Accès ouvert

Geochemistry of Neoproterozoic metasedimentary rocks from the Mai Kenetal-Werii area, northern Ethiopia: implications for provenance and tectonic setting

Article scientifique 2024 Anglais

Résumé

Abstract The Mai Kenetal-Werii area in northern Ethiopia consists mainly of metavolcanics, metavolcanoclastics, and metasedimentary rocks. This study investigates the provenance and depositional setting of the low-grade metasedimentary rocks of the area using whole-rock geochemistry. The major and trace element compositions were analyzed by X-ray fluorescence spectrometry (XRF) and inductively coupled plasma mass spectrometry (ICP-MS). The chondrite-normalized rare earth element (REE) pattern shows an increase in light REEs (LaN/SmN, 0.93–4.03; average 2.24), negligible negative Eu anomalies (Eu/Eu*, 0.68–1.11; average 0.85), and relatively flat heavy REEs (GdN/YbN, 0.47–2.30; average 1.4). The chemical indices, such as the chemical index of alteration, plagioclase index of alteration, and chemical index of weathering, as well as the ratios of K2O/Al2O3, Rb/Sr, Th/U, and the A-CN-K (Al2O3-(CaO*+Na2O)-K2O) ternary plot, indicate that the source area of the metasedimentary rocks has undergone moderate to intense chemical weathering. The ratios of Al2O3/TiO2, La/Sc, Th/Sc, La/Co, Th/Co, and Th/U, as well as the A-CN-K ternary plot, suggest that the protoliths of the metasedimentary rocks originated from a combination of mafic and felsic igneous sources. Additionally, the Th/Sc, Zr/Sc, and SiO2/Al2O3 ratios, along with the index of compositional variation, indicate that the metasedimentary rocks were derived from a mixture of immature mafic and felsic igneous sources, first-cycle sediments with minimal recycled components. The discrimination diagrams of La-Th-Sc and Th-Sc-Zr/10 suggest that the Mai Kenetal-Werii metasedimentary rocks were deposited in an oceanic island arc setting.

Citer ce document

Molla, M., Alene, M., Sano, T., Mengesha, H. (2024). Geochemistry of Neoproterozoic metasedimentary rocks from the Mai Kenetal-Werii area, northern Ethiopia: implications for provenance and tectonic setting. https://doi.org/10.21203/rs.3.rs-4029055/v1

Accès au document

Texte intégral en lecture en ligne, réservé aux abonnés SPHAERO et aux membres de l'institution. Se connecter

Voir l'article sur le site de la revue

Statistiques

Consultations : 1

Téléchargements : 0