The contribution of regional uplift and coseismic slip to the vertical crustal motion in the Messina Straits, southern Italy: Evidence from raised Late Holocene shorelines

[1] Detailed mapping and dating of raised Late Holocene shorelines in southern Calabria, central Mediterranean region, reveals that the superposed shoreline record of uplift has both steady and abrupt components. Analysis reveals quantitative constraints may be applied to displacement partitioning between regional and fault-related sources in a context dominated by forearc uplift and extension above a retreating slab. Rapid displacements of arguable coseismic origin occurred at similar to 1.9 and similar to 3.5 ka and possibly at similar to 5 ka and show a consistent site value, pattern of along-strike variation, and recurrence time (similar to 1.6 ka). The source of the rather large (similar to 1.5-2.0 m) slip per event based on the raised shoreline is not directly known and tentatively coincides with the Scilla extensional fault, which is inferred to run largely offshore. Although large uncertainties exist on the trace location, length, and seismogenic potential of the fault, our findings suggest that a substantial fraction of Holocene displacement is accommodated by coseismic footwall uplift. Precise compensation for sea level changes constrains Late Holocene steady uplift during the interseismic intervals at similar to 1 mm/yr, a value consistent with long-term (0.1-1 Ma) estimates of regional uplift. Thus, Late Holocene total uplift of a similar to 20-km stretch of coastline at similar to 1.6-2.1 mm/yr is nearly equally balanced between regional and coseismic components. Appraisal of the present elevation attained by a suite of 125 ka and younger marine terraces indicate that rapid net uplift occurred in two episodes: (1) similar to 100-80 ka and (2) after similar to 5 ka; given the constancy in regional uplift rate, the two episodes are attributable to enhanced fault slip rate. Efficient seismic strain release was clustered in intervals of 10-20 ka and intercalated with a similar to 80-Ka-long period of fault quiescence.