热液溶解作用；[地质] 热水溶液
The hydrothermal solution from the magma is proved to be an important factor ior ore-formation.
来自岩浆熔体的热水溶液是导致成矿的重要因素。
The boundary of precious metal and metal sulfide mineralizations is normally correspondent with the level of episodic boiling of the hydrothermal solution.
贵金属和金属硫化物矿化带的分界线，通常是热液在成矿作用过程中发生沸腾的部位。
This paper made a new exploration on geochemical characteristic, migration form and enrichment conditions of gold in hydrothermal solution of Erze Gold Deposit.
描述耳泽金矿热液的地球化学特征及其迁移形式、富集条件，提出纳米金合金迁移的新机制。
Potassium is one major component of gold-bearing hydrothermal solution.
钾是含金热液最主要的组分之一。
Research work shows that mineralization of Nanhegou copper deposit is controlled by both peel fault and hydrothermal solution of metamorphic origin with polygenic ore forming characteristics.
研究表明南和沟铜矿床受剥离断层和变质热液两重成矿作用控制，具有多因成矿特征。
Uranium contents in the country rocks close to the contact zone increase significantly under the influence of postmagmatic hydrothermal solution.
紧靠接触带的固岩，由于受岩浆期后热液的影响，铀含量明显增高。
The mineralization material is mainly derived from rich in uranium postmagmatic hydrothermal solution which is from the cooling and crystal fractionation of rich in uranium granite magma.
成矿物质，主要来源于深部富铀花岗岩浆冷凝结晶分异时产生的富铀岩浆期后热液。
Hydrothermal solution is derived from mixture of meteoric water with deep-source water.
热液水来自天水和深源水的混合；
The source of the mineralizing solution is metamorphic hydrothermal solution. The mineral is from the source bed while the ore forming element of the source bed is from mantle.
成矿热液来源是变质热液，矿质来源于矿源层，矿源层的成矿元素来源于地幔。
Hydrothermal solution sediment differs from the common sediment and is mainly related to hydrothermal fluid type.
热水沉积物不同于普通沉积物，主要与热水流体类型有关。
A comprehensive study of Hanwang BIF shows that its ferruginous material was associated with volcanic hydrothermal solution and was formed in a marine chemical sedimentary environment.
综合研究结果认为韩旺条带状铁矿具有与火山热液伴生的铁质，形成于海洋化学沉积环境。
The hydrothermal anhydrite with 28% of facial porosity factor is a favorable deep reservoir and proves the existence of deep hydrothermal solution.
这种热液型硬石膏，面孔率达28%，是深部有利的储层，同时也是深部热液存在的证据之一。
So, the authors conclude that the stratabound skarn of the Jiama deposit has nothing to do with magma hydrothermal solution, and however, has likely something to do with the hot brine in the basin.
因此，推断甲马矿床层状矽卡岩的形成与岩浆热液没有直接的成因联系，而很有可能是与盆地演化过程中的热（卤）水活动有关。
In hydrothermal solution, gold is activated and migrates in the form of hydride, carbonyl compound, nanometer particle, and nanometer alloy.
在热液中金呈金氢化物、金羰基化合物及纳米金粒子、纳米金合金粒子活化迁移。
By means of stable isotope research, metallogenicmaterials and hydrothermal solution came mainly from magmatic hydrothermal solution which was homologous to diabase.
通过稳定同位素研究，成矿物质和成矿热液主要来源于与辉绿岩同源的岩浆热液。
The mineralization was formed by filling metasomasis of the Upper Silurian volcanic hydrothermal solution, and superimposition reformation of the Hercynian magmatic hydrothermal solution.
矿化过程经历晚志留世火山热液充填交代作用和海西早期岩浆热液的叠加、改造作用。
Oxygen isotope analyses show that the hydrothermal solution of the ore-forming stage was derived from the meteoric water.
氧同位素分析表明，成矿热液来源于大气降水。
Shangmanggang tectonic-altered rock type Au deposit is founded in south Lushui-Ruili region. The Au deposit is controlled by source bed, structure and hydrothermal solution.
滇西泸水—瑞丽地区南部的上芒岗金矿为该区新发现的构造蚀变岩型金矿，金源、构造、热液蚀变是主要的控矿因素。
The chalcopyrite disease texture of intimate intergrowths of chalcopyrite (Cp) and sphalerite (Sp) is commonly considered as the result of replacement of Sp by Cu-rich hydrothermal solution.
闪锌矿和黄铜矿交生形成的”黄铜矿病毒”结构通常被解释为由富铜热液交代闪锌矿形成。
The Glod-bearing hydrothermal solution moves up with the activies of early Cretaceous terminalvolcano-magma, and deposits in the favorable places.
早白垩纪晚期的火山—岩浆活动为深部含金热液的运移提供了通道，并在其有利的构造部位沉淀成矿。
Various data demonstrate that ore-forming material of the Shaxi porphyry copper (gold) deposits came mainly from magmatic hydrothermal solution.
各种数据资料证明沙溪斑岩铜（金）矿床成矿物质主要来自岩浆热液。
The gold deposit of Jinshan is metamorphic hydrothermal solution type which is controlled by the ductile shear belt.
“金山式”金矿床属于受韧性剪切带控制的变质热液型金矿床。
Generation of uranium was closely related to migration and escaping of natural gas and may be also relevant to hydrothermal solution activities during epigenesis period.
铀的形成主要与天然气的运移和逸散有关，也可能与后生阶段的热液活动有关。
The metallogenetic substance is derived mainly from postmagmatic hydrothermal solution, secondarily bound up with wall rock and dike rock.
成矿物质主要来自岩浆期后热液，其次与围岩、脉岩等关系密切。
As for the minerogenic substances, there are such different source ideas as magmatic hydrothermal solution, migmatitic (migmatized) hydrothermal solution, etc.
对于该矿的成矿物质来源，有岩浆热液、混合岩化热液等不同认识。
A chemical model for activation, migration, precipitation and enrichment of silver in hydrothermal solution and in supergene conditions has been established.
建立了在热液和表生条件下银的活化、迁移、沉淀、富集的化学模式。
The posttraumatic hydrothermal solution is the principal source of ore-forming fluid.
断裂和岩浆岩是两大重要的成矿地质条件。
热液（hydrothermal solution） 指地球内部（主要在地壳中）受热驱动并循环流动的、富含矿物质的热水溶液。它是地质作用中物质迁移和矿床形成的关键媒介。以下是详细解释：
术语构成与基本含义
因此，“hydrothermal solution”直译为“热水溶液”，特指地质背景下高温的热水流体。
形成与来源
热液主要源于：
这些水在地下深处（通常数公里）被加热（温度范围从几十摄氏度到超过600°C），并在高温高压环境下溶解围岩中的矿物质（如金属、硅、硫化物等），形成富含化学物质的热液。
关键特征
地质作用与意义
热液是多种重要地质过程的核心：
科学意义
研究热液对于理解地球内部物质循环、元素富集机制（矿床成因）、地热资源开发、海底极端环境生命起源与演化以及行星（如火星）地质历史都具有重大意义。
来源参考：
（注：由于未能获取到可直接引用的、与用户问题完全匹配且内容详实的单一权威网页链接，以上解释综合了地质学领域的共识性知识。建议查阅专业教科书或通过学术数据库检索相关文献以获取最详尽和前沿的信息。）
“Hydrothermal solution”是地质学和地球科学中的专业术语，通常指高温、富含矿物质的热水或热液流体。以下是详细解释：
如需进一步了解具体案例（如海底热液生物群落或矿床形成机制），可参考地质学或海洋科学专业文献。
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