同位素和包体资料表明成矿溶液主要为大气降水。
Meanwhile, the isotopic and inclusion data show that mineralizing solution is mainly meteoric water.
阐述了成矿溶液中的水主要来自大气降水的事实；
水成岩墙的存在对油气和其它成矿溶液的运移和储集具有重要意义。
The existence of neptunian dikes is of great significance in the migration and accumulation of oil and gas, and other diagenetic fluids.
通过氧同位素研究证明了成矿溶液的来源由早期岩浆水转变为晚期大气降水；
The isotopic composition of oxygen shows that the origin of the ore forming solution was turn from magmatic water in early stage to circulated meteoric water in later stage.
稳定同位素特征揭示了矿质来说从围岩中淋取；成矿溶液主要来源于大气降水。
The characteristics of stable isotope indicatedthat the ore-forming material was leached from the wall rocks ; and the ore-forming fluid wasmainly supplied by meteoric water.
电导度是溶液导电能力的相对尺度，电导度的大小能直接反映出成矿溶液的高低。
The electric conductivity is a relative ruler to the conductance of ore forming solution.
借助于电子顺磁共振、成矿溶液电导度和红外光谱方法对刺猬沟金矿区石英进行了分析。
The quartz is studied using an electron paramagnetic resonance (EPR), infrared spectrum (IR) and the electrical conductible degree of ore-bearing fluids.
成矿溶液为中等盐度的中性偏碱性水； 成矿作用是在低温、低压、弱氧化或弱还原条件下进行的。
The ore is formed in the conditions of low temperature, low pressure and weak oxidation or weak reduction.
橄榄岩像玄武岩一样和二氧化碳饱和溶液发生化学反应后能迅速生成矿物质，其中一些含有碳。
Like basalt, peridotite chemically reacts with carbon dioxide-saturated water to quickly form minerals, some of which contain carbon.
成矿流体是大气水和沉积地层水的混合溶液。
The ore -forming fluid is a mixed solution of the atmospheric water and sedimentary stratal water.
碳酸盐岩地区的重晶石矿床，是在浅层条件下，以岩溶地下热卤水溶液为介质，岩溶作用为主导成矿作用形成的。
Barite deposits in carbonate rock area forms under shallow condition with karst hydrothermal brine solution as medium and karstification as leading factor of mineralization.
它是在浅层条件下，以岩溶地下热(卤)水溶液为介质，岩溶作用为主导成矿作用形成的。
It is formed under the shallow layer conditions with hydrothermal (brine) solution, as medium and karstification as leading mineralization.
成矿早阶段以深源富碳流体为主，中阶段流体发生沸腾，晚阶段为盐水溶液。
The fluid-system was rich in CO_2 in the early stage, boiled in middle stage, and characteristic of water solution in late stage.
其成矿温度在90 ~ 300之间，成矿流体为低盐度的弱酸性弱堿性大气降水、海水和岩浆水的混合溶液。
The mineralization temperature is in a range of 90 ~ 300, and the mineralization fluid is a combination of slightly acidic - slightly alkalic precipitations, seawater and magmatic water.
其中高温高压下矿物在水中或者其它自然界常见溶液中的溶解性质则是研究成岩成矿作用最重要的基础资料之一。
The dissolution and precipitation of different minerals in water and other solutions under high temperature and high pressure are one of the basic data in the mine-water systems.
因此，矿物在溶液中的溶解与沉淀对于成矿作用具有重要的意义。
So, the dissolution and precipitation of minerals in the solutions during the mineralization processes are very important.
因此，矿物在溶液中的溶解与沉淀对于成矿作用具有重要的意义。
So, the dissolution and precipitation of minerals in the solutions during the mineralization processes are very important.
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