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1)  Pingdingshan salt field
平顶山盐田
1.
Based on analysis on well drilling data and regional data in Louzhuang Mine Section,this paper summarizes the structural condition under which halite bed of Pingdingshan salt field is formed and rhythmic characteristics of salt lake sedimentation.
通过对娄庄矿段现有钻井资料及区域资料的分析,总结了平顶山盐田石盐矿床形成的构造条件和盐湖的沉积的韵律性特征;利用测井曲线的形态进行了岩矿层对比分析,确定了沉积标志层,据矿层物性特征划分了岩层界线,论证了本矿沉积的稳定性。
2.
The paper has summarized briefly the history of discovery of Pingdingshan salt field and the course of geological exploration and development,evaluated the previous geological work,and summarized the present geological exploration degree,the geological characters of the salt field and its situation of development and utilization.
该文对平顶山盐田的发现及地质勘探开发过程进行了简明扼要的综述。
2)  Pingdingshan coalfield
平顶山煤田
1.
Based on the elemental, maceral, micro-fracture, coal facies, liquid nitrogen adsorption/desorption and mercury injection analyses, the coalbed methane (CBM) geological characteristics, coal reservoir physical characteristics, CBM resources and its exploration and exploitation prospect in Pingdingshan coalfield were systematically studied.
通过对平顶山煤田采集煤样的煤质、煤岩显微组分、煤相、煤岩显微裂隙分析,低温氮比表面及孔隙结构和压汞孔隙结构测试,研究了该区的煤层气赋存地质条件、煤层气生气地质条件和煤储层物性特征。
2.
it is discovered that Guodishan fault in Pingdingshan coalfield is a syndepositional inheritable coal-control fault- It was active during coal-forming period.
研究表明,平顶山煤田锅底山断层是1个同沉积、继承性控煤断层。
3)  flat-topped crest
平顶山顶
4)  Dingfengshan mine field
顶峰山井田
1.
According to drilling data and revealed underground geological condition of Dingfengshan mine field,Fujian Province,as well as a study on structural and coal seam features of the mine field,the paper analyzed the main geological factor to affect the changing of coal thickness.
根据福建省顶峰山井田的钻孔资料和已揭露的井下地质情况,通过对井田构造特征和煤层特征的研究,分析了影响井田煤层厚度变化的主要地质因素,对煤矿生产具有一定的指导意义。
5)  Pingdingshan
平顶山
1.
Constructing a Resource-Saving,Environment-Friendly and Modern Industrial Pingdingshan City;
资源节约环境友好与平顶山新型工业城市建设
2.
Discussion on Characteristic of Rock Salt Deposit Genesis of Pingdingshan Salt Field,Henan Province;
河南省平顶山盐田石盐矿床成矿特征探讨
3.
Geological characteristics and origin of Pingdingshan gold deposit;
平顶山岩金矿床地质特征及成因探讨
6)  Pingdingshan city
平顶山市
1.
The prevalence and control of endemic fluorosis in Pingdingshan City.;
河南省平顶山市地方性氟中毒病流行与防治概况
2.
Changes of Landuse and Landscape Pattern in Pingdingshan City Based on Remote Sensing;
基于遥感的平顶山市土地利用及其景观格局变化研究
3.
Study on the dynamic change of land use of Pingdingshan city based on RS;
基于RS的平顶山市土地利用动态变化研究
补充资料:太平顶

位于徂徕山中部的太平顶,是徂徕山的最高峰。在山巅双峰并立,古松覆盖其上。西峰较平,上边建有感应侯祠,感应侯祠是金代章宗皇帝在明昌元年(1190年)封山神为“护国感应侯 ”而建,后来毁了。故址之上巨石屹立,上边有元至正二十五年(1365年)文人补刻唐代隐士国子博士王希夷的《王野人诗》:“徂徕山下是吾家,吸露嘘风卧紫霞。几百年来无个事,朝朝座对老松花。” 西崖下有天然石洞,每当天晴气朗、夕阳西下,洞内即攒红散紫,金光烁烁,所以叫紫霞洞。王希夷曾在此修真。下边是李源寨。 顶的南边是万松岭,自古以来就多有“美松”挺立。公元前六世纪,鲁国僖公修寝庙,曾下令伐徂徕山之松树、新甫的柏树。今天这里松柏遍布,岭下有一石屋,有一眼泉水,泉水很旺。 顶东南是贵人峰。峰巅有奇石突兀,独立擎天,远望如人立。引得古人有:“泰山有丈人,徂徕有贵人。”一说。

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