Abstract:On November 6,1988,two earthquakes with a magnitude >7 occurred in the Lancang and Gengma area of the southwestern part of the Yunnan province.The maximum intensity of the M7.6 Lancang earthquake was IX on the Chinese scale,which is similar to the Modified Mercalli scale.The surface rupture of the tectonic activity of the Lancang MS7.6 earthquake occurred because of the earthquake-related extensional ground cracks and small fault scarps in the epicentral region. The area within which the cracks and small scarps occurred was approximately 35-km long and 3-km wide.The maximum vertical and the dextral horizontal offsets were 1.5mand 1.4m,respectively.The M7.6earthquake showed complicated earthquake-generating tectonics and formed a separate obvious seismic deformation belt along the Heihe and Lancang faults.The Heihe fault is one of the seismogenic faults of the 1988 M7.6event of Lancang.The Heihe fault,located in the southwestern part of the Yunnan province,having a length of 168km and a trend of 280°~310°,is an active fault zone in the late Quaternary,which is mainly a right-lateral strike slip with a dip slip.It turns out that the Heihe fault zone can be divided into three secondary fault segments,namely,Cangyuan-Mujia(F1-1),Mujia-Nandai(F1-2),and Nandai-Mengwang(F1-3).The activity gradually becomes weak when this segment of fault travels eastward.Through satellite image interpretation and field geological investigation,we studied the geological and geomorphologic characteristics of activity along the middle and the western segments of the Heihe fault in this research.The middle and western segments of the Heihe fault,having a length of 88km and a trend of 280°~310°,is an active fault zone in the late Quaternary,which is mainly a right-lateral strike slip with a dip slip.A variety of dislocation landforms have been formed along the fault by the new tectonic activities since the late Quaternary,such as the dextral dislocation of gullies and ridges,fault trenches,fault passes,fault scarps,and pits.A series of dextral dislocations of gullies and ridges,and scratches on the cross section along the fault show that the middle-western segment on the Heihe fault is dominated by a right-lateral strike slip.In the Xuelidazai village,the age of the displaced stratum is(2 530±25)a.B.P.,and on the faultplane,a loosely consolidated gouge is developed across several cross sections of the fault.This implies that the latest active time of the middle-western segment on the Heihe fault is the late Holocene.Near Baishuijing,there are synchronous dextral dislocations of four small gullies because of the dextral movement of faults;these dislocations range from 9to 14m.By using the differential GPS measurement,the sample dating and the regional comparison of the fault slip rate,we calculated the right-lateral strike slip rate of the segment to be(3.54±0.78)mm/a.This value agrees with the regional characteristics of the fault slip rate.