Zobrazeno 1 - 10
of 54
pro vyhledávání: '"M. Amenna"'
Publikováno v:
Annals of Geophysics, Vol 44, Iss 5-6 (2001)
A paleomagnetic study was carried out in the carbonates and marls of the Liassic member of the Zarzaïtine Formation of the Illizi basin (SE Algeria) deposited in a continental environment. Two magnetization components were identified. The first, def
Externí odkaz:
https://doaj.org/article/ae06e8e5277b47e490b01d09206de144
Autor:
M. E. M. Derder, B. Henry, S. Maouche, M. Amenna, A. Ouabadi, B. Bayou, R. Bestandji, H. Bouabdallah, M. Ayache, M. Beddiaf
Publikováno v:
International Journal of Earth Sciences. 111:1185-1200
Autor:
Bernard Henry, M. Amenna, Said Maouche, Sofiane Gharbi, M.E.M. Derder, H. Djellit, Catherine Dorbath, Abdeslam Abtout, R. Bestandji, H. Ymel
Publikováno v:
Tectonics. 38:4249-4266
Autor:
M.E.M. Derder, M. Amenna, Rafik Bestandji, Yves Missenard, Philippe Robion, B. Bayou, Souhila Hassina Boukerbout, Aziouz Ouabadi, Bernard Henry, Said Maouche
Publikováno v:
Arabian Journal of Geosciences. 14
Previous paleomagnetic studies performed in the central North-Algeria (Chellif and Mitidja basins) on Neogene formations pointed out tectonic clockwise blocks rotations. This deformation pattern was interpreted as resulting from a bookshelf neotecton
Autor:
Abdeslam Abtout, A. Lamali, A. Yelle-Chaouche, M. Amenna, Lamine Hamai, Nacer-Eddine Merabet, Said Maouche, Bernard Henry, Mohamed Hamoudi
Publikováno v:
1st Conference on Geophysics for Geothermal-Energy Utilization and Renewable-Energy Storage.
Summary Paleomagnetim of the Paleozoic formations in the Illizi Basin evidenced two distinct magnetization components. Using African APWP shows remagnetizations of Cenozoic and Permian ages. The distribution of the directions of these components indi
Autor:
Yves Missenard, B. Bayou, Philippe Robion, Rafik Bestandji, Bernard Henry, M. Amenna, Said Maouche, Salamet Mahboubi, M.E.M. Derder
Publikováno v:
On Significant Applications of Geophysical Methods ISBN: 9783030016555
Previous paleomagnetic studies, performed in central North-Algeria (Chelif and Mitidja basins) on Neogene formations, pointed out some tectonic clockwise rotations of large blocks, sometimes of large amplitudes. Narrow zones represent also important
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a855de5a09797b264ace453060124fe8
https://doi.org/10.1007/978-3-030-01656-2_8
https://doi.org/10.1007/978-3-030-01656-2_8
Publikováno v:
Studia Geophysica et Geodaetica. 61:185-198
The reliability of an Apparent Polar Wander Path (APWP) obviously depends on the paleomagnetic poles used to determine it. The APWP of Africa and South America are fairly well defined for the 330–260 Ma interval. However, this study pointed out a m
Publikováno v:
The Geology of the Arab World---An Overview ISBN: 9783319967936
The magnetic fabric obtained in the Hoggar shield on several plutons is related to various origins: simple flow, syn-deformation flow, stress field during late-magmatic stage and solid-state deformation. These results also evidenced the important rol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b64a48d3600c986f3fbda35459e7b4a8
https://doi.org/10.1007/978-3-319-96794-3_4
https://doi.org/10.1007/978-3-319-96794-3_4
Publikováno v:
The Geology of the Arab World---An Overview ISBN: 9783319967936
Numerous paleomagnetic studies were performed in the western Saharan basins, particularly during the last decades. Primary magnetization of the sedimentary formations older than Bashkirian appeared as totally overprinted. By contrast, 23 new coherent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c774e4f1d2b353defcf7f4e9065ba75
https://doi.org/10.1007/978-3-319-96794-3_7
https://doi.org/10.1007/978-3-319-96794-3_7
Autor:
M.E.M. Derder, M. Ayache, Aziouz Ouabadi, Hamza Bouabdallah, Bernard Henry, Said Maouche, M. Beddiaf, Rafik Bestandji, M. Amenna, B. Bayou
Publikováno v:
Arabian Journal of Geosciences. 10
In Ordovician and Silurian sedimentary formations of the Murzuq basin (Saharan platform, Algeria), different remagnetization processes have been highlighted. These magnetic overprints totally replaced the primary magnetization. They are mainly due to