<?xml version="1.0" encoding="UTF-8"?>
<records>
<record>
<language>eng</language>
<publisher>Science and Education Publishing</publisher>
<journalTitle>Journal of Geosciences and Geomatics</journalTitle>
<eissn>2373-6704</eissn>
<publicationDate>2025-07-14</publicationDate>
<volume>13</volume>
<issue>2</issue>
<startPage>31</startPage>
<endPage>43</endPage>
<doi>10.12691/jgg-13-2-1</doi>
<publisherRecordId>JGG20251321</publisherRecordId>
<documentType>article</documentType>
<title language="eng">Geochemistry and 40ar/39ar Geochronology of Amphibolites from Banefo-Mvoutsaha Area, Central Domain of the Pan-African Fold Belt in Cameroon</title>
<authors>
<author>
<name>MVODO Hermine</name>
<affiliationId>1</affiliationId>
</author>
<author>
<name>NGA ESSOMBA TSOUNGUI Philom¨¨ne Estelle</name>
<affiliationId>2</affiliationId>
</author>
<author>
<name>KOUANKAP NONO Gus Djibril</name>
<email>kouankap@yahoo.fr</email>
<affiliationId>3</affiliationId>
</author>
<author>
<name>KAMGUIA WOGUIA Brice</name>
<affiliationId>4</affiliationId>
</author>
<author>
<name>SIMO Pascal</name>
<affiliationId>4</affiliationId>
</author>

</authors>
<affiliationsList>
<affiliationName affiliationId="1">Departement of Geosciences and Environnement, University of Ebolowa, P.O.Box 118 Ebolowa, Cameroon</affiliationName>
<affiliationName affiliationId="2">Department of Mining Engineering and Mineral Processing, National Advanced School of Mines and Petroleum Industries, University of Maroua, P.O.Box 46 Maroua, Cameroon</affiliationName>
<affiliationName affiliationId="3">Department of Geology, HTTC, University of Bamenda, P.O.Box 39 Bambili; Bamenda, Cameroon</affiliationName>
<affiliationName affiliationId="4">Laboratory of Petrology and Structural Geology, University of Yaound¨¦ I, PO Box 3412 Messa-Yaound¨¦, Cameroon</affiliationName>

</affiliationsList>
<abstract language="eng">The Banefo-Mvoutsaha area lies along the Central Cameroon Shear Zone and belongs to the Central Domain of the Pan-African Fold Belt in Cameroon. The amphibolites of the study area are of two types: The banded amphibolites which are associated with migmatites and composed of Hbl + Bt + Qtz + Kfs + Pl &#177; Grt + Op; and the massive amphibolites which outcrops as discontinuous bands within the garnet bearing-gneisses; its mineral assemblage is made up of Hbl + Qtz + Kfs &#177; Grt &#177; Op. The studied amphibolites are ortho-derived, their SiO2 contents range from 48 to 52 wt%, they are enriched in LREEs and LILEs relatively to HREE, and display negative Eu anomalies (0.65 ¡Ü Eu/Eu* ¡Ü 0.96), characteristics of alkali basaltic rocks, which belong to intraplate tholeiitic series. The banded amphibolites samples yield an Ar-Ar age of 618.14 &#177; 11.43 Ma, while the massive amphibolites samples ages are 547.50 &#177; 3.15 Ma. The 618 Ma age coincide with the emplacement age of granitoids that intruded the metamorphic basement of the area. The age of 547.50 &#177; 3.15 Ma is correlated to amphibolitic metamorphism events that mark the end of the Pan-African orogeny in the study area. These new Ar-Ar ages therefore point out at least two phases of amphibolitic metamorphism in the Central domain of the Pan-African Fold Belt in Cameroon.</abstract>
<fullTextUrl format="pdf">https://pubs.sciepub.com/jgg/13/2/1/jgg-13-2-1.pdf</fullTextUrl>
<keywords language="eng"><keyword>Pan-African</keyword>
<keyword>Amphibolite</keyword>
<keyword>Tholeiites series</keyword>
<keyword>Intraplate basalts</keyword>
<keyword>Argon-Argon</keyword>
</keywords>
</record>
</records>
