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1)  north piedmont zone of Wutai Mountain
五台山北麓
1.
The studied samples are collected detailedly in two fault scarp collapse wedges(D1 and D2) from the schematic section of Nanyukou in north piedmont zone of Wutai Mountain in Xinding basin,Shanxi Province.
以山西忻定盆地五台山北麓南峪口探槽为例,对该探槽中的两期崩积楔(D1、D2)各个部位不同类型沉积物进行系统采样,对样品采用细颗粒石英(4~11μm)简单多片再生法(SMAR)进行光释光(OSL)测年,根据光释光年龄,得出如下认识:(1)D1、D2崩积楔演化过程与常规的正断层崩积楔演化模式有些差别;(2)D1崩积楔古地形面由断层处向外延伸堆积而成,D2崩积楔古地形面由水平堆积形成,且较D1厚;(3)D1崩塌结束后经历较强的水流作用;(4)两次古地震事件分别发生于(42。
2)  The north foot of Wuguishan mountain
五桂山北麓
3)  Wuguishan North Foot Fault
五桂山北麓断裂
1.
Through data processing and interpretation of the gravimetric and magnetic data,the existence of Wuguishan North Foot Fault as a deep-large fault is confirmed and it is proved strongly by the data of geology,drilling,geophysical exploration,deformation and mobile gravimetric survey observed in some important sections such as Zhongshan city.
通过对重力和航磁资料的处理,确认了五桂山北麓断裂的存在。
4)  North Wu-tai-shan
北五台山
5)  Northern piedmont of the Tianshan Mountains
天山北麓
1.
The northern piedmont of the Tianshan Mountains covers Yiwu County,Barkol Kazak Autonomous County,Changji Hui Autonomous Prefecture,Urumqi City,Shihezi City,Yili Kazak Autonomous Prefecture,Bortala Mongol Autonomous Prefecture,which was a typical area of immigration in modern times.
清代以来,新疆天山北麓地区出现了大规模的人口迁移活动,外来人口逐渐占据了当地人口的主体。
6)  northern footslope of Jishan
箕山北麓
补充资料:五台
1.唐高宗龙朔中尚书﹑门下﹑中书﹑秘书﹑御史五官署均以台名,合称"五台"。 2.见"五台山"。
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