Geochemical constraints on provenance and source area weathering of metasedimentary rocks from the Paleoproterozoic (~2.1 Ga) Wa-Lawra Belt, southeastern margin of the West African Craton. Issue 1 (1st January 2019)

• Record Type: Journal Article
• Authors: Asiedu, Daniel K.; Agoe, Magdalene; Amponsah, Prince O.; Nude, Prosper M.; Anani, Chris Y.
• Is Part Of: Geodinamica acta. Volume 31:Issue 1(2019)
• Page Start: 27
• Page End: 39
• Publication Date: 2019-01-01
• Subjects: Birimian -- geochemistry -- metasedimentary rocks -- provenance -- Wa-Lawra Belt; Geodynamics -- Periodicals; Physical geography -- Periodicals
• DOI: 10.1080/09853111.2019.1670414
• Languages: English
• ISSNs: 0985-3111

Abstract

ABSTRACT: The Wa-Lawra Belt which is situated in the northern part of Ghana consists of Paleoproterozoic Birimian fine metasedimentary rocks metamorphosed to greenschist facies, particularly, in the western part. A whole-rock geochemical study of these metasedimentary rocks was undertaken to unravel their source area weathering, provenance and tectonic setting. Geochemical characteristics of the studied shales show that they are immature in nature and first cycle in origin, with little or no recycled component. Compared to Post-Archaean Australian Shales (PAAS), the studied shales indicate reduction in Zr, Hf, La, Nb, Th and Ta being the high field strength elements and evidences of transition metal enrichments in V, Ni, Sc, Co, and Cr. Major element geochemistry indicates that the shales were subjected to slight potassium metasomatism after deposition. Pre-metasomatized Chemical Index of Alteration calculations indicates that weak to moderate degree of chemical weathering took place at the sediment source area. Co-Th-La-Sc systematics reveals a combination of mafic and felsic provenances for the shales. Eu/Eu* together with values of Th/U and some abundances of trace elements show that the shales were mainly derived from juvenile rocks. Average REE model calculations suggest that the source materials are composed of about 49% basalt, 16% TTG and 35% granite.