks and minerals, to which subject part D of this chapter is devoted. This is also important in other branches of physics of the earth. For example, much of the earth’s heat is generated by its radioactive elements.

禁止,切斷

,The Magnetism of the Earth’s Body,t in the neighbourhood of a magnetized sphere of lodestone—a . as he termed it—the magnetic field was directed in a similar manner to the field observed at the surface of the earth. Thus by this simple model experiment . came to his well-known conclusion, “.”.

cruise

引起痛苦

Seismic Prospecting,tion and refinement of instruments, field methods, and interpretation techniques. It is the most expensive method of geophysical prospecting, but also the most powerful. In many areas it can map beds many thousands of feet deep and detect depth variations of the order of a few feet.

overbearing

Messung elastischer Eigenschaften von Gesteinen,o am Gesteinsk?rper unter seinen natürlichen Bedingungen in der Natur m?glich und vorzuziehen. Demgegenüber besitzen Untersuchungen an Proben . vor allem me?technische Vorteile, wobei jedoch auf die oben genannten Einflüsse geachtet werden mu?, wenn man die an kleinen Proben gewonnenen Ergebnisse auf das umgebende Gestein übertragen will.

Abrupt

https://doi.org/10.1007/978-3-642-91279-5proprement parler. Le courant tellurique est essentiellement un courant variable dont l’intensité, la direction, le sens même varient d’une fa?on très capricieuse en fonction du temps. Il est possible qu’il présente une composante continue, mais en tout cas très petite, dont la réalité même est considérée aujourd’hui comme douteuse.

煉油廠

貿(mào)易

The Rotation of the Earth, and the second, the unit of time. Material standards of length and mass are provided by the International Prototype Metre and Kilogram, preserved at the International Bureau of Weights and Measures at Sèvres, near Paris. Any length or mass can be compared either directly or indirectly with sub-stan