Manteldynamik, magmatische Prozesse und das Aufbrechen der Kontinente

The separation of Africa and South America about 130 million years ago was accompanied by huge volumes of magma derived from the mantle. Erosion has removed many of the surficial lavas but dolerite dyke swarms beneath them are preserved. These dykes are under study to determine the composition of ma...

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Bibliographic Details
Main Authors: Trumbull, Robert B., Keiding, Jakob K., Veksler, Ilya, Romer, Rolf L.
Format: Text
Language:German
Published: Deutsches GeoForschungsZentrum GFZ 2012
Subjects:
Online Access:https://dx.doi.org/10.2312/gfz.syserde.02.02.3
https://gfzpublic.gfz-potsdam.de/pubman/item/item_76827