熱液溶解作用；[地質] 熱水溶液
The hydrothermal solution from the magma is proved to be an important factor ior ore-formation.
來自岩漿熔體的熱水溶液是導緻成礦的重要因素。
The boundary of precious metal and metal sulfide mineralizations is normally correspondent with the level of episodic boiling of the hydrothermal solution.
貴金屬和金屬硫化物礦化帶的分界線，通常是熱液在成礦作用過程中發生沸騰的部位。
This paper made a new exploration on geochemical characteristic, migration form and enrichment conditions of gold in hydrothermal solution of Erze Gold Deposit.
描述耳澤金礦熱液的地球化學特征及其遷移形式、富集條件，提出納米金合金遷移的新機制。
Potassium is one major component of gold-bearing hydrothermal solution.
鉀是含金熱液最主要的組分之一。
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.
研究表明南和溝銅礦床受剝離斷層和變質熱液兩重成礦作用控制，具有多因成礦特征。
Uranium contents in the country rocks close to the contact zone increase significantly under the influence of postmagmatic hydrothermal solution.
緊靠接觸帶的固岩，由于受岩漿期後熱液的影響，鈾含量明顯增高。
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.
成礦物質，主要來源于深部富鈾花崗岩漿冷凝結晶分異時産生的富鈾岩漿期後熱液。
Hydrothermal solution is derived from mixture of meteoric water with deep-source water.
熱液水來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.
成礦熱液來源是變質熱液，礦質來源于礦源層，礦源層的成礦元素來源于地幔。
Hydrothermal solution sediment differs from the common sediment and is mainly related to hydrothermal fluid type.
熱水沉積物不同于普通沉積物，主要與熱水流體類型有關。
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.
綜合研究結果認為韓旺條帶狀鐵礦具有與火山熱液伴生的鐵質，形成于海洋化學沉積環境。
The hydrothermal anhydrite with 28% of facial porosity factor is a favorable deep reservoir and proves the existence of deep hydrothermal solution.
這種熱液型硬石膏，面孔率達28%，是深部有利的儲層，同時也是深部熱液存在的證據之一。
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，推斷甲馬礦床層狀矽卡岩的形成與岩漿熱液沒有直接的成因聯繫，而很有可能是與盆地演化過程中的熱（鹵）水活動有關。
In hydrothermal solution, gold is activated and migrates in the form of hydride, carbonyl compound, nanometer particle, and nanometer alloy.
在熱液中金呈金氫化物、金羰基化合物及納米金粒子、納米金合金粒子活化遷移。
By means of stable isotope research, metallogenicmaterials and hydrothermal solution came mainly from magmatic hydrothermal solution which was homologous to diabase.
通過穩定同位素研究，成礦物質和成礦熱液主要來源于與輝綠岩同源的岩漿熱液。
The mineralization was formed by filling metasomasis of the Upper Silurian volcanic hydrothermal solution, and superimposition reformation of the Hercynian magmatic hydrothermal solution.
礦化過程經曆晚志留世火山熱液充填交代作用和海西早期岩漿熱液的疊加、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，成礦熱液來源于大氣降水。
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—瑞麗地區南部的上芒崗金礦為該區新發現的構造蝕變岩型金礦，金源、構造、熱液蝕變是主要的控礦因素。
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.
閃鋅礦和黃銅礦交生形成的”黃銅礦病毒”結構通常被解釋為由富銅熱液交代閃鋅礦形成。
The Glod-bearing hydrothermal solution moves up with the activies of early Cretaceous terminalvolcano-magma, and deposits in the favorable places.
早白垩紀晚期的火山—岩漿活動為深部含金熱液的運移提供了通道，并在其有利的構造部位沉澱成礦。
Various data demonstrate that ore-forming material of the Shaxi porphyry copper (gold) deposits came mainly from magmatic hydrothermal solution.
各種數據資料證明沙溪斑岩銅（金）礦床成礦物質主要來自岩漿熱液。
The gold deposit of Jinshan is metamorphic hydrothermal solution type which is controlled by the ductile shear belt.
“金山式”金礦床屬于受韌性剪切帶控制的變質熱液型金礦床。
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.
鈾的形成主要與天然氣的運移和逸散有關，也可能與後生階段的熱液活動有關。
The metallogenetic substance is derived mainly from postmagmatic hydrothermal solution, secondarily bound up with wall rock and dike rock.
成礦物質主要來自岩漿期後熱液，其次與圍岩、脈岩等關系密切。
As for the minerogenic substances, there are such different source ideas as magmatic hydrothermal solution, migmatitic (migmatized) hydrothermal solution, etc.
對于該礦的成礦物質來源，有岩漿熱液、混合岩化熱液等不同認識。
A chemical model for activation, migration, precipitation and enrichment of silver in hydrothermal solution and in supergene conditions has been established.
建立了在熱液和表生條件下銀的活化、遷移、沉澱、富集的化學模式。
The posttraumatic hydrothermal solution is the principal source of ore-forming fluid.
斷裂和岩漿岩是兩大重要的成礦地質條件。
熱液（hydrothermal solution） 指地球内部（主要在地殼中）受熱驅動并循環流動的、富含礦物質的熱水溶液。它是地質作用中物質遷移和礦床形成的關鍵媒介。以下是詳細解釋：
術語構成與基本含義
因此，“hydrothermal solution”直譯為“熱水溶液”，特指地質背景下高溫的熱水流體。
形成與來源
熱液主要源于：
這些水在地下深處（通常數公裡）被加熱（溫度範圍從幾十攝氏度到超過600°C），并在高溫高壓環境下溶解圍岩中的礦物質（如金屬、矽、硫化物等），形成富含化學物質的熱液。
關鍵特征
地質作用與意義
熱液是多種重要地質過程的核心：
科學意義
研究熱液對于理解地球内部物質循環、元素富集機制（礦床成因）、地熱資源開發、海底極端環境生命起源與演化以及行星（如火星）地質曆史都具有重大意義。
來源參考：
（注：由于未能獲取到可直接引用的、與用戶問題完全匹配且内容詳實的單一權威網頁鍊接，以上解釋綜合了地質學領域的共識性知識。建議查閱專業教科書或通過學術數據庫檢索相關文獻以獲取最詳盡和前沿的信息。）
“Hydrothermal solution”是地質學和地球科學中的專業術語，通常指高溫、富含礦物質的熱水或熱液流體。以下是詳細解釋：
如需進一步了解具體案例（如海底熱液生物群落或礦床形成機制），可參考地質學或海洋科學專業文獻。
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