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1)  Tonglu area
桐庐地区
2)  Tongcheng-Lujiang area
桐城-庐江地区
3)  Tonglu
桐庐
1.
Technique and Efficiency of Oriented Forest Conservation in Tonglu;
桐庐县定向封山育林技术措施及成效初报
2.
Single grain zircon U Pb isotopic ages of the volcanic intrusive complexes in Tonglu and Xiangshan areas.;
桐庐、相山火山-侵入杂岩单颗粒锆石U-Pb年龄
3.
The Qixia Formation in the Tonglu area of Zhejiang Province can be divided into two fusulinid biozones:the upper Cancellina neoschwagerinoides-Verbeekina grabaui zone of the Xiangbo Stage and the lower Misellina claudiae zone of the Luodian Stage.
浙江桐庐栖霞组可划分为二个带:上部为Cancelli naneoschwagerinoides-Verbeekina grabaui带,归属祥播阶;下部为Misellinaclaudiae带,归属罗甸阶。
4)  Lu-Zong region
庐枞地区
1.
Uranium and polymetals (iron and copper) constitute the regional metallogenetic seriesin Lu-Zong region,the metallogenesis of which is mainly controlled by regional gigantic deepfaults and pre-volcanic "basement" faults.
庐枞地区铀与铁、铜等多金属组成区域成矿系列,其成矿作用主要受区域性深大断裂及火山岩前“基底”断裂的控制,燕山期的岩浆活动及其演化是成矿的内在因素。
5)  Lushan region
庐山地区
1.
Studies on geologic-geomorphologic tourism resources exploitation in Lushan region;
庐山地区地质地貌旅游资源开发研究
2.
Based on the hydrometeorological data, this paper analyzed the climatic characteristics and hydrologic characteristics of Lushan region.
根据水文气象资料,系统分析了庐山地区的气候特征和水文特征,为开发利用庐山自然旅游资源提供可靠依据。
6)  Lushan area
庐山地区
1.
This article analyzes the reasons for jiujiang earthquake from the angle of geological conditions in lushan area and the possbility of strong shock in Huangshi in future.
本文从庐山地区地质条件的角度分析了九江地震的原因,并对黄石地区今后发生强烈地震的可能性进行了分析。
2.
He peiyuan (1989) drew a conclusion that there were four glacial stages in the Lushan area in the Quaternary based on his tests on Fe2O3 and FeO.
本文认为用Fe~(3+)/Fe~(2+)值推算庐山地区第四纪古温度是可行的,但认为在推算方法上必须严谨合理。
补充资料:夜泊桐庐先寄苏台卢郎中
【诗文】:
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