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1)  Wutai period
五台期
1.
Intrusives in Neo-archaean Wutai period developed widely in Matouya area of Feixian county.
费县马头崖地区新太古代五台期侵入岩发育广泛 ,为一套石英闪长岩—英云闪长岩—奥长花岗岩—花岗闪长岩的岩石序列组合 (TTG岩系 ) ,在形成时间和空间分布上相对一致 ,为一次岩浆热事件多次活动的产物 ,其成分和结构具有双重演化特征 ,构成一个较完整的岩浆演化序列。
2)  Wutai Mountains
五台山南台
1.
Ecological Response of Subalpine Meadow Populations to Tourism Disturbance on the Wutai Mountains,China;
五台山南台山地草甸种群对旅游干扰响应的识别
3)  Wutai terranes
五台地体
1.
In this paper,the ore-forming mechnism is discussed and the differences of matellogeny are explained throngh analyzing the regional ore-forming backgrourd,and comparing the geological characters of Luliang and Wutai terranes and their three-dimensional crystallization.
从区域成矿背景入手,通过对吕梁地体和五台地体地质特征的对比,结合三维地壳结晶结构,探讨其成矿机理和成矿作用的差异性。
4)  Wutaishan area
五台山区
1.
Wutaishan area is riched in iron mineral resource.
五台山区富含铁矿资源。
5)  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
6)  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
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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