The Nobi fault system consists of en-echelon left-lateral strike-slip
faults. Two restraining steps, the Midori and Hakusan upwarps, have fo
rmed between the en-echelon faults, and have demonstrated different fa
ilure behaviour. The Midori upwarp has developed into a secondary reve
rse fault while the Hakusan one has not and is still a fold. Structura
lly, the Midori upwarp is more evolved than the Hakusan upwarp. Recent
faulting has had a shorter recurrence interval since c. 14, ka B.P. T
his change may have been associated with the development of the second
ary reverse fault through the Midori upwarp, as an effective linkage i
n the Nobi fault system.