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Geologic and geomorphic characteristics of Late Quaternary reverse-thrusting segmented propagation along the Minle–Yongchang Fault within the Hexi Corridor, NW China
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DOI：10.1016/j.geomorph.2026.110365.png)
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Abstract
En 中文
• The Minle–Yongchang Fault (MYF) is segmented into three tectonic–geomorphic domains. • The Dahuang Shan segment records the highest Late Quaternary uplift and vertical slip rate. • MYF acts as a major back-thrust with SW propagation and progressive younging.
Keywords:
Minle–Yongchang Fault
Late Quaternary reverse-thrusting
tectonic–geomorphic domains
vertical slip rate
segmented propagation
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