TY - JOUR
T1 - Provenance and paleogeography of the Nama Group (Ediacaran to early Palaeozoic, Namibia)
T2 - Petrography, geochemistry and U-Pb detrital zircon geochronology
AU - Blanco, G.
AU - Germs, G. J.B.
AU - Rajesh, H. M.
AU - Chemale, F.
AU - Dussin, I. A.
AU - Justino, D.
N1 - Funding Information:
A post-graduate grant from the Faculty of Science (University of Johannesburg, UJ) provided financial assistance to the first author. This publication forms part of the doctoral thesis of the first author carried out at the Faculty of Science, UJ. U. Zimmermann for the guidance as co-supervisor during the doctoral thesis of the first author. We thank P. Abre, C. Cingolani and C. Gaucher for numerous discussions on the Gondwana geology. Field expenses and part of the analyses were financed by a research grant from the Sasol Fund of the Faculty of Science, UJ to G.J.B. Germs. The reviewers H.E. Frimmel and D. Chew are thanked by the positive and encouraging comments improving substantively the manuscript. P. Cawood is thanked for his efficient editorial handling. This is a contribution to IGCP 478.
PY - 2011/5
Y1 - 2011/5
N2 - A provenance study using petrography, geochemistry and U-Pb zircon dating was carried out on selected siliciclastic units of the Nama Group, a major lithostratigraphic unit in southwestern Gondwana which crops out in southern Namibia and adjacent north-western South Africa. Petrographic and geochemical results from the Nama Group indicate a homogenous recycled upper crust composition characterized mainly by metamorphic and granitic sources, with minor input from mafic rock sources that have not undergone significant weathering. Previous works based on facies and palaeocurrent analyses, and silicified volcanic ash beds and chromian spinel bearing sandstones of the Nama Basin points to a syn-tectonic volcanic island arc source located in the adjacent Damara Belt. U-Pb detrital zircon geochronology of the Nama Group rocks displays major peaks at Neoproterozoic (Pan-African orogeny) and Mesoproterozoic (Namaqua-Natal orogeny) indicating a foreland geotectonic setting for Nama deposition, confirming facies and palaeocurrents analyses. A paleocurrent shift from the north to the west in the upper "molassic" Nama Group is associated with a switch to an influx of Neoproterozoic-Cambrian detrital zircons (76%). These ages probably indicate exhumation (after 531 ± 9 Ma) of a felsic volcanic arc (Arachania) root, which is presently attached to the Río de la Plata Craton. The provenance of the Nama foreland basin suggests that continent-continent collision of the Kalahari/Congo Cratons and the Cuchilla Dionisio Pelotas Terrane (Arachania Arc) with the Río de la Plata Craton most likely occurred due to strike-slip accretion related to a component of N-S shortening in the period between 530 and 495. Ma.
AB - A provenance study using petrography, geochemistry and U-Pb zircon dating was carried out on selected siliciclastic units of the Nama Group, a major lithostratigraphic unit in southwestern Gondwana which crops out in southern Namibia and adjacent north-western South Africa. Petrographic and geochemical results from the Nama Group indicate a homogenous recycled upper crust composition characterized mainly by metamorphic and granitic sources, with minor input from mafic rock sources that have not undergone significant weathering. Previous works based on facies and palaeocurrent analyses, and silicified volcanic ash beds and chromian spinel bearing sandstones of the Nama Basin points to a syn-tectonic volcanic island arc source located in the adjacent Damara Belt. U-Pb detrital zircon geochronology of the Nama Group rocks displays major peaks at Neoproterozoic (Pan-African orogeny) and Mesoproterozoic (Namaqua-Natal orogeny) indicating a foreland geotectonic setting for Nama deposition, confirming facies and palaeocurrents analyses. A paleocurrent shift from the north to the west in the upper "molassic" Nama Group is associated with a switch to an influx of Neoproterozoic-Cambrian detrital zircons (76%). These ages probably indicate exhumation (after 531 ± 9 Ma) of a felsic volcanic arc (Arachania) root, which is presently attached to the Río de la Plata Craton. The provenance of the Nama foreland basin suggests that continent-continent collision of the Kalahari/Congo Cratons and the Cuchilla Dionisio Pelotas Terrane (Arachania Arc) with the Río de la Plata Craton most likely occurred due to strike-slip accretion related to a component of N-S shortening in the period between 530 and 495. Ma.
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U2 - 10.1016/j.precamres.2011.02.002
DO - 10.1016/j.precamres.2011.02.002
M3 - Article
AN - SCOPUS:79954782284
SN - 0301-9268
VL - 187
SP - 15
EP - 32
JO - Precambrian Research
JF - Precambrian Research
IS - 1-2
ER -