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1)  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。
2)  The north foot of Wuguishan mountain
五桂山北麓
3)  Northern Liulengshan piedmont fault
六棱山北麓断裂
4)  Northern piedmont fault of the Changlingshan
长岭山北麓断裂
5)  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。
6)  Changlingshan Northern piedmont Fualt
长岭山北麓活动断裂
补充资料:五桂
1.旧称进士登第为折桂。五桂,对亲族五人相继登科的美称。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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