1) North Wu-tai-shan
北五台山
2) 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。
4) Mount Wutai
五台山
1.
Niche characteristics of dominant species from Oxytropis coerulea communities in mount Wutai,Shanxi;
五台山蓝花棘豆群落优势种群生态位研究
2.
A study on the diversity of the Oxytropis coerulea community of mount Wutai in Shanxi province;
山西五台山蓝花棘豆群落的多样性研究
3.
On Local Chronicles of Mount Wutai in History;
五台山历代山志编撰略考
5) Wutaishan
五台山
1.
Petrogenesis of Neoarchean Wutaishan Granitoids and Its Geodynamic Significances;
五台山晚太古代花岗岩的成因及其动力学意义
2.
Early Proterozoic high-pressure metamorphism in the Wutaishan.;
五台山早元古代高压变质作用研究
3.
Late Archaean Mafic ultramafic Rocks from the Wutaishan, Shanxi Province: a Possible Ophiolite Melange;
山西省五台山晚太古代镁铁质-超镁铁质岩: 一种可能的古蛇绿混杂岩
6) Wutai Mountain
五台山
1.
Impact of tourism activities on patterns of meadow population on south top of Wutai Mountain;
五台山南台旅游活动对山地草甸优势种群格局的影响
2.
β-Diversity of Subalpine Meadows in Wutai Mountain;
五台山亚高山草甸的β多样性研究
3.
Apatite fission track study of Cenozoic uplifting and exhumation of Wutai Mountain, China;
五台山新生代隆升剥露的磷灰石裂变径迹研究
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"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条