File:Toarc.jpg
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Summary
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| Description | Toarcian fault breccia from Nontron, Dordogne, France. The breccia was created by synsedimentary faulting along the local Piégut-Pluviers Granodiorite. |
| Date | |
| Source | Own work |
| Author | Rudolf Pohl |
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I, the copyright holder of this work, hereby publish it under the following licenses:
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License. |
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File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 10:54, 19 September 2021 | | 3,456 × 4,608 (5.37 MB) | Rudolf Pohl (talk | contribs) | {{Information |Description=Toarcian fault breccia from Nontron, Dordogne, France. The breccia was created by synsedimentary faulting along the local Piégut-Pluviers Granodiorite. |Source={{own}} |Date=19/09/2021 |Author= Rudolf Pohl |Permission= |other_versions= }} Category:Toarcian Category:Nontron Category:Dordogne Category:Breccia |
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Metadata
Categories:
- Toarcian
- Geology of Nontron (Dordogne)
- Geology of Dordogne
- Breccia in Dordogne
- Faults in Dordogne
- Outcrops and exposures of Piégut-Pluviers Granodiorite
- Jurassic geology of Dordogne
- Fault breccia
- Argiles et marnes grises localement dolomitiques, dolomies gris-bleu massives ou en petits bancs localement à passées gréseuses - brèches à ciment gréseux ou grès purs à la base (Pliensbachian-Toarcian; Dordogne)