Evolution of the Damara Orogen of South West Africa/Namibia: National Geodynamics ProgrammeR. McG. Miller |
Contents
THE OKONGUARRI TURBIDITES | 30 |
The Stratigraphy and Palaeoenvironment of the Damara Sequence in | 37 |
A Turbidite Succession Equivalent to the Entire Swakop Group | 65 |
Copyright | |
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alaskites albite amphibolite basalts basement basin biotite Cape Town carbonate Central Zone Chuos Formation Cloudina composition conglomerate continental crust crustal Damara Belt Damara Orogen Damara Sequence deformation deposits distal fluvial dolomite dome Duruchaus evaporite facies Fish River Subgroup folds foliation garnet geol geology gneiss granite greywackes Hakos interbedded Karibib Kasch Khomas Kröner Kuibis Subgroup Kuiseb Formation layers limestone marble Matchless Member metamorphic Miller mineralisation minerals mixtites Namibia Nappe Nappe Complex northern Nosib Group occur Okahandja Okahandja Lineament Okonguarri Omitara area pelitic phase Porada post-tectonic pre-Damara Precambrian Precambrian Res quartz quartzite ratios Rb-Sr regional rocks Salem granite samples Sandstone Sawyer schist sedimentary sediments serpentinites shale shear zones Sole Dolomite South West Africa South West Africa/Namibia southern Damara Southern Margin Zone Southern Zone Spec stratigraphic stromatolites structures subtidal Surv Swakop Group Swakop River tectonic temperature thick thrust Tinkas turbidite units Univ upper Vaalgras Subgroup volcanic Windhoek