Changma area 昌马地区
Changma Reservoir 昌马水库
Changma fault zone 昌马断裂带
Changma alluvial fan 昌马冲洪积扇
The results show that Changma fault is a hinge fault and its hinge axis lies at the central segment of the fault.
结果表明，昌马断裂是一条枢纽断裂，枢纽轴位于断裂中段。
The fault has been mainly in stick slip from Subei to Arkesai, and in creep slip from Bage Valley to Changma Dam since Holocene Epoch.
全新世以来，该断裂的肃北至阿克塞一段以粘滑为主，而东边的巴个峡至昌马大坝之间断裂的滑动方式则为蠕滑。
The paper predicts the changing tendency of groundwater resource in Changma alluvial fan by numerical modeling, applying the method of finite difference and irregular polygon cells.
应用有限差分方法，采用不规则多边形剖分，对昌马冲洪积扇区地下水资源数量的变化趋势进行了模拟计算。
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