Die Entwicklung der Erdrinde

  • H. Berckhemer


The key and the well established basis for our present understanding of the evolution of the earth’s lithosphere is the continous creation of new oceanic lithosphere in the mid oceanic ridge system. Paleomagnetic evidence and the concept of global plate tectonics permit a quantitative reconstruction of the kinematic history of the lithosphere for the past 200 m.y. This leads to continent configurations very similar to those proposed by A. Wegener. Plate tectonic processes can be traced back until Precambrian times. Before that, due to the generally higher temperature of the earth, the evolution was apparently governed by different processes. Thermal convection and gravitational instabilities are considered as driving forces for the lithosphere.


Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.


  1. 1.
    Möller D., Ritter, B.: J. Geophys. 47, 110 (1980)Google Scholar
  2. 2.
    Uyeda, S.: The New View of the Earth. San Francisco: Freeman 1978Google Scholar
  3. 3.
    Wegener, A.: Die Entstehung der Kontinente und Ozeane. Nachdruck der 1. und 4. Auflage 1915, 1929 (Hrsg. A. Vogel). Braunschweig: Vieweg 1980Google Scholar
  4. 4.
    Scotese, C.R.: Continental Drift “Flip Book”. Univ. of Chicago 1979Google Scholar
  5. 5.
    Kröner, A. (ed.): Precambrian Plate Tectonics. Amsterdam: Elsevier 1980Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 1981

Authors and Affiliations

  • H. Berckhemer
    • 1
  1. 1.Institut für Meteorologie und Geophysik der UniversitätFrankfurt/M.Deutschland

Personalised recommendations