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South Equatorial Undercurrent in the western to central tropical Atlantic

✍ Scribed by Fischer, Jürgen; Hormann, Verena; Brandt, Peter; Schott, Friedrich A.; Rabe, Benjamin; Funk, Andreas

Book ID
118664788
Publisher
American Geophysical Union
Year
2008
Tongue
English
Weight
454 KB
Volume
35
Category
Article
ISSN
1944-8007

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In south-western Algeria, dolerite sills and dykes and scarce basalt lava flows occur in the Tindouf, Reggane, Hank basins and Bechar area, and are part of the large Central Atlantic Magmatic Province (CAMP). They represent the north-easternmost witnesses of this province into the African continent.