Abstract. In spite of an increasing number of paleoseismic studies carried out over
the last decade along the Himalayan Arc, the chronology of historical and
prehistorical earthquakes is still poorly constrained. In this paper, we
present geomorphologic and paleoseismic studies conducted over a large
river-cut exposure along the Main Fontal Thrust in southwestern Bhutan. The
Piping site reveals a 30 m high fault-propagation fold deforming late
Holocene alluvial deposits. There, we carried out detailed paleoseismic
investigations and built a chronological framework on the basis of 22
detrital charcoal samples submitted to radiocarbon dating. Our analysis
reveals the occurrence of at least five large and great earthquakes between
485±125 BCE and 1714 CE with an average recurrence interval of 550±211 years. Coseismic slip values for most events reach at least 12 m
and suggest associated magnitudes are in the range of Mw 8.5–9. The
cumulative deformation yields an average slip rate of 24.9±10.4 mm yr−1 along the Main Frontal Thrust over the last 2600 years, in agreement with
geodetic and geomorphological results obtained nearby.
A 2600-year-long paleoseismic record for the Himalayan Main Frontal Thrust (western Bhutan)