Petrological and geochronological constraints on the origin of the Palimé–Amlamé granitoids (South Togo, West Africa): A segment of the West African Craton Paleoproterozoic margin reactivated during the Pan-African collision

Author:

Agbossoumondé Y.,Ménot R.-P.,Paquette J.L.,Guillot S.,Yéssoufou S.,Perrache C.

Publisher

Elsevier BV

Subject

Geology

Reference57 articles.

1. The tectono-stratigraphic relationship between the Upper Precambrian and Lower Paleozoic Volta basin and the Pan-African Dahomeyide orogenic belt (West Africa);Affaton;American Journal of Science,1978

2. Affaton, P., 1990. Le bassin des Volta (Afrique de l'Ouest): une marge passive du Protérozoïque supérieur, tectonisé au Panafricain (600+/−50 Ma). Thèse Doctorat d'Etat, 2 vol., Collection Etudes et Thèses, Ed. ORSTOM, Paris, 499p.

3. The Dahomeyide Orogen: Tectonothermal Evolution and Relationships with the Volta Basin;Affaton,1991

4. Metamorphic evolution of Neoproterozoic eclogites from South Togo (West Africa);Agbossoumondé;Journal of African Earth Sciences,2001

5. Pan-African subduction–collision event evidenced by high-P coronas in metanorites from the Agou massif (Southern Togo);Agbossoumondé;Precambrian Research,2004

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