Reflection data have revealed Seaward Dipping Reflectors (SDRs) offshore Norway, Greenland, Rockall Plateau, Antarctica, Southwest Africa, Northwest Australia, East Coast USA and India (Hinz 1981). The principal evidence for volcanism has come from seismic reflection and refraction profile data. Volcanic rifted margins, which may comprise a majority of the world's rifted margins, are distinguished by their extrusive volcanism and intrusive magmatism at the time of continental break up (Hinz 1981 Mutter et al. Gravity anomalies and Earth structure, Africa, Continental tectonics: extensional, Lithospheric flexure INTRODUCTION The steep gradient that is often observed in the Airy isostatic gravity anomaly at rifted margins is therefore a useful proxy for the seaward edge of the dykes that intrude the crust prior to seafloor spreading, rather than a change in basement elevation at the boundary between oceanic and continental crust, as had been proposed by previous workers. Results from a case study in the Orange Basin, offshore Namibia show good general agreement between observed Airy isostatic anomalies and calculated gravity anomalies with T e in the range 1–3 km. We have verified our results using process-oriented gravity modelling, in which the gravity effect of surface volcanic infill loads is calculated and combined with the gravity effect of buried dyke loads and the gravity effect of their isostatic compensation. Decreasing the T e for successive loads as rifting progresses produces offlap of subpackages, while increasing the T e produces onlap. Results suggest a broken plate or significantly weakened continuous plate model is required to produce the characteristic arcuate shape. By comparing observed and calculated dips we are able to constrain the elastic plate model type and the effective elastic thickness of extended lithosphere, T e. The model, which does not require a bounding normal fault, explains the arcuate shape, limited offlap geometries and downdip thickening of SDRs as observed in seismic reflection profile data. These loads cause a surface flexure, which is subsequently infilled and loaded by volcanic material.
We present here a simple model in which SDRs are formed by a succession of dykes which intrude and load the crust. However, their origin has been disputed with some workers suggesting they form by progressive subsidence of extended crust while others propose they are accommodated within the crust by one or more continent-dipping normal faults. Seaward dipping reflectors (SDRs) are ubiquitous features of the offshore regions of volcanic rifted continental margins where they comprise wedge-shaped packages of mainly extrusive lava flows.
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