First evidence for large earthquakes on the Deshir Fault, Central Iran Plateau

H. Nazari (1) , M. Fattahi (2, 3, 4) , Bertrand Meyer (5) , Michel Sébrier (5) , M. Talebian (1) , M. Foroutan (1) , Kristell Le Dortz (5) , M.D. Bateman (3) , M. Ghorashi (1)

1 Research Institute for Earth Sciences
2 The Institute of Geophysics
3 Sheffield Centre for International Drylands Research, Department of Geography
4 Center of Environment South Parks Road
5 iSTeP - Institut des Sciences de la Terre de Paris

Although sliced by several strike slip faults, a large part of Central Iran remained aseismic during the period of time covered by the instrumental and historical seismic records. Stating the existence of earthquakes in the Holocene is therefore important for the assessment of the regional seismic hazard. A paleoseismic study of the Deshir fault demonstrates that Central Iran hosted large earthquakes during latest Pleistocene and Holocene. The last event corresponds to 1m-deep fissures which sandy infilling yielded an optically stimulated luminescence (OSL) age of 2.8±1.4 ka. At least two previous events, outlined by older fissures and/or colluvial wedges, have been recorded over the last 10-30 ka. The magnitudes are difficult to assess because the actual slips per event are unknown. The size of the fissures and the significant vertical displacement associated to a colluvial wedge are nevertheless compatible with M≈7 events along a primary strike-slip surface break.

Domaines: Sciences de la Terre

H. Nazari, M. Fattahi, Bertrand Meyer, Michel Sébrier, M. Talebian, et al.. First evidence for large earthquakes on the Deshir Fault, Central Iran Plateau. Terra Nova, 2009, 00, pp.1-10. ⟨10.1111/j.1365-3121.2009.00892.x⟩. ⟨hal-00425581⟩