Can the geometry of an injection clastic dike swarm indicate a short-term process? Examining the Dead Sea Basin in Israel

Abstract

Despite the importance of identifying dynamic stress fields, doing so is not straightforward. This is because most geological processes occur slowly and the formation of fractures is generally attributed to long-term processes.Within the seismically active Dead Sea Basin (DSB), radial and concentric injection clastic dikes were emplaced during earthquake events, but a satisfactory explanation for their geometric configuration is lacking. In this study, field observations were used to explore whether the geometry of the injection clastic dike swarm reflects a quasistatic state of stress, such as with a salt diapir, or if it reflects a dynamic short-term stress state associated with the passage of seismic waves. The results show that the radial clastic dikes are not concentrated toward one central point located approximately 3 km east of the Ami'az Plain, that the concentric clastic dikes are arranged by three subsets, and that the spatial density and strain of both fracture sets are focused mainly toward the center of the Ami'az Plain. This evidence does not fit with a quasistatic state-of-stress interpretation of the region that would be associated with a local stress state around a salt diapir. A more plausible explanation is that the geometry of the radial and concentric clastic dike sets was controlled by short-term seismic waves that were probably generated by earthquake events located along an adjacent fault and that were trapped by the sedimentary basin located below the Ami'az Plain itself.The reconstruction of the injection clastic dike pattern may provide an opportunity to more deeply understand the short-term process induced by paleoearthquakes occurring adjacent to sedimentary basins close to the surface.