FN Archimer Export Format
PT J
TI The Segmented Zambezi Sedimentary System from Source to Sink: 2. Geochemistry, Clay Minerals, and Detrital Geochronology
BT 
AF Garzanti, Eduardo
   Bayon, Germain
   Dinis, Pedro
   Vermeesch, Pieter
   Pastore, Guido
   Resentini, Alberto
   Barbarano, Marta
   Ncube, Lindani
   Van Niekerk, Helena Johanna
AS 1:1;2:2;3:3;4:4;5:1;6:1;7:1;8:5;9:5;
FF 1:;2:PDG-REM-GEOOCEAN-ASTRE;3:;4:;5:;6:;7:;8:;9:;
C1 Laboratory for Provenance Studies, Department of Earth and Environmental Sciences, University of Milano-Bicocca, 20126 Milano, Italy
   Unité de Recherche Geosciences Marines, Ifremer, CS 10070, 29280 Plouzané, France
   MARE-Marine and Environmental Sciences Centre, Department of Earth Sciences, University of Coimbra, Portugal
   London Geochronology Centre, Department of Earth Sciences, University College London, London, WC1E 6BT, UK
   Department of Environmental Sciences, University of South Africa, Pretoria, South Africa
C2 UNIV MILANO, ITALY
   IFREMER, FRANCE
   UNIV COIMBRA, PORTUGAL
   UNIV COLL LONDON, UK
   UNIV SOUTH AFRICA, SOUTH AFRICA
SI BREST
SE PDG-REM-GEOOCEAN-ASTRE
UM GEO-OCEAN
IN WOS Ifremer UMR
   copubli-europe
   copubli-int-hors-europe
   copubli-sud
IF 1.8
TC 8
UR https://archimer.ifremer.fr/doc/00750/86185/91450.pdf
LA English
DT Article
AB Elemental geochemistry, Nd isotopes, clay minerals, and U-Pb zircon ages integrated by petrographic and heavy-mineral data offer a multi-proxy panorama of mud and sand composition across the Zambezi sediment-routing system. Detrital-zircon geochronology highlights the four major episodes of crustal growth in southern Africa: Irumide ages predominate over Pan-African, Eburnean, and Neoarchean ages. Smectite, dominant in mud generated from Karoo basalts or in the equatorial/winter-dry climate of Mozambican lowlands, prevails over illite and kaolinite. Elemental geochemistry reflects quartz addition by recycling (Uppermost Zambezi), supply from Karoo basalts (Upper Zambezi), and first-cycle provenance from Precambrian basements (Lower Zambezi). Mildly negative for sediments derived from mafic granulites, gabbros, and basalts, åNd values are most negative for sand derived from cratonic gneisses. Intrasample variability among cohesive mud, very coarse silt, and sand is principally caused by the concentration of Nd-rich monazite in the fine tail of the size distribution. The settling-equivalence effect also explains deviations from the theoretical relationship between åNd and TNd,DM model ages, suggesting that monazite carries a more negative åNd signal than less dense and less durable heavy minerals. Elemental geochemistry and Nd isotopes reveal that the Mazowe-Luenha river system contributes most of the sediment reaching the Zambezi Delta today, with minor supply by the Shire River. Sediment yields and erosion rates are lower by an order of magnitude on the low-relief Kalahari Plateau than in rugged Precambrian terranes. On the Plateau, mineralogical and geochemical indices testify to extensive breakdown of feldspars and garnet unjustified by the presently dry climate. Detrital kaolinite is recycled by incision of Cretaceous- Cenozoic paleosols even in the wetter lower catchment, where inefficient hydrolysis is testified by abundant fresh feldspars and undepleted Ca and Na. Mud geochemistry and surficial corrosion of ferromagnesian minerals indicate that, at present, weathering increases only slightly downstream the Zambezi River. 
PY 2022
PD MAY
SO Journal Of Geology
SN 0022-1376
PU University of Chicago Press
VL 130
IS 3
UT 000793503600001
BP 171
EP 208
DI 10.1086/719166
ID 86185
ER

EF