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双语推荐:形成条件

储、盖、通、源是对地热形成条件的简述。通过多年的地热勘查工作实践,笔者认为:储、盖、通、源仅仅是地热形成的必要条件,深部“承压水滞留”才是地热形成的充分条件。“储、盖、通、源、滞”是地热形成的“充要”条件
“Reserve ,cover ,tunnel ,source”is a brief introduction of geothermal formation conditions .De-pending on geothermal exploration in several years ,it is regarded that “reserve ,cover ,tunnel ,source”is a necessary conditon of geothermal formation ,while deep“confined water” detention”is a full conditon of geothermal formation .“reserve ,cover ,tunnel ,source ,detention” is the sufficient and necessary condi-tions of geothermal formation .

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本文是在充分研究地质灾害形成条件,以遥感解译、地面调查和勘查测绘为工作手段,完成的汉台区地质灾害详细调查工作的基础上实现的。通过分析地形地貌、地质构造、地层岩性、岩土体类型、降水、地表水、地下水、人类工程活动、地震等形成条件与地质灾害的关系,认为汉台区地质灾害是各种形成条件综合作用的结果,每类地质灾害形成或发生,其主导条件不尽相同。因此,研究地质灾害的形成条件,对于分析地质灾害的成因和机制,掌握其发育规律以及减灾、防灾十分必要。
This article is achieved in the full study on geological hazards forming conditions, by remote sensing interpretation, ground investigation, exploring and surveying, on the basis of detailed investigations of geological hazards in Hantai which is completed. By analyzing the relationship between geological disasters and formation conditions of topography, geological structure, lithology, soil and rock type, precipitation, surface water, groundwater, human engineering activities, earthquakes. Thinking geological hazard in Haitan is a result of the combined effects of the formation conditions. The formation or occurrence of each type geological hazards, the dominant condition is different. Therefore, the study on formation of geological hazards is necessary for analyses the causes and mechanism of geologic hazards, controls their development, disaster mitigation and disaster preparedness.

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结合798水电站引水渠道右滑坡体工程地质条件,分析了滑坡的形成条件、诱发因素、形成机理,对滑坡体稳定性进行了评价,提出了相应的处理措施。
Combined with the engineering geological conditions of diversion channel right landslide mass of 798 hy-dropower station,the author analyzed the inducing factors,formation conditions and mechanism of landslide;ap-praised the stability of landslide mass;and proposed corresponding treatment measures.

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本文叙述了西藏自治区浪江(浪卡子—江孜)公路泥石流的形成条件及泥石流的物质来源,阐述了不同条件形成的泥石流体积计算方法,并提出了防治措施。
Describes the formation conditions and material source of debris flow of Lang-jiang(Langkazi - Jiangzi) highway in Tibet Autonomous Region, expounds volume calculation method of debris lfow formed in different conditions, and puts forward prevention measures.

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长江是中国第一大河流,在其发展、形成过程中,如何贯通三峡形成当今格局,主要取决于当时的气候条件和当地的地形地貌、地质构造、地层岩性等地质条件。三峡地区地形高差大、雨水和雪水量大,水动能及势能充足,岩溶发育,地下暗河大规模形成,最终在更新世时期贯通三峡,形成统一的长江水系。
The Yangtze River is the largest river in China ,how did it through the Three Gorges and formed today''s pattern in its development process? That depended on the climatic conditions and the local topography such as geological struc -ture,stratum lithology.In The Three Gorges area there are large terrain elevation ,large quantity of rainwater,great water kinetic energy&potential energy and large scale of underground water .Finally it runs through Three Gorges in the Pleis-tocene Epoch ,forms a unified the Yangtze River System .

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广州地区轨道交通沿线岩溶是在有利的地层条件、地质构造条件和水文地质条件形成的。溶洞高度大多数小于3m,溶洞埋藏较浅,溶洞顶板较薄等。岩溶分布规律与发育程度主要受岩性、地质构造、地下水位变化等因素的控制。查明岩溶形成条件、分布规律和特征,对于隧道施工风险防范具有重要意义。
s:The karst in Guangzhou was developed under favorable geologic conditions including strtigraphy,geological structure and hydrogeology.The height of the most caves are less than 3 m.The buried depth is shallow,and the thicknesss of the cave roof is thin.The distribution and degree of development is controlled by lithologic characters,geologic structure,the fluctuating underground water table and other factors.It is important to explore its forming conditions,distribution rule and character for avoiding tunneling danger.

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根据商标的特性,将影响商标名汉语外来语音节可接受性的制约条件宏观地分为六大类:语言制约条件、美学制约条件、法律制约条件、商业制约条件、文化制约条件和心理制约条件。此外,也发现了商标名汉语外来语形成中采取的增音,减音和音变等策略具体的制约条件,并研究出其制约条件的等级排列。
Based on the specific characteristics of brand name ,it detected six macro types of constraints on the syllable acceptability of Chinese loanwords in brand name ,which respectively were linguistic ,aesthet-ic,legal,commercial,cultural and psychological constraints .Furthermore,it explored the concrete con-straints on the choices of different types of strategies such as epenthesis , deletion and replacement in sound ,and discovered the constraint hierarchies for each of the strategic choices .

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受城市建设的发展、工程地质条件、水文地质条件及人为因素等的影响,原本稳定的边坡逐渐转变成滑坡。综合大理团山南滑坡的形成特点、工程地质及水文地质特征,对已形成的公园滑坡提出加固治理方案,为今后的类似工程提供参考和借鉴。
The slope gradually turned into landslide due to the development of city construction, engineering geologic condition, hydrogeological condition and some human activities. Taking the landslide formation feature, the engineering geological and hydrogeological condition of slope of Dali Mountain park into account, this paper puts forward the corresponding reinforcement treatment solutions, providing a reference for future similar enginerings.

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雎水河流域位于四川省安县西北部,属于“5.12”汶川 Ms 8.0级地震重灾区。地震发生后的5个汛期内,每年均有不同规模的群发性泥石流发生。其中以2013年7月9日的泥石流灾害最为严重,规模与灾情巨大,造成了惨重的损失。在对雎水河流域泥石流灾害现场调查的基础上,从泥石流形成的物源条件、地形地貌条件和水动力条件入手,以ArcGIS为平台,利用DEM数据,结合区域地质构造和地层岩性等信息,分析了泥石流的形成条件、分布特征及灾害特征。研究得出结论:①流域地形地貌为泥石流的形成和径流流通提供了极为有利的地形条件,固体松散物质补给量潜力巨大,为泥石流的形成提供了物源条件,大强度局地暴雨给泥石流的形成提供了强大的水动力条件。②研究区内泥石流主要分布在页岩等软弱地层区域以及断裂构造发育的区域,地形坡度陡、地形起伏度大的地区则更为密集。③流域内泥石流具有群发性、高频率、密度大、搬运能力强、崩滑流灾害相互叠加灾害效应放大的特征。
Jushui River is located at Northwest of Anxian County in Sichuan Province,which belongs to the epicenter area of the 2008 Wenchuan Earthquake.During the past five flood seasons,there are group-occurring debris flows with different scales every year at Jushui River. The debris flows happened on July 9 of 2013 is the most destructive,and has brought out huge damages to the area of Jushui River.In this paper,we discussed the characteristics,distribution and formation conditions of the debris flow in Jushui River on the basis of tracking investigation, topographic and rock information,and got some preliminary conclusions as listed below:firstly, the large elevation deviation,huge amount of unconsolidated sediments and intensive rainstorm in Jushui River area are beneficial conditions to the generation of huge and destructive debris flows;secondly,The debris flow mainly distributes in the area where shale,fractures exposed,as well as the areas with sharp terrain slope and elevatio

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客家是中华民族汉族的一个分支,它在闽粤赣边地形成。它形成的基本条件为:第一,主体条件:客家不是一个单纯的文化概念,有其实存的主体;中原汉人移民及其融合的原住民是客家文化的主体;主体的形成必须有相当的人口规模;客家血缘因素与文化因素并存。第二,地域条件:一定的地域是客家文化物质基础的形成地;在一定的地域内的繁衍生息构成生产力第一要素;在一定的地域发展经济奠定客家文化的物质基础;一定的地域是客家人口播迁的出发地和寻根的祖地。第三,时间条件:人口集聚和发展生产需要一定的历史时期;客家民俗文化在一定的历史时期形成;客家方言在一定的历史时期形成。第四,环境条件:需要安定的社会环境;需要与之相适应的宗法制社会环境;需要良好的文化教育环境。客家思想文化的形成,是客家文化成熟的重要标志。
Hakka is a branch of the Han nationality , which formed in the border among Fujian , Guangdong and Jiangxi provinces.The following is the basic condition for its formation.The first is the subject condition.Hakka is not a simple concept of culture , there are actually existent subject.Central plains Han Chinese migration and fusion of Aboriginal are the subject of Hakka culture.The formation of the subject must have considerable population scale, the coexistence of Hakka consanguinity and culture factors.The second is the regional condition.A certain region is the formative place of Hakka culture.Human multiply makes up the first element of the productivity in the region.The regional economic development lays material base of Hakka culture.The region is the starting point of Hakka population migration , and the ancestral land of seeking roots.The third is the time condition.The popula-tion agglomeration and production development need some time.The formation of Hakka folk culture and H

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