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thermal spring
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  温泉
     CO_2/~3He RATIO OF VOLCANIC THERMAL SPRING GAS AND THE RELEASING AND RESERVOIR FORMATION MECHANISMS OF MANTLE GAS
     火山温泉气体CO_2/~3He比率与幔源气体的释放和成藏机制
短句来源
     Study on the Thermal Spring Character of Isotope and Element Hydrogeochemistry in Daocheng, Sichuan
     四川稻城温泉同位素、元素水文地球化学特征研究
短句来源
     New View of the Causes of Volcano and Thermal Spring
     火山、温泉成因新探
短句来源
     ISOTOPIC TRACER OF THERMAL SPRING OF S1 WELL AT SANJIAN,MIANZHU
     绵竹三箭水S1井温泉补给源的同位素示踪研究
短句来源
     Methods Gamma dose rate in the circumstances of thermal spring was determined with FD-3013 gamma instrument.
     方法 用FD -3 0 13数字式γ辐射仪测定温泉周边环境γ辐射剂量率 ;
短句来源
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  热泉
     The water of HCO3-Na type which are divided into four groups based on the related logarithm maps of Na+ versus HCO3- contents and Na+ versus SiO2 contents is the most common species in Tengchong thermal spring waters.
     腾冲的热泉大部分是BCO_3-Na型水。
短句来源
     The Fankou Ore bearing fluid is related to circulation hydrothermal in deep formation, and middle lower temperature Pb Zn Ag Hg polymetallic sedimentary deposit by sea floor thermal spring and overflowing was formed.
     凡口型流体与深部建造的循环热液有关 ,形成中低温海底热泉喷溢沉积铅锌银汞矿床 ;
短句来源
     The ore-bearing fluid of Fankou was relate to circulation hydrothermal fluid in deep formation and formed Pb Zn Ag Hg polymetallic middle-lower temperature sedimentary deposit by sea floor thermal spring overflowing.
     凡口型流体与深部建造的循环热液有关 ,形成中低温海底热泉喷溢沉积铅锌银汞矿床 ;
短句来源
  “thermal spring”译为未确定词的双语例句
     The Chemical Model of Thermal Spring Water of HCO_3-Na Type, Tengchong
     腾冲HCO_3-Na型热泉水的化学模型
短句来源
     This suggests that in summer the thermal spring is mainly recharged by melted ice and snow from high mountains with lower δD and δ~(18)O values, while in winter it is chiefly recharged by underground water with higher δD and δ~(18)O values.
     反映其夏季主要受δD、δ18O值低的高山常年积雪溶融水补给,冬季主要为δD、δ18O值高的地下水补给。
短句来源
     δ~18 O values of quartz in ores are 12.4‰~16.3‰ and fall in the region of thermal spring type quartz.
     矿石中黄铁矿内流体包裹体的δD值为-116.2‰,其δ18OH2O值为-5.7‰,接近美国黄石公园酸性热泉的δD值和δ18O值。
短句来源
     Heat treatment process for the springs made of TiNi shape memory alloy and its effect on the axial thermal spring back behavour of the springs have been studied.
     对TiNi形状记忆合金弹簧的热处理工艺及其对弹簧轴向热回复行为的影响进行了研究。
短句来源
     ANODIC STRIPPING SEMIDIFFERENTIALELECTROANALYSIS OF BISMUTH ATTHIN MERCURY FILM ELECTRODE——THE DETERMINATION OF Bi INSEA WATER, LAKE WATER. WELL WATER AND THERMAL SPRING WATER
     汞膜电极阳极溶出半微分电分析法测定铋的研究——海水、湖水、井水、温泉水中超痕量铋的测定
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  thermal spring
The characteristics of thermal spring waters are briefly described.
      
Within the "isolated sub-Illyrian colony" along the Thermenlinie (thermal spring line) south of Vienna, it prefers the altitude of the montane beech zone between 250 m-1250 m.
      
On the other hand, the people who live around the thermal spring area face no risk with consumption of the foodstuffs.
      
The results obtained showed that Emendere thermal spring and Emendere stream waters are unsuitable for consumption as drinking purpose.
      
At the same time, the gross-α and β concentrations are also determined in the mentioned samples and the thermal spring and other water samples.
      
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Based on the experimental results of the thermal springs, the earthquakes, the structures, the distribution Of magmatite and the thermal breaks, this paper states the characteristics of the geotherm field and discusses the relations between block movement and the Geotherm-Earthquake in Fujian, Guangdong and Jiangxi regions. The result of this study shows that the block differentiation actions are very strong in the regions since the Yanshan movement, it is closely related to the two important thermal...

Based on the experimental results of the thermal springs, the earthquakes, the structures, the distribution Of magmatite and the thermal breaks, this paper states the characteristics of the geotherm field and discusses the relations between block movement and the Geotherm-Earthquake in Fujian, Guangdong and Jiangxi regions. The result of this study shows that the block differentiation actions are very strong in the regions since the Yanshan movement, it is closely related to the two important thermal stage actions (90 million to 120 million years from now and 157 million to 165 million years from now)in crustal deep. Modern thermal field is mainly the result of the geothermal stage action which continued to develop in Mesozoic Era. It is found that the front peak of magmatic action in Fujian-Guangdong tectonic zone had become Weak and backed obviously from ocean to inland in Cenozoic Erā. But there remain the characteristics of block structure that cold block and thermal block alternated from northeast to southwest. The stronger the activities, the more remarkable the Geotherm-Earthquake Effect, and there was the characteristic that the activities gradually became stronger and stronger from inland to Taiwan.Analysing the ratio that the Geotherm-Earthquake energy in south Fujian-north Cuangdong block was depleted and disperred, we found that each of the blocks has specific DEPLETING-DISPERSING STRUCTURE, which is the thoroughfare that energy is transmitted and changed between the lower crust and upper mantle. It depends mainly on the foundation heat flow in upper mantle and the lateral nonuniformity. The energy flow of the Geotherm-Earthquake fakes about 2% of the geothermal flow of the ground Applying the equifinal principle, we study the problem that tectonic force and thermal stress act unitedly on the preparation of intraplate earthquake and the breaking mechanism, and put forward that the end points and inflection points of the rhombic block circumference are the favourable locations, which cause easily thermal break. Therefore, it is possible that Manson-Coffin effect causes the thermal fatigue of the depth rock and elastic breakearthquake. Thus it may be inferred that to study the Geotherm-Earthquake structure is a new subject which has the theoretical and practical significance.

本文依据温泉、地震、构造、岩浆岩分布及其热破裂实验结果,论述了闽粤地区热场特点,讨论断块活动与热震关系。研究表明,燕山运动以来,断块分异作用强烈,与地壳深部二次重要热幕活动(距今90—120百万年及157—165百万年)密切相关。现代热场主要是中生代热幕活动继续发展的结果。分析发现,闽粤构造活动在新生代,其岩浆活动的前峰明显减退。但却存在自北东往西南冷热交替的块断热震耗散结构特征。断块活动性越强,热震效应越显著,同时呈现从内陆向台湾渐次增强特点。剖折闽南—粤北断块的热震能量耗散比率,表明每一断块具有特定的耗散结构。这是地壳下部与上地幔进行能量传递、转换过程的渠道。它主要取决于上地幔热流及向横不均匀性。热震能流约占地表大地热流2%±。本文根据等效原理,探讨构造力和热应力对板内地震孕育及破裂机制联合作用问题。提出“菱形”断块的周边的深断层端点、拐点是易于热破裂有利场所,并可能存在曼森—科芬效应导致深部岩石热疲劳和弹性破裂——发生地震。说明研究热震效应是具有理论和实用价值的新课题。

The present paper uses on-the spot recondings in Zhangzhou area provided by mieroearthquake station net of 1982, makes a comprehensive analysis on seismic data over the years, and gives a fundamental outline of recant stress field of South Fujian derived from the results of focal mechanism and microseismic synthetic mechanism explanation, It is also dealed with that the following respects are as follows:1. Recent tectonic stress field of South Fujian has different characteristics in the eastern and western parts...

The present paper uses on-the spot recondings in Zhangzhou area provided by mieroearthquake station net of 1982, makes a comprehensive analysis on seismic data over the years, and gives a fundamental outline of recant stress field of South Fujian derived from the results of focal mechanism and microseismic synthetic mechanism explanation, It is also dealed with that the following respects are as follows:1. Recent tectonic stress field of South Fujian has different characteristics in the eastern and western parts of the area where the Putian-Shaoan fault belt serves as a boundary. There is EW principal compressive stress axis in sea area of the eastern part of South Fujian and SE and NW principal compressive stress axes in inland of the western part of South Fujian.2.Approaching recent activity ways and its mechanical behavior of the geological fault in this area.3.Discussing the distributed characteristics of thermal springs and the genetic relationship with the active fault, this paper puts the stress on studying and investigating Nanqing-Xiamen fault belt trending EW and NW structure within NE Putian-Shaoan fault belt when thermal resources are explorated in South Fujian.4.It is prosposed that the method of studying recent structural stress field is possibly applied to exploration for oil-gas bearing structures.

本文使用1982年微震台网在漳州地区的实地记录,并结合历年地震资料进行综合分析,以震源机制及微震综合机制解的结果。得出闽南现今构造应力场的基本轮廓。指出: 1、闽南现今构造应力场具有东西分区的特点,其分界线在莆田—诏安断裂带的滨海断裂一带。东部海域地区主压应力轴为东西向,西部内陆地区主压应力轴为南东—北西向。 2、探讨了各区地质断裂的现今活动方式及其力学性质。 3、讨论了闽南内陆众多温泉的分布特征及其与活动断裂的关系,提出在闽南勘探地热资源,应重点研究与解剖东西向南靖—厦门断裂带及北东向莆田—诏安断裂带内的北西向构造。 4、提出了以研究现今构造应力场的方法扩展去探索油、气储构造的设想。

The thermal spring is located in Shuimogou district of North-Eastern Urumqi. The parameters obtained by water quality analysis demonstrates that its H_2S, F, PO_4, H_3BO_3, HCO_3 + Na + Ca + Mg, Cl + Na + Ca + Mg con-tents exceed all the norme of medical mineral spring water promulgated byWHO. The analysis of various components' content shows that the thermalspring's heat resource is originated from deep layer magmatic column (room),belonging to the high temperature deep layer circulating hot water...

The thermal spring is located in Shuimogou district of North-Eastern Urumqi. The parameters obtained by water quality analysis demonstrates that its H_2S, F, PO_4, H_3BO_3, HCO_3 + Na + Ca + Mg, Cl + Na + Ca + Mg con-tents exceed all the norme of medical mineral spring water promulgated byWHO. The analysis of various components' content shows that the thermalspring's heat resource is originated from deep layer magmatic column (room),belonging to the high temperature deep layer circulating hot water whosetemperature reaches 187.3℃. At same time, the research is taken about cal-culating method of underground heat reserve's structure, extent, depth andvolume, and the volume calculated of its heat reserve is 8km~2.

水质分析数据表明水磨沟温泉具有医疗矿泉利用价值,文中对热储成因、水化学成份与温度之间、多种化学成份之间的关系作了分析,并对该区地热资源的计算方法作了探讨和计算,论证了进一步开发水磨沟温泉的可行性。

 
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