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geothermal area
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  地热区
     REGIONAL ANOMALY OF VERTICAL ELECTRIC SOUNDING IN THE GEOTHERMAL AREA OF THE NORTHEAST PART OF NORTH CHINA PLAIN
     华北平原东北部地热区垂向电测深区域异常研究
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     The Relationship between the Contents of Principal Altered Minerals and the Original Rocks in Tengchong Geothermal Area, Yunnan Province
     云南腾冲地热区主要蚀变矿物含量与蚀变母岩的关系
短句来源
     This paper mainly analyses the relations of the shallow geother-mal field to the local heat source, shallow groundwater action and structure in Zhangzhou geothermal area.
     本文主要分析了漳州地热区浅层地温场与局部热源、浅层地下水活动和构造的关系。
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     Exemplified by the Qixian geothermal area,this paper points out that the combination of the radon surveying method and the magnetic method is an effective means in search for geothermal resources.
     以祁县地热区为例,说明测氡法与磁法相结合是寻找地热资源的一种行之有效的手段。
短句来源
     In this paper, the general principle and the characteristics of bipole-dualdipole survey method, a rapid effective method in geothermal field which has been developed in recent years, are described, and some experiment results in the geothermal area in Yinshan, Hubei province are shown.
     本文阐述了近年才发展起来的一种快速、有效的地热田勘查方法——双极-双偶极法的基本原理、方法特点及其在湖北省英山地热区取得的实验效果。
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  “geothermal area”译为未确定词的双语例句
     Calculating geothermal water amount with the method of finite state mixed cell model in Tianjin geothermal area
     用有限混合网络模型计算天津地热田热水量
短句来源
     The result showed that land subsidence of geothermal area in Fuzhou city was mainly induced by the excessive extraction of geothermal water in the thesis.
     分析了地下热水历年水位、水量动态变化特征,并探讨地下热水与地面沉降的相关关系,结果表明过量开采地下热水是导致福州市温泉区地面沉降的主要原因。
短句来源
     The exploring depth in non anomalous geothermal area will reach to 2000 meter.
     随着经济技术条件的不断发展,大城市、经济发达地区的非地热异常型地热开发将会有快速的发展,2000m将成为非地热异常区的主要开发深度.
短句来源
     Two fault soil gas observation spots were set up at the Xiadian fracture in the east of Beijing and Houhaoyao geothermal area in Huailai,Hebei Province,during Nov. and Dec. ,1989,and components of fault soil gas,H2, Ar,CO2,CH4 ,Hg,etc.
     建立了两个断层气观测点,观测H_2、Ar、N_2、CO_2、Hg等断层气成分。
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     With the hydropower resources greatly exploited in Southwest of our country, to construct the big span underground powerhouse in the abnormal geothermal area is a new engineering geological problem which the hydroelectric station project meets.
     随着我国西南地区水电资源的大量开发,在地温异常地区修建大跨度地下厂房是水电站工程遇到的一个新的工程地质问题。
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  相似匹配句对
     In the area, J.
     这方面,J.
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     In Tianjin coastal area there are abundant in geothermal resources.
     天津市滨海地区包括塘沽、大港、汉沽三个地区。
短句来源
     Analyses on mechanism of geothermal origin in Tianjin area
     天津地区地热形成机理分析
短句来源
     In the study area .
     长期以来,在教师教育问题研究中,研究者们关注的是中小学教师的发展。
短句来源
     The geothermal potential.
     可是具有良好地热田远景的区域。
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  geothermal area
Full Moment Tensor Retrieval from Waveform Inversion in the Larderello Geothermal Area
      
Lichen biomonitoring of trace elements in a geothermal area (central Italy)
      
Two case studies were carried out, one in the Horniman Museum and its associated storage and study building, London, UK, and the other in the vicinity of a pulp and paper mill and geothermal area North Island, New Zealand.
      
The hydrothermal evolution of the Sengan geothermal area, Northern Honshu, was studied using fluid inclusion microthermometry.
      
No seasonal variations are observed for most of the acid aerosols in the geothermal area except that the types of hot spring affect the SO4-2 concentration nearby.
      
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Songliao Basin is characterited by a higher geothermal gradient and a higher heat flow.The average geothermal gradient is 42℃/km.The average heat flow is 1.443H FU.In this paper,main characteristics of geothermal field in Songliao Basin have be- en discussed.Relation between geothermal field and oil and gas bearing area have been studied.It is pointed out that higher geothermal gradient is in accord with main source bed in the stratigraphic section and higher geothermal area is approximately co- incide...

Songliao Basin is characterited by a higher geothermal gradient and a higher heat flow.The average geothermal gradient is 42℃/km.The average heat flow is 1.443H FU.In this paper,main characteristics of geothermal field in Songliao Basin have be- en discussed.Relation between geothermal field and oil and gas bearing area have been studied.It is pointed out that higher geothermal gradient is in accord with main source bed in the stratigraphic section and higher geothermal area is approximately co- incide with oil and gas bearing area.

松辽盆地具有高地温、高热流特征,平均地热梯度为42℃/公里,平均热流值为1.443HFU。文中论述了松辽盆地地热场的基本特征,探讨了地热场和油田区的关系。指出:在地层剖面上,高地热梯度段和主要生油层相一致;在平面上,高地温异常区和油田区相一致。

Based on the research of silica heat flow in Fujian, to discuss the main heat flow parameters (qr, A, D),the thermal regime of lithosphere in different depth was determined. Authors considered that in eastern Fujian, the silica heat flow was rather high, the thickness of lithosphere was thinner, the depth of Curie point was shallow (more than 27 km), thermal activity was more intensive, it was a weak positive anomaly geothermal area; but in the western Fujian, it was quite different, thermal activity was...

Based on the research of silica heat flow in Fujian, to discuss the main heat flow parameters (qr, A, D),the thermal regime of lithosphere in different depth was determined. Authors considered that in eastern Fujian, the silica heat flow was rather high, the thickness of lithosphere was thinner, the depth of Curie point was shallow (more than 27 km), thermal activity was more intensive, it was a weak positive anomaly geothermal area; but in the western Fujian, it was quite different, thermal activity was weaker. However, even in eastern Fujian, there are no condition for the formation of magmatic reservoir, hot dry rock or high temperature hydrothermal fields, so there is no anomalous heat source. The widespread springs are produced by the deep-seated circulation of ground water along the faults under a weak geothermal anomaly state.

本文由福建硅热流值研究出发,探讨了热流省参数(qr,A,D),并进而推算了岩石圈不同深度上的温度状态。笔者认为福建东部地区硅热流值偏高,岩石圈厚度较小,居理点深度较浅(大于27km)。热活动性较强,属微弱的地热正异常地区;而西部则反之,热活动性较差。然而,即使在闽东地区也不具备形成岩浆房、干热岩或高温热田的条件,无异常热源。广布的温泉是在微弱地热异常状态下,沿断裂通过地下木的深循环所造成的。

Temperature measurement is a direct method in geothermal exploration and the temperature measurement at shallow depth is a promising method because of its high efficiency and low cost. Since the geothermal field near the Earth's surface is liable to be affected by various disturbing factors such as daily and annual variations, the key point is to recognize and correct them. This paper focuses attention on the recognition and correction approaches of them The temperature distribution at shallow depth...

Temperature measurement is a direct method in geothermal exploration and the temperature measurement at shallow depth is a promising method because of its high efficiency and low cost. Since the geothermal field near the Earth's surface is liable to be affected by various disturbing factors such as daily and annual variations, the key point is to recognize and correct them. This paper focuses attention on the recognition and correction approaches of them The temperature distribution at shallow depth is the result of composite effect of the subsurface heat source. Therefore, the distribution of the heat source can be deduced in terms of shallow temperature anomalies. The calculated results of heat sources with simple shapes (e.g. horizontal infinitive cylinder and sphere) indicate that if the threshold of the geothermal anomaly is 1℃, then 100℃ heat source at 500m. Depth can be determined by the temperature measurements at 1m. In the same way, sources with the same size and same temperature at 800m can be detected by measurements at 10m. Although the above results are obtained in ideal conlitions, they can be taken as reference in practical work. The paper also describes the interpretation method and the geological significance of 1m by temperature measurement in prospecting for underground thermal water in the Zhangzhou geothermal areas.

测温法是寻找地热田的一种直接勘探方法,而浅层测温法则由于工作效率高、成本低是一种很有前途的勘探方法。但因近地表温度场易受日变、年变等各种干扰因素的影响,因此,区分与校正各种干扰因素是方法能否取得良好效果的关键。本文讨论了校正与区分各干扰因素的方法。地表浅层温度信息是地下热源状况综合作用的结果。因此,利用近地表温度异常可推断地下热源分布状况。通过对简单形状热源(无限长圆柱形和球形)计算表明:当取1℃作为可探测到的温度异常时,利用1米深测温可发现埋深近500米、温度100℃的局部热源,而利用10米深测温可探测到埋深近800米同样规模同样温度的局部热源。计算结果虽然是在理想条件下进行的,但对指导实际工作具参考价值。文章结合漳州地热区的实际资料说明解释方法及应用1米深测温勘察地下热水取得的地质效果。

 
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