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Continental Terminal Formation

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This is an old revision of this page, as edited by Rangoon creeper (talk | contribs) at 07:28, 4 January 2025 (Created page with '{{Short description|Geological formation in Western Africa}}{{Infobox rockunit | name = Continental Terminal Formation | period = Palaeogene | age = ?Eocene to Pleistocene <br />~{{Fossilrange|56|1}} | image = | imagesize = | caption = | type = Geological formation | prilithology = Sandstone | otherlithology = | unitof = | subunits = | underlies = | overl...'). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Revision as of 07:28, 4 January 2025 by Rangoon creeper (talk | contribs) (Created page with '{{Short description|Geological formation in Western Africa}}{{Infobox rockunit | name = Continental Terminal Formation | period = Palaeogene | age = ?Eocene to Pleistocene <br />~{{Fossilrange|56|1}} | image = | imagesize = | caption = | type = Geological formation | prilithology = Sandstone | otherlithology = | unitof = | subunits = | underlies = | overl...')(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff) Geological formation in Western Africa
Continental Terminal Formation
Stratigraphic range: ?Eocene to Pleistocene
~56–1 Ma PreꞒ O S D C P T J K Pg N
TypeGeological formation
AreaSahara Desert
Thicknessup to
Lithology
PrimarySandstone
Location
Continental Terminal Formation is located in AfricaContinental Terminal FormationContinental Terminal Formation (Africa)

The Continental Terminal Formation is A Geological Formation in West Africa deposited during the Palaeogene to Quaternary Periods (Eocene to Pleistocene Epochs).

Fossil Content

  1. Lang, J.; Kogbe, C.; Alidou, S.; Alzouma, K.A.; Bellion, G.; Dubois, D.; Durand, A.; Guiraud, R.; Houessou, A.; de Klasz, I.; Romann, E.; Salard-Cheboldaeff, M.; Trichet, J. (1990). "The continental terminal in West Africa". Journal of African Earth Sciences (and the Middle East). 10 (1–2): 79–99. doi:10.1016/0899-5362(90)90048-J.
  2. Universite Abdou Moumouni de Niamey, Faculte des Sciences et Techniques, Departement de Geologie, Laboratoire Eaux Souterraines et Georessources, BP: 10662, Niamey, Niger.; Abdourahamane Attourabi, Sofiyane; Mamane Hallarou, Mallam; Universite Abdou Moumouni de Niamey, Faculte des Sciences et Techniques, Departement de Geologie, Laboratoire Eaux Souterraines et Georessources, BP: 10662, Niamey, Niger.; Agaissa, Assagaye; Universite Djibo Hamani de Tahoua, Faculte des Sciences de lEducation, BP : 255, Tahoua, Niger.; Moustapha Sanda Chekaraou, Mahamane; Universite Djibo Hamani de Tahoua, Faculte des Sciences de lEducation, BP : 255, Tahoua, Niger.; Ranaou Noura, Gambo; Universite Abdou Moumouni de Niamey, Faculte des Sciences et Techniques, Departement de Geologie, Laboratoire Eaux Souterraines et Georessources, BP: 10662, Niamey, Niger.; Idi Chamsi, Lawali; Universite Abdou Moumouni de Niamey, Faculte des Sciences et Techniques, Departement de Geologie, Laboratoire Eaux Souterraines et Georessources, BP: 10662, Niamey, Niger. (2024-02-29). "MAPPING RADIOACTIVITY IN CONTINENTAL TERMINAL 3 (CT3) FORMATIONS: THE CASE OF THE THREE SISTERS, NIAMEY REGION (EASTERN EDGE OF THE WEST AFRICAN CRATON, ILLUMMEDEN BASIN)". International Journal of Advanced Research. 12 (02): 17–23. doi:10.21474/IJAR01/18260.{{cite journal}}: CS1 maint: multiple names: authors list (link) CS1 maint: numeric names: authors list (link)
  3. Conrad, Georges; Lappartient, Jean-René (1987). "Le 'continental terminal', sa place dans l'évolution géodynamique du bassin sénégalo-mauritanien durant le Cénozoïque". Journal of African Earth Sciences (1983) (in French). 6 (1): 45–60. doi:10.1016/0899-5362(87)90106-0.