地热流体
- 网络Geothermal fluid
![地热流体](../cache/969001.jpg)
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克热1井地热流体为HCO3·Cl-Na型、弱碱性水、淡水。
G hot wells geothermal fluid HCO3 · CI-Na-type alkaline water , freshwater .
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天津附近奥陶系地热流体成因与补排分析
Analysis of causes and recharge-discharge of Ordovician geothermal fluid in Tianjin area
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例子B是意大利一个电站利用低温地热流体的流程示意图。我想了解下学期有关意大利语课程的一些信息。
The schematic flow of low temperature geothermal fluids through a power station in Italy is presented in example B. I 'd like some information about Italian courses next term .
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沉积盆地热流体活动及其成藏动力学意义
Thermal Fluid Flow in Sedimentary Basins and Its Significance to Pool-forming Dynamics
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地热流体气相成分对构造环境的指示作用
Composition of gases in geothermal fluids as an indicator of tectonic setting
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地热流体阳离子组份以Na+为主。
Geothermal fluid cationic component of Na + - based .
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云南腾冲地区现代地热流体活动类型
Active types of modern geothermal fluids at the Tengchong region , Yunnan Province
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云南腾冲地区地热流体的地球化学特征
Geochemical characteristics of geothermal fluid in Tengchong Area , Yunnan Province , China
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腾冲地区存在两类地热流体活动。
In the Tengchong region , there exist two kinds of active geothermal fluids .
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河南省鹤壁市新区地热流体特征及成因分析
Features and origin of geothermal fluid in the new district of Hebi , Henan
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地热流体中一些组分的浓度依赖于热流体温度的高低。
The content of some components of geothermal fluid are highly dependent on temperature .
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奥陶系高矿化度地热流体在天津地热开发利用中的分析
The analysis of Ordovician high salinity development and utilization of geothermal fluid in Tianjin
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天津市奥陶系热储层地热流体水化学特征及其主要影响因素
Hydrochemical Properties of Geothermal Fluids in Ordovician Reservoirs of Tianjin and Main Affecting Factors
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地热流体及其循环蚀变作用导致银矿、钠基膨润土矿等系列矿产的形成,并建立了矿床成矿模式。
A metallogenic model of the ore deposits has been set up in this paper .
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区内其它地热流体活动多属构造活动成因。
Other geothermal fluids are all generally the thermal discharge caused by the tectonic activity .
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地热流体成矿作用分析
An analysis of geothermal fluid mineralization
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因此,地热流体的化学监测可以提供许多有关地热系统变化的宝贵信息。
Therefore , chemical monitoring of geothermal fluid may give important information about the changes of geothermal systems .
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从而为合理开发利用地热流体资源提供了地质依据。
These may provide a geological basis for the proper development and utilization of the geothermal fluid in this district .
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莺&琼盆地热流体活动示踪标志及其油气运聚指向意义
Trace markers of thermal fluid flow in ying & qiong basin and their directional significance of hydrocarbon migration and accumulation
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在水平方向上地热流体自北东向南西矿化度逐渐增高,水质渐趋复杂。
TDS values of geothermal fluids gradually increase horizontally from northeast to southwest , with the water types becoming increasingly complex .
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莺歌海盆地热流体上侵活动与天然气运聚富集关系探讨
Geotemperature field and up - welling action of hot flow body and its relationship with natural gas migration and accumulation in Yinggehai Basin
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王4井的地热流体正是具备了合适的水化学条件,同时伴随着有利的水动力条件才生成了我们所看到的钙华。
So , the appropriate geochemical condition and the advantaged water dynamic condition compose the growth of the tufa of Wang 4 well .
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目的查明西安地热流体中气体的基本组成和特征,探讨其理论和经济意义。
Aim Detecting the elementary composition and features in the natural gas in Xi ′ an geothermic fluid , and researching it ′ s theoretical and economic significance .
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区域性深大断裂是沟通天水和地热流体的主要通道,次级断裂是矿体的储矿构造,脆性粗碎屑岩和火山碎屑岩(沉积火山岩)构成的断裂构造岩是主要的容矿岩石。
Regional deep-fault is the main pathway for meteoric water and geothermal fluids , subsidiary fracture is ore depositing structures , and fault tectonite are the main host rocks .
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利用抽水试验、地热流体质量分析、动态监测等勘查手段,查明地热资源分布、储量、品质及开发利用条件。
Using pumping tests , quality analysis of geothermal fluid , dynamic monitoring of exploration means to identify conditions of distribution , storage , quality and utilization of geothermal resources .
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根据热流体活动的主要输导通道的差异,将莺-琼盆地热流体划分为侧向对流型、垂向对流型和侧向-垂向对流复合型;
According to the difference of main migration channels the thermal flow of the basin can be divided into three types : the lateral convection type , the vertical convection type and the compound type of lateral-vertical convection .
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地热流体的碘、溴、偏硅酸、偏硼酸均达到矿水浓度,氟达到有医疗价值浓度,适合医疗热矿水开发,适合洗浴。
Geothermal fluid , iodine , bromine , silicic acid and borate are up to the concentration of mineral water , fluorine reach the concentration of medical value , suitable for the development of medical thermal mineral water suitable for bathing .
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根据羊八井地热水成矿作用特点和矿化分布规律,提出成矿区主要位于地热流体卸压排泄系统成矿的论点,并建立了羊八井盆地地热水系统成矿概念模型。
Sulfur mineralization took place mostly at places where the geothermal heat fluids could release pressure to move , an argument that is based on knowledge of the mineralizing features and distribution and on establishment of a metallogenetic model for the geothermal system .
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其众多的热液系统不断的向地表释放地热气体和流体。
As a result , Kamchatka has numerous hydrothermal systems , which constantly release geothermal gases and fluids out to the earth surface .
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滑石的成因模式主要有两类:一为与岩浆热液有关的热液交代成矿模式,另一是起源于盆地热卤水的变质流体交代成矿模式。
One is hydrothermal metasomatism related to magmatic-derived fluids and another is hydrothermal replacement of metamorphic fluids that possibly derived from formation brines .