地热流体

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 .

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

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 .

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

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

地热流体阳离子组份以Na+为主。

Geothermal fluid cationic component of Na + - based .

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

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

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 .

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

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 .

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

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

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 .

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 .

地热流体成矿作用分析

An analysis of geothermal fluid mineralization

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 .

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 .

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

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 .

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

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 .

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 .

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 .

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 .

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 .

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 .

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 .

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 .

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 .