Sediment Input into the Heidelberg Basin as determined from Downhole Logs
The Upper Rhine Graben, and the Heidelberg Basin in particular, play an important role in the investigation of climate change and tectonic activity during the Tertiary and Quaternary periods. Several research boreholes were recently drilled to acquire data for a new interpretation of the geology of...
Main Authors: | , |
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Format: | Article |
Language: | deu |
Published: |
Copernicus Publications
2009-04-01
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Series: | Eiszeitalter und Gegenwart |
Online Access: | https://www.eg-quaternary-sci-j.net/57/367/2009/egqsj-57-367-2009.pdf |