J. Kokonyangi

Petrology and geochronology of Mesoproterozoic mafic–intermediate plutonic rocks from Mitwaba (D. R. Congo): implications for the evolution of the Kibaran belt in central Africa

Mesoproterozoic supracrustal rocks in the Kibaride belt (southeast Congo) were intruded by mafic–intermediate plutonic rocks. These igneous rocks were affected by greenschist- to amphibolite-facies metamorphism during the Mesoproterozoic Kibaran orogenesis. U–Pb single zircon dating of the Mitwaba mafic–intermediate plutonic rocks yields an emplacement age of 1.38 Ga. The compositions of the Mitwaba mafic–intermediate plutonic rocks range from gabbro to diorite and show the following elemental concentrations: SiO2: 49–58 wt %, TiO2: 0.53–0.92 wt %, Al2O3: 13.1–18.68 wt %, Zr: 45–142 ppm, Y: 13–43 ppm. Mg no. 40–66 indicates variable degrees of fractionation of the magmas. The rocks are marked by high and variable Th/Ta (3–14), La/Nb (2–5) and low Ce/Pb (0.3–12.8) and Ti/V (10–19). Chondrite-normalized REE patterns exhibit enrichment in LREE relative to HREE ((La/Yb)N = 2.9–5.8). Primordial mantle-normalized spider diagrams show negative slopes with gradual decrease from LIL to HFS elements and are marked by Nb and Ti negative anomalies. Immobile trace-element contents indicate a continental arc setting for these mafic–intermediate igneous rocks. They are inferred to have originated from a mantle wedge enriched by fluid from a subducting slab, with possibly an additional contribution from subducted sediments. Low, sub-chondritic Nb/Ta ratios in these mafic rocks support this interpretation. A model involving underplating of mafic–intermediate arc magma into the crust, triggering partial melting of Mitwaba group metasedimentary rocks during the accretionary stage of the Kibaran orogeny, is proposed to explain the coeval emplacement of mafic–intermediate arc magmas and peraluminous S-type granitoids in the Kibaride belt of central Africa.

U‐Pb SHRIMP Dating of Detrital Zircons from the Nzilo Group (Kibaran Belt): Implications for the Source of Sediments and Mesoproterozoic Evolution of Central Africa

The Kibaran Supergroup, a >3000‐km‐long belt of metasedimentary and igneous rocks in the southeastern Congo, is in a critical location between the Congo Craton (sensu stricto) and the Tanzania‐Bangweulu Block. Understanding its tectonic evolution will shed much‐needed light on the amalgamation history of sub‐Saharan Africa. This study presents U‐Pb SHRIMP age data for 150 detrital zircons from four metasedimentary formations of the Nzilo Group, the middle lithostratigraphic unit within the Kibaran Supergroup in Katanga Province. These samples yielded dates between \documentclass{aastex} \usepackage{amsbsy} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{bm} \usepackage{mathrsfs} \usepackage{pifont} \usepackage{stmaryrd} \usepackage{textcomp} \usepackage{portland,xspace} \usepackage{amsmath,amsxtra} \usepackage[OT2,OT1]{fontenc} \newcommand\cyr{ \renewcommand\rmdefault{wncyr} \renewcommand\sfdefault{wncyss} \renewcommand\encodingdefault{OT2} \normalfont \selectfont} \DeclareTextFontCommand{\textcyr}{\cyr} \pagestyle{empty} \DeclareMathSizes{10}{9}{7}{6} \begin{document} \landscape

The Mesoproterozoic Kibaride belt (Katanga, SE D.R. Congo)

3214\pm 7

Paleoarchaean charnockite in the Ntem Complex, Congo Craton, Cameroon: insights from SHRIMP zircon U-Pb ages

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Geological Fieldwork in the Kibaran-Type Region, Mitwaba District, Congo (former Zaire), Central Africa

1329\pm 32

International Conference on the Sediment-hosted Base Metals in Neoproterozoic West Gondwana – Report of IGCP-450 Meeting in Lubumbashi, DR Congo, South-Central Africa

\end{document} Ma. Prismatic Mesoproterozoic detrital zircons (dated at \documentclass{aastex} \usepackage{amsbsy} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{bm} \usepackage{mathrsfs} \usepackage{pifont} \usepackage{stmaryrd} \usepackage{textcomp} \usepackage{portland,xspace} \usepackage{amsmath,amsxtra} \usepackage[OT2,OT1]{fontenc} \newcommand\cyr{ \renewcommand\rmdefault{wncyr} \renewcommand\sfdefault{wncyss} \renewcommand\encodingdefault{OT2} \normalfont \selectfont} \DeclareTextFontCommand{\textcyr}{\cyr} \pagestyle{empty} \DeclareMathSizes{10}{9}{7}{6} \begin{document} \landscape