Geochemical compositions of Neoproterozoic to Lower Palaeozoic (?) shales and siltstones in the Volta Basin (Ghana): Constraints on provenance and tectonic setting

Author:

Amedjoe Chiri G.,Gawu S.K.Y.,Ali B.,Aseidu D.K.,Nude P.M.

Funder

KNUST Research Fund

College of Engineering

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference90 articles.

1. The provenance and tectonic setting of the Neoproterozioc Urn Hassa Greywacke Member, Wadi Hammamat area, Egypt. Evidence from petrography and geochemistry;Abd El-Rahman;Journal of African Earth Sciences,2010

2. Provenance and source area weathering derived from the geochemistry of pre-Cenomanian Sandstones, East Sinai, Egypt;Adel;Journal of Applied Sciences,2011

3. Le Bassin des Volta (Afrique de l'Ouest): une marge passive, d'âge Protérozoïque supérieur, tectonisée au Panafricain (600 ± 50 Ma). Edition de l'ORSTOM, Collection Etudes et Thèses, Paris, 2 vol.;Affaton,1990

4. The tectono-stratigraphic relationships between the Upper Precambrian and Lower Paleozoic Volta Basin and the pan-African Dahomeyide Orogenic Belt (West Africa);Affaton;American Journal of Science,1980

5. Trace and rare earth elements geochemistry of Oshosun sediments of Dahomey Basin, Southwestern Nigeria;Ajayi;Journal of Applied Sciences,2006

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