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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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African Platform (1)
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Central Africa
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Angola (2)
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Congo (1)
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Gabon (1)
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Chad Basin (2)
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East Africa
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Sudan (17)
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East African Rift (2)
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Kufra Basin (5)
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Nile River (2)
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North Africa
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Algeria
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Tassili n'Ajjer (1)
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Atlas Mountains
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Egypt
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Libya
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South Africa (3)
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Tibesti Massif (2)
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West Africa
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Synapsida
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Cephalopoda
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Protista
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Primary terms
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East African Rift (2)
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Palynomorph composition and palynofacies analysis of the Cenomanian Bahariya Formation in the north Western Desert of Egypt: Depositional palaeoenvironment and sequence stratigraphic implications
Late Messinian submarine channel systems in the Levant Basin: Challenging the desiccation scenario
The 21st Glossop Lecture: engineering geology and the geoscience time machine
On the Variability of Benthic Foraminiferal Species of the Genus Ramulina in the Tethys
Gouge fabrics reset by thermal pressurization record stress on faults after earthquakes
Re-assessing copper and nickel enrichments as paleo-productivity proxies
Gravimetry and petrophysics for defining the intracratonic and rift basins of the Western-Central Africa zone
The enigmatic continental crust of North-Central Africa: Saharan Metacraton or Central Sahara Shield?
Pollen morphology of the subfamily Salicornioideae (Chenopodiaceae) in Eurasia and North Africa
Transfer zones in Mediterranean back-arc regions and tear faults
The Campotosto linkage fault zone between the 2009 and 2016 seismic sequences of central Italy: Implications for seismic hazard analysis
Palaeosecular variations of the geomagnetic field in Africa during the Holocene: a review
Abstract The importance of the full understanding of the Holocene geomagnetic field spans from human history and archaeology, to palaeoclimatic changes and engineering, to geomagnetic field modelling and unravelling of the geomagnetic field characteristics and anomalies. Unfortunately, the dearth of data from large under-covered areas such as oceans, the African and South American continents, and the southern hemisphere (only 4–6% of the global datasets) dramatically limits our knowledge of the temporal and spatial evolution of the geomagnetic field and its application. Here, a review of all data from the African continent is presented in order to encourage and motivate a new generation of palaeomagnetic and archaeomagnetic studies. New data will sharpen the palaeomagnetism as a dating tool, improve our knowledge of local/global geomagnetic features, and will help to finally answer some of the fundamental questions in palaeomagnetism, like the temporal and spatial distribution of the palaeointensity peaks described, and the origin and evolution of the South Atlantic Anomaly.