Contribution à l'étude des formations superficielles de la boutonnière du Bélinois (Sarthe, France)
The geomorphological and sedimentological study makes it possible to distinguish several superficial formations preserved in the Belinois depression. The lower fine sands come from the alteration of Jurassic marl-limestone whereas the upper sands issue from Cenomanian outlying sands and were brought...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Physio-Géo
2008-09-01
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| Series: | Physio-Géo |
| Subjects: | |
| Online Access: | http://journals.openedition.org/physio-geo/765 |