Radiating graben-fissure systems are common on Venus. Most are thought to be underlain by mafic dykes, fed by centrally-located magmatic centres. From previous work it has been shown that these magmatic plumbing systems can extend out up to 2000. km or more and that interaction between neighbouring systems can provide insight into the relative chronology of their magmatic centres. Systematic mapping of graben-fissure systems has potential as a tool for regional magmatic chronology and correlation on Venus.This methodology is applied to the Ulfrun Regio area (200-240°E,. 0-25°N) where we mapped 47,000 graben and fissures. From these, 66 radiating systems comprised of 13,000 individual graben and fissures, and having radii of up to 2000. km have been identified, and are interpreted to be underlain by dyke swarms focussed on magmatic centres. Cross-cutting relationships among these systems and with the Hecate Chasma rift zone have been examined to provide a relative chronology for the magmatic centres. Two trends emerged: (a) an apparent younging from the southwest to northeast of the study area and (b) a cluster of older ages in the southwest, linked to the Atla Regio mantle plume.

Additional Metadata
Keywords Dyke, Graben, Tectonics, Venus, Volcanism
Persistent URL dx.doi.org/10.1016/j.icarus.2011.06.026
Journal Icarus
Citation
Studd, D., Ernst, R.E, & Samson, C. (2011). Radiating graben-fissure systems in the Ulfrun Regio area, Venus. Icarus, 215(1), 279–291. doi:10.1016/j.icarus.2011.06.026