Study of Paleoearthquakes by Combined Trench on Zemuhe Fault around Daqingliangzi,Xichang, Sichuan Province
摘要
There exist some uncertainties in dating paleoearthquakes. To improve the credibility of determination of the earthquakes, comprehensive analysis of movement patterns, sedimentary environment and micro-topography has been made to investigate the paleoseismic events along the Zemuhe active fault zone. Combined trenches were excavated near Daqingliangzi, which reveal three palaeoearthquakes with ages of 160 a, 3 100 a and 5 500~8 900 a, respectively, and a recurrence interval of about 3 000 years. Sedimentary processes related to strike-slip fault type earthquakes are discussed and a sedimentary model is put forward for strike-slip fault on condition that bulges and reverse scarps were formed at hillside area.