Hot orogen behaviour, partial melting and ductile flow: Case study of the Damara Orogen, Namibia

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The Damara Orogen in Namibia preserves an exceptional record of Neoproterozoic–Cambrian continent–continent collision during Gondwana assembly. It provides a natural laboratory suitable for testing thermomechanical models of hot orogens. We integrate regional-scale structural mapping from satellite imagery and aeromagnetic data with published lithostratigraphic, metamorphic, magmatic, and geochronological constraints; this is used to evaluate the first-order architecture and tectonic evolution of the belt. Results show strong partitioning between a high-temperature, low-pressure (HTLP) Central Zone and lower-temperature, higher-pressure (LTHP) Northern and Southern zones. The Central Zone is characterised by Buchan-series metamorphism, widespread granite–migmatite terranes, voluminous crustally derived leucogranites, complex dome-and-basin interference patterns, non-cylindrical folds, and distributed syn-magmatic deformation. In contrast, the flanking zones preserve comparatively linear fabrics, inverted Barrovian metamorphic gradients, and foreland-vergent fold-and-thrust architectures consistent with oppositely dipping marginal wedges. Igneous evolution in the Central Zone records early calc-alkaline to tholeiitic magmatism at ca. 575–540 Ma, followed by widespread crustal-melt leucogranite magmatism at ca. 530–510 Ma; this 2-stage time-evolution is characteristic of radiogenic heat production in thickened crust. We interpret the Damara Belt as a hot orogen in which partial melting triggered a transition from wedge-dominated contractional tectonics to distributed mid-crustal flow within the Central Zone. The Damara Orogen demonstrates how temperature, partial melting, and crustal rheology fundamentally influence deformation during continental collision. It further demonstrates that even moderately sized orogens may evolve large-hot-orogen style behaviour under favourable thermal conditions.

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