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deep geothermal
相关语句
  深部地热资源
     THE APPLICATION OF ELECTROMAGNETIC SOUNDING METHOD IN DEEP GEOTHERMAL INVESTIGATION
     电磁测深方法在深部地热资源调查中的应用
短句来源
     Based on the examples of controlled source audio-frequency magnetotellurics application, the paper discuses the problems of electromagnetic sounding in deep geothermal investigation.
     以可控源音频大地电磁测深应用实例,讨论电磁测深方法在深部地热资源调查中的应用问题。
短句来源
  “deep geothermal”译为未确定词的双语例句
     Study on boundary property of deep geothermal water field with ~(14)C method
     用~(14)C方法确定深部地下热水系统边界性质的研究
短句来源
     Application of bridge filter pipe to the deep geothermal well in plain area
     桥式滤水管在平原地热深井中的应用
短句来源
     On the basis of total 822 heat flow measurement in the continental area of China, the deep geothermal characteristics of lithosphere of the major tectonic units was studied, which includes the temperature at 40 km depth, the thickness of thermal lithosphere, the cumulated strength and effective elastic thickness (EET) of lithosphere and so on.
     根据中国大陆 82 2个实测热流数据 ,研究了中国大陆主要构造单元的深部地热特征 ,包括 40km深度的地温值、热岩石圈厚度、岩石圈累积强度和有效弹性层厚度 (EET)等 .
短句来源
     A TENTATIVE DISCUSSION ON THE APPLICATION OF THE DEEP GEOTHERMAL EXPLORATION METHOD IN BEIJING AREA
     深部地热勘查方法在北京地区应用的探讨
短句来源
     According to heat flow values and deep geothermal characteristics, three large scale thermo tectonic domains, i.e. Eastern, Central and Western domain, can be identified in the continental area of China.
     根据热流值和深部地热参数 ,中国大陆可以划分为东部、中部和西部三个大尺度热 构造区 .
短句来源
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  相似匹配句对
     DRILLING TECHNOLOGY USED IN DEEP GEOTHERMAL WELL
     深层地热水井钻探工艺
短句来源
     Geothermal anomaly area and deep seated faults are determined.
     结果 ,发现地球水化学与地温场存在密切关系 ,并依此确定了地热异常区和深部断裂构造。
短句来源
     The geothermal potential.
     可是具有良好地热田远景的区域。
短句来源
     the hypocenter is deep;
     震源较深;
短句来源
     Deep Autumn
     秋深
短句来源
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  deep geothermal
A Model for Deep Geothermal Brines,III: Thermodynamic Properties - Enthalpy and Viscosity
      
A Model for Deep Geothermal Brines, II: Thermodynamic Properties - Density
      
A Model for Deep Geothermal Brines, I: T-p-X State-Space Description
      
The dominancy of hydrogen-users strongly suggested that H2 plays an important role as a primary substrate in the microbial ecosystem of this deep geothermal aquifer.
      
The meteoric water falling at higher elevations percolates to the local groundwater system at a shallow level and flows to the deep geothermal system.
      
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Sepiolite is a kind of chain and layered silicate mineral containing water and enriched in magnesium, with its mineral veins generally being 2--3 centimeters in thickness. Its fibres are usually several centimeters long and may even reach over ten centimeters. Various sorts of analyses were carried out by the author, including differential thermography, infrared spectrometry, X-ray diffraction, scanning electron microscopy and chemical analysis, showing the composition to be SiO_2 56.16%, MgO 22.61% and H_2O~(±)17.88%....

Sepiolite is a kind of chain and layered silicate mineral containing water and enriched in magnesium, with its mineral veins generally being 2--3 centimeters in thickness. Its fibres are usually several centimeters long and may even reach over ten centimeters. Various sorts of analyses were carried out by the author, including differential thermography, infrared spectrometry, X-ray diffraction, scanning electron microscopy and chemical analysis, showing the composition to be SiO_2 56.16%, MgO 22.61% and H_2O~(±)17.88%. Following tectonic fragmentation, as a reset of dissolution, the original dolomitic marble concentrated and precipitated its magnesium ions to form the mineral called sepiolite.Sepiolite finds wide application in different: Purposes, being now used as ion exchanger, absorbent, catalyst and sludge material for deep geothermal and oil drilling.

海泡石是一种层链状硅酸盐,是含水富镁的粘土矿物。该区海泡石矿层厚度一股为2~3厘米,海泡石的单个纤维长一般为几厘米,有的长达十几厘米。笔者对海泡石作了差热、X射线衍射、红外光谱、扫描电镜和化学全分析。它的化学成分为:SiO_2 56.16%,MgO 22.61%,H_2O±17.88%。海泡石是由白云质大理岩经构造破碎、分解使镁离子集中沉淀形成的。海泡石的用途较广,可以作为离子交换剂、吸附剂、催化剂、地热和深部石油钻井中的泥浆原料等。

In 1986 and 1987 we have made low-frequency MTS in the eastern area of Fujian Province. The results are as following:1.An arising (i.e. diapiric structure) of asthenosphere was found in the upper mantle in both Fuzhou and Zhangzhou regions where lithosphere become thin and diapiric sub-structure exists at a depth of 20-30km. That means the geothermal activities are strong and hot springs connect with deep geothermal background thrre.2.There is a low-resistive zone with direction of N60°E from Huian to...

In 1986 and 1987 we have made low-frequency MTS in the eastern area of Fujian Province. The results are as following:1.An arising (i.e. diapiric structure) of asthenosphere was found in the upper mantle in both Fuzhou and Zhangzhou regions where lithosphere become thin and diapiric sub-structure exists at a depth of 20-30km. That means the geothermal activities are strong and hot springs connect with deep geothermal background thrre.2.There is a low-resistive zone with direction of N60°E from Huian to Longhai. Along the zone the geoelectrical structure is similar with that of the ocean crust. It is probably a suture of the old continent and the obducted oceanic crust.3.Two promising geothermal prospective areas were found in Yongchun and Tongan where the depths of highly conductive layers in the crust are obviously shallow. It is necessary to make more detailed investigation there.

1986年至1987年我们在福建东部做了深部大地电磁测深,取得以下主要结果: 1.福州、漳州两地区存在上地幔软流层的隆起(底辟),岩石层变薄,并有次级底辟发育于20—30km深度,说明地幔热活动强烈,两地热田有深部热背景. 2.惠安至龙海一线大致呈北60°东为一低阻断面,该断面的地下电性结构和洋壳地电结构相似,推测该断面是向上仰冲的古洋壳与陆缘的缝合线. 3.永春、同安地区壳内高导层埋深明显比其它地区浅,是有希望的地热远景区,需进一步做工作.

This paper introduces the concept of mantle heat flow and its calculation method; the structural model of the crust and the distribution model of radio-active heat source of rocks in Xiangshah area has been established, the mantle heat flow for the area is determined to be 38. 17mw/m~2. The study indicates that the Xiangshan area is of the deep geothermal features between the structurally stable and active areas. That is, Xiangshan area being in the state of quasi-stable.

本文介绍了地幔热流的概念及计算方法,建立了相山地区的地壳结构模型和岩石放射性热源分布模型;计算出相山地区地幔热流值为38.17mW/m~2;研究表明相山地区具有介于构造稳定区和活动区之间的深部地热特点,即该区为一构造准稳定区。

 
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