Spatiotemporal patterns of the anticlines in the frontal Fars arc of the Zagros: insights from landscape evolution model
Haopeng Geng
During the Cenozoic, the Arabia-Eurasia collision led to deformation series of fold-and-thrusts along the Zagros foreland. This deformation produced a wide and spectacular units of fold trains. Consequently, this area presents an exceptional natural laboratory for examining the fundamental question of how and what mechanism of active fault segments grow in length. Here, we focus on the anticlines in the frontal Fars Arc, the youngest fold train in this region. It is governed by the Mountain Fron