Paleomagnetism of the Djebel Reouina Namurian Formation (Tindouf Basin, Algeria) /
The paleomagnetic study of the Namurian of Reouina (28.9°N, 08.0°W) revealed the existence of two magnetization components, either juxtaposed or superimposed, besides a viscous component. The high blocking temperature component, carried by hematite, has a mean direction defined by D = 126.9° and I =...
| Hlavní autor: |
Merabet, N.
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Autor )
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| Další autoři: |
Henry, B.
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Autor )
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| Typ dokumentu: | Článek |
| Jazyk: |
angličtina |
| ISSN: | 0039-3169 |
| Zdroj: | Studia geophysica et geodaetica : a journal of geophysics, meteorology and climatology, geodesy.: Roč. 43, č. 4 (1999), s. 376-389. |
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