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热液的的英文

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"热液的"怎么读用"热液的"造句

英文翻译手机手机版

  • hydatothermal
  • hydrothermal

例句与用法

  • By the time of yanshanian structural hydrothermal superimposed caused the ore - forming chemical element of the pyritization sources activated , it results from the elements had been moving and expected turning into minerals in the beneficial structural position
    经燕山期构造热液的叠加,驱使矿源层中的成矿元素活化、迁移,在有利的构造部位富集成矿。
  • Now , sr isotopes can be used not only to constrain the origin and evolution of magma and hydrothermal ore - forming solutions , calculate the scale and degree of lithogenesis and ascertain the relations between fluids and rocks , but also to study sea - level fluctuation , plate movement , ocean - floor spreading and lithogenic evolution
    现在,锶同位素不仅在示踪岩浆及成矿热液的来源和演化、计算晚期成岩改造作用的规模和程度及流体/岩石比等方面已趋于成熟,并且越来越广泛运用于海平面变化、板块活动、海底扩张、成岩演化等方面的研究。
  • 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
  • The hydrothermal activities which were complicated and acted a positive effect in the formation of the zhulazaga gold deposit resulted in hydrothermal alterations of multiepisode , including pyroxeneization , actinolitization , epidotization , ice - feldsparization , silicification , chloritization and carbonatization etc . the research on inclusions in quartz of the ore indicates that the hydrothermal fluid varying greatly in temperature with an average of 286 shows characteristics of high temperature
    3 、朱拉扎嘎金矿的形成中热液活动起到了积极的作用,热液活动不仅复杂而且具多期性,有透辉石化、阳起石化、绿帘石化、绿泥石化、硅化、冰长石化、碳酸盐化等。矿石中石英包裹体的研究表明,含矿热液的温度变化范围较宽广,平均在286 ,显示中偏高温特征。
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