By Wolf-Christian Dullo, Geologische Vereinigung e.V.
Because the early a long time of the final century, a few eminent eu scientists have contributed to the construction of a brand new viewpoint of our planet Earth. a few amazing clinical articles have been released within the magazine Geologische Rundschau (now International magazine of Earth Sciences), regularly in German. those milestones of geoscientific learn come in English for the 1st time and are offered during this quantity. recognized authors comprise for instance Alfred Wegener, a pioneer of recent geology, Gustav Steinmann, Alexander Du Toit, Wolfgang Schott, Hans Cloos and Carl W. Correns. The reader will discover a wealth of knowledge approximately how new insights in particular fields have prompted the advance of geoscientific study.
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Extra resources for Milestones in Geosciences: Selected Benchmark Papers Published in the Journal Geologische Rundschau
Lief 1925 C. Diener, Grundzüge der Biostratigraphie. Leipzig u. Wien, F. Deuticke 1906 Albert Heim, Ein Profil am Südrand der Alpen, der Pliozänfjord der Breggiaschlucht. Geol. Nachlese Nr. 15. Vierteljahrsschr. d. Naturf. Ges. Zürich 51, p. 1–49, t. 1, 2 1924 Arnold Heim, Über submarine Denudation und chemische Sedimente. Geol Rundschau 15, p. 1–47 1915 F. Heritsch, Die österreichischen und deutschen Alpen (Ostalpen). Handb. d. reg. Geol. II, 5 1903 H. Hoek, Geologische Untersuchungen im Plessurgebirge um Arosa.
Rundschau 4, p. 572–575 1892 F. Wähner, Korallenriffe und Tiefseeablagerungen in den Alpen. Ver. f. Verbreitung naturwiss. Kentnisse, Wien 1903 – –, Das Sonnenwendgebirge im Unterinntal. I. Teil. Leipzig und Wien, Fr. Deuticke 1906 K. Zöppritz, Geologische Untersuchungen im Oberengadin zwischen Albulapaß und Livigno. Ber. d. Naturf. Ges. Freiburg i. B. 16, p. 164–232, t. 5, 6 S34 S35 S36 S37 S38 S39 S40 S41 S42 A. L. du Toit Amerika und Eurafrika: the origin of the Atlantic–Arctic Ocean Geol Rundsch 30:138–147 Received: 8 April 2002 © Springer-Verlag 2002 Abstract The Atlantic–Arctic Basin is antipodal to the Pacific.
The ones cut at an angle or vertically are not drawn, but are represented by the same dotted pattern as the sparse matrix between the coccoliths. This matrix consists of small globules of saprokonite. Drawn at 200 times magnification, and magnified 3 times in the figure. Polished piece of the Maran breccia, in natural size. The dolomitic material appears light to dark gray. In general, the newly formed calcite veins, which crosscut the dolo- Fig. 4 Maran Breccia. Maran near Arosa, Bünden mite clasts, are brighter.