hydrothermal solution meaning in Chinese
热水溶液
热液溶解作用
水热溶液
Examples
- The study covers regional stratigraphy , regional geological structures and their evolution ; deep - large fracture system and building - moutain straps in the basin ; distributing of mineralization concentration area and mineralazition characteristics of different metal fields ; volcanic magmatic activity and magmatic distributing ; the petrology , element geochemistry features of the magmatic rock series ; the relationship between magmatic distributing and mineralization ; the relationship between magmatic forming - age and mineralization ; the relationship between magmatic form and mineralization ; source of mineral materials , source of hydrothermal solution and source of mineralizing agent ; transport forms of metal in the solution ; the ore - forming geochemical mechanism , etc . it turns out as follows : ( 1 ) lanping basin formed in the linkup of the plates and it was propitious to form deep - large fracture
研究内容包括：区域地层及区域构造演化；盆地深大断裂系统及造山带；区域地球物理场；矿集区矿床的时空分布、矿化特征；岩浆岩活动与岩浆岩分布；岩浆岩岩石学特征；岩浆岩元素地球化学特征；岩浆岩分布与成矿的关系；岩浆岩成岩时代与成矿的关系；岩浆岩组成与成矿的关系；成矿物质的来源，成矿流体的来源；成矿物质搬运、富集的地球化学机理等。研究结果表明：兰坪盆地发育于板块的拼接地带，有利于发育深大断裂系统。 - The charac teristics of homogenization temperature and salinity data also reports that this high - salinity inclusions were not generated by aqueous fluid immiscibility or boiling in ore - forming processes , but generated directly from a water - saturated crystallizing magmatic melt and that the main mechanism of ore deposition is the mixing of magmatic fluid and underwater not boiling of hydrothermal solution
均一温度和盐度特征还表明，高盐度包裹体不是由热水溶液的不混溶作用或沸腾作用形成的，而是由岩浆熔体直接分离的卤水形成的；沸腾作用对矿质沉淀的作用不大，而流体的混合作用是银山矿床矿质沉淀的主要机制。 - On the basis of this , the paper specially discusses the ore precipitating mechanism and the ore origin . fluid - inclusion observations and microthermometric data suggest that the ore - forming fluid is middle - low temperature hydrothermal solution , it also reports the presence of high - salinity inclusions containing hilite in porphyry rock and ore - hosted quartz vein
流体包裹体岩相学和显微测温学研究表明，银山矿床成矿流体属于中低温热液范畴，在石英斑岩和多金属矿脉中都发现有含石盐子矿物的高盐度流体包裹体。 - By applying the theory and method of geological anomaly , it is focused on the analysis of the characters of major geological anomalies and their effect of mineralization in daye - jiurui region . the analysis result shows that the basement fault anomalies control a few major large hidden batholiths and their associated orefields ; that the anomalies of cover structure confine most cu - au deposits and fe - cu deposits within their scope ; that the geochemical anomalies and lithofacies - paleogeographical anomalies are major geological factors leading to trataboundness of some cu - au deposits ; that the anomalies of rock operties provide the favorable chemical and physical conditions for the ore - forming process , including the seepage , circulation , convergence and deposit of ore - bearing hydrothermal solution ; that the anomalous ctive stage of mesozoic magmatite is almost consistent with the major mineralization epoch of the fe , cu deposits , and the structure of multi - levels , and the zoning in magmatic system determine the spatial distribution of the mineralization system . then , based on the above analysis , a comprehensive variate , geological combination entropy , is brought forward for reflecting the complex degree of the combination of geological ore - controlling factors . after circumscribing the anomalies of geological combination entropy , the relations between the anomalies and ore deposits are determined
从地质异常的角度，重点分析了大冶九瑞地区主要地质异常的特征及其对成矿的影响.由分析可知：基底断裂异常控制了本区若干重要规模较大的隐伏岩基及伴生矿田，而盖层构造异常控制铜金矿床和铁铜矿床的空间位置；地层的地球化学异常和岩相古地理异常是造成一些铜金矿床层控性的主要地质因素；盖层的岩性异常为含矿热液的渗流、循环、聚集和矿质沉淀等一系列成矿作用提供了有利的物理和化学条件；中生代岩浆岩的异常活动期也是本区主要的铁铜成矿期，岩浆岩系统的多层分枝和分带性结构控制了本区成矿系统的三维空间分布.在上述分析的基础上，构置了地质组合熵作为反映控矿地质因素组合系统结构复杂程度的综合变量，并圈定出组合熵异常，由此确定了综合地质异常与矿床的关系