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Zur tektonischen Stellung des jungen Vulkanismus in Mittel-Europa
The regional arrangement of tertiary and post-tertiary (simic) volcanisme, together with postvolcanic CO2-exhalations has been used to determine the boundary lines of larger units of the earth's crust in Middle-Europe. Hypothetic conclusions are based on a map showing the distribution of volcanic phenomena into the tectonic fabric of the continent.
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