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not permit Ghassemi et al . (2014) to use the radiocarbon age of sample Ira.2008/C-IV (1105 ± 30 yr BP) to identify a possible seismicevent at the base of unit 27, to be associated with the 958 AD Ray-Taleghan event (M ≈ 7.7).
If the MAM age of sample IRA4 (3.5 ± 0.4 ka) has overestimated the true burial age of unit 29, it has positive effect on the interpretation of Ghassemi et al . (2014) to associate trench seismicevents to some historical events (e.g., unit 27, to be associated with the 958 AD Ray-Taleghan). Particularly, it may confirms Ghassemi et
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