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deep-seated geothermal
相关语句
  “deep-seated geothermal”译为未确定词的双语例句
     They are respectively the cold water aquifer (depth < 2.2 km ), up per, middle and deep-seated geothermal water (depths are separately 2.2-3. 4 km, 3. 5 - 3. 9 km, > 4. 0km).
     2.2km以上为冷水层,2.2—3.4km、3.5—3.9km、4km以下分别为上部、中部和深部热水层。
短句来源
     Pressure transient response in deep-seated geothermal stress-sensitive fissured composite gas reservoir
     应力敏感裂缝性双区复合气藏压力动态特征
短句来源
  相似匹配句对
     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
     DEEP SEATED FLUID AND ITS METALLOGENY
     初论深部流体与成矿作用
短句来源
     2.deep-seated xenocryst;
     (2)深源捕虏晶;
短句来源
     What are the deep-seated causes for its existence?
     它存在至今的深层原因是什么?
短句来源
     DEEP-SEATED THETMOCOMVECTION AND PLATE MOVEMENT
     深部热对流与板块运动
短句来源
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The features of deep- seated fluid component and stable isotopic compositonsin Tianchi volcanic area indicate that there are four water - bearing formations of every description. They are respectively the cold water aquifer (depth < 2.2 km ), up per, middle and deep-seated geothermal water (depths are separately 2.2-3. 4 km, 3. 5 - 3. 9 km, > 4. 0km). The modern geothermal water activityall associat with strong deep- seated gas discharges. The ratios of the carbon andhelium stable isotopes suggest,...

The features of deep- seated fluid component and stable isotopic compositonsin Tianchi volcanic area indicate that there are four water - bearing formations of every description. They are respectively the cold water aquifer (depth < 2.2 km ), up per, middle and deep-seated geothermal water (depths are separately 2.2-3. 4 km, 3. 5 - 3. 9 km, > 4. 0km). The modern geothermal water activityall associat with strong deep- seated gas discharges. The ratios of the carbon andhelium stable isotopes suggest, these deep-seated gases were mostly derived fromthe mantle- derived magma. Among them there was a little air, and the contamination of the crust source gases was not important. And now the mass mantlederived gas discharges concentrate mainly around the Tianchi caldera lake. It is entirely possible to exist fixed hot mantle-derived magmatic reservoir in shallowcrust there. Based on the carbon isotope geothermometer, the top of magmatic reservoir is 5 km from the land surface in crust. The gas dynamic change moitoringsuggests, this hot magmatic reservoir is instable now, and must take the matterseriously.

天池火山区深部流体成分和稳定同位素组成特征指示,该区地下有相对独立的四个含水层。2.2km以上为冷水层,2.2—3.4km、3.5—3.9km、4km以下分别为上部、中部和深部热水层。现代水热活动均伴随强烈的深源气体释放,碳和氦同位素比值揭示,这些气体属幔源气体,其中仅混入少量大气,壳源物质混染不明显。大规模幔源气体释放主要集中在天池火山湖周围,这表明该区地壳浅部可能存在一定规模的热的幔源岩浆体。据碳同位素地质测温估算,该岩浆体的热变质带顶部距地面约5km。气体动态变化显示该岩浆体目前处在不稳定期,值得引起重视。

By means of studying the interaction of the water between meteorology, geology and biology and the circulating relation of the water between ocean, land and atmospheric layer, this paper discusses the regional environmental geology problems of Lingao Nuclear Power Plant, Guangdong, including the times of the pore - fissure water in weathering zone 0f the bedrock and the circulation, system and utilization of the regional medium and deep seated geothermal water, and concluds that the water is ineffective...

By means of studying the interaction of the water between meteorology, geology and biology and the circulating relation of the water between ocean, land and atmospheric layer, this paper discusses the regional environmental geology problems of Lingao Nuclear Power Plant, Guangdong, including the times of the pore - fissure water in weathering zone 0f the bedrock and the circulation, system and utilization of the regional medium and deep seated geothermal water, and concluds that the water is ineffective on transfering the polution resources of the nuclear power plant. In addition, the paper expounds the force source of the neotectonic movement and considers that the site of the nuclear power plant is stable and suitable because it is just located in the blank spot 0f the force source of the plate motion.

本文以水在气象、地质和生物间相互作用和海、陆、空循环关系,探讨了广东岭澳核电站区域环境地质问题。包括基岩风化带孔隙—裂隙水的时代归属问题.及区域中、深层地下热水循环、体系和开发利用问题、水对核电站的污染源,难起传输作用。本文还着重陈述了新构造运动力源。并认为核电站恰处板块作用力源空档区,因此较为稳妥而优越。

Yuzhong Basin is located in the middle part of Lanzhou Dingxi mesozoic cenozoic depression.Based on the preliminary study on the geothermal field and hydrochemistry of the Basin,it is found that there exists a close relationship between hydrochemistry and geothermal anomaly.Geothermal anomaly area and deep seated faults are determined. The results are essentially consistent with those from geophysical electrical sounding and drilling.It was further verified that there exist a structural...

Yuzhong Basin is located in the middle part of Lanzhou Dingxi mesozoic cenozoic depression.Based on the preliminary study on the geothermal field and hydrochemistry of the Basin,it is found that there exists a close relationship between hydrochemistry and geothermal anomaly.Geothermal anomaly area and deep seated faults are determined. The results are essentially consistent with those from geophysical electrical sounding and drilling.It was further verified that there exist a structural background situation of geothermety and a deep seated geothermal mechanism in Yuzhong Basin.

榆中盆地位于兰州—定西中新生代凹陷盆地的中部。为探求和寻找可供开发利用的地热资源 ,从 1999年春节开始 ,对榆中盆地地热形成机制进行了初步研究 ,5月开始进行地温、水化学的全面调查与实地测定。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。其形态、空间分布特征与后来物探电测深成果和钻探成果基本一致。证实榆中盆地存在地热构造背景条件和深热源机制 ,为进一步的地热勘探和地热资源开发提供了可靠依据。

 
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