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   geothermal fields 在 地质学 分类中 的翻译结果: 查询用时:0.011秒
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geothermal fields
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  地热田
    Based on the data derived from the selected typical geothermal fields in Iceland, CO2, H2S, H2, CO2/H2 and H2S/H2 gas geothermometers were used to calculate reservoir temperature. The factors disturbing accuracy of gas geothermometers were discussed in detail. It is suggested that CO2 and H2S geothermometers may give good results.
    基于冰岛部分地热田的实际资料,选择有代表性的、不同温度的地热田,应用 CO_2、H_2S、H_2、CO_2/H_2和 H_2S/H_2气体地热温度计计算热储温度,深入探讨了影响温度计准确性的各种因素,提出 CO_2和 H_2S 温度计具有良好的实用价值。
短句来源
    Active Faults and Geothermal Fields in the Taupo Volcanic Zone,New Zealand
    新西兰陶波火山带的活动断裂与地热田
短句来源
    DISTRIBUTION AND FORMATION OF GEOTHERMAL FIELDS IN TENGCHONG AREA YUNNAN PROVINCE
    腾冲地热田的分布及形成特征
短句来源
    CHARACTERISTICS OF GRAVITY AND MAGNETIC ANO-MALIES OP GEOTHERMAL FIELDS IN LUOYANG,XINJIANG AND XIAXIANG
    洛阳、新绛、夏县地热田的重磁异常特征
短句来源
    Geothermal fields and high temperature fumaroles in Tengchong hydrothe-rmal active area and their hydrothermal mineralization are all closely relatedto volcanic eruptions.
    腾冲水热活动区的地热田及其高温喷气、水热矿化等现象都与火山喷发活动密切相关。
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  地温场
    (2) The time that hydrocarbon source rock enters mature threshold in this area is different obviously from 5Ma to 20Ma, because there have been different geologic back-grounds in terms of various geothermal fields and tectonic rates of subsidence;
    该区在不同地温场和不同构造沉积速率的地质背景下,烃源岩进入成熟门限所需的时间有明显差别,从5~20Ma不等;
短句来源
    Comparison of regional geothermal fields and analysis of organic geochemistry exhibited thermal evolution characteristics of organic matter in each fault depression, established hydrocarbon generation model, and summarized the extent of oil formation zone and hydrocarbon generation potential of source rock in three different fault depression of Erlian rift system. Furthermore, it is pointed out that Ⅰ type fault depression enriched in oil is the most favourable target for oil/gas exploration.
    通过区域地温场的对比和大量的有机地化资料分析研究,明确了各断陷有机质热演化特征,建立了断陷群烃源岩有机质的热演化生烃模式,总结归纳出二连裂谷系三种类型断陷烃源岩的成油带长度及生油气潜力,指出Ⅰ类断陷为含油断陷,是二连裂谷断陷群中最有勘探前景的断陷。
短句来源
    Such hydrocarbon dis- tribution pattern is clearly different from that generated slowly in normal geothermal fields,whieh shows symmetrical distribution with balanced light and heavy hydrocarbons.
    与正常地温场缓慢生成烃类的轻、重烃平衡、对称的分布模式明显不同。
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  “geothermal fields”译为未确定词的双语例句
    A PRELIM DISCUSSION ON THE REGIONAL GEOLOGICAL STRUCTURE IN FUZHOU—YONGTAI AREA AND ITS CONTROL TO GEOTHERMAL FIELDS
    福州—永泰区域地质构造及其对热田控制作用的初步探讨
短句来源
    The characteristics of gravity, magnetic and geothermal fields in Qaidam basin are analyzed. According to the information of geophysical field, the basin's sedimentary structure, regional structural framework and deep geologic feature are discussed, providing scientific bases for the petroleum exploration, widening applied domains of non-seismic geophysical information.
    分析了盆地重力场、磁场和温度场特征,根据地球物理场信息探讨了盆地沉积构造、区域构造格架和深部地质特征,并与塔里木盆地、准噶尔盆地的地球物理场进行了对比,为油气勘探部署提供了科学依据,拓宽了非地震地球物理信息的应用领域,而且对其它含油气盆地的综合地质与地球物理研究和油气勘探部署也有借鉴作用,同时也有助于区域大地构造和盆地对比研究。
短句来源
    A FRELMINARY STUDY OF GOLD MINERALIZATION INHIGH-TEMPERATURE GEOTHERMAL FIELDS
    高温热田上金矿化的初步研究
短句来源
    Strontium isotope data for thermal waters in selected high-temperature geothermal fields, China.
    中国典型高温热田热水的锶同位素研究
短句来源
    As there are much differences in geothermal fields,the sourcethreshold would be controlled by sedimentary units in minor sags.
    其生油门限因块断湖盆地温场差异性大,又为小洼陷沉积单元所控制。
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  geothermal fields
The geothermal fields monitored in the study were, from west to east, Yalova, Efteni, Bolu, Mudurnu, Seben, Kur?unlu-?ank?r?, Hamam?zü, G?zlek and Re?adiye.
      
Such a mechanism is possibly significant under high-temperature conditions at geothermal fields because of temperature enhancement on chemical reactions for the sealing.
      
The locations of geothermal fields therefore appear to be influenced by plate geometry and correspond to lateral breaks in the continuity of the underthrusting plate.
      
A preliminary analysis, however, suggests that these geothermal fields are not situated along entire segments of plate boundaries but only at certain locations.
      
A number of geothermal fields explored so far in the circum-Pacific area occur along spreading ridges and subduction zones in areas of young tectonism and volcanism.
      
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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...

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。

On the basis of geothermal data from 133 wells in the Dongying depression collected, systematized and analyzed, the regional geothermal gradient is determined as 3.6℃/100m. The fundamental features of its geothermal field are discussed in the paper. It is pointed out that the variation of geothermal gradient can basically be divided into four vertical sections. They are mainly caused by the difference of thermal conductivity of rocks. The distribution of geothermal anomalies is...

On the basis of geothermal data from 133 wells in the Dongying depression collected, systematized and analyzed, the regional geothermal gradient is determined as 3.6℃/100m. The fundamental features of its geothermal field are discussed in the paper. It is pointed out that the variation of geothermal gradient can basically be divided into four vertical sections. They are mainly caused by the difference of thermal conductivity of rocks. The distribution of geothermal anomalies is obviously controlleed by regional tecto-nics and large faults, and is closely related to the relief of basement. Based upon the terminal threshold temperature of oil generation, a prediction of the lower limit of depth of oil distribution is made. It is believed that the dep-ression may hold great potiential for oil and gas exploration at depth.

本文收集、整理和分析了东营凹陷133口井的地温资料,由此确定的区域地温梯度值为3.6℃/100米。文中论述了东营凹陷地温场的基本特征。指出地温梯度的变化在纵向上大致可划分为四段,这主要是由于岩石热导率的差异而造成的;地温异常在平面上的分布明显地受到区域构造和大断层的控制,并与基底起伏密切相关。文中根据本区生油终止门限温度对石油分布的下限深度进行了预测,认为本区深部尚有相当大的油气潜量可供勘探。

As a part of a platform before the Indo-Chinese Movement, the Xiangzhong region in the central part of Hunan province was reduced to a depressed area following the violent tectonic activities during the Meso-Cenozoic time. Marine carbonate rocks constitute the main body of upper Paleozoic rocks of the region, with the organic carbon content corresponding to gam-ma distribution and a fairly low average value. Before the Indo-Chinese Movement, the normal geothermal field and the time of burial were the principal...

As a part of a platform before the Indo-Chinese Movement, the Xiangzhong region in the central part of Hunan province was reduced to a depressed area following the violent tectonic activities during the Meso-Cenozoic time. Marine carbonate rocks constitute the main body of upper Paleozoic rocks of the region, with the organic carbon content corresponding to gam-ma distribution and a fairly low average value. Before the Indo-Chinese Movement, the normal geothermal field and the time of burial were the principal factors that controlled the transformation of organic matter, but since then, tectonic deformation and magmatism played the dominant role. Due to the high level of evolution of organic materials in late Paleozoic, the authors propose that exploration of gas pools should be main objective of this region.

湘中地区在印支运动以前是一个地台的一部分,中新生代强烈活化而成为地洼区。海相碳酸盐岩组成本区上古生界的主体,其有机碳丰度数据符合伽马分布,平均值较低。正常地温场和埋藏时间在印支运动以前是控制有机质演化进程的主导因素,但从印支运动以来,构造变动和岩浆活动对这一进程的影响十分明显。因为上古生界有机质的演化水平很高,地质工作的重点应该摆在气藏的普查勘探方面。近三年来,由于油气资源定量预测工作的需要,我们以中泥盆统棋梓桥组至下石炭统石磴子组的碳酸盐岩为重点,对湘中地区的上古生界(图1)进行了野外调查和室内研究。本文试图对控制本区上古生界碳酸盐岩油气生成过程的内因和外因,进行初步分析。

 
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