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热卤水的英文

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"热卤水"怎么读用"热卤水"造句

英文翻译手机手机版

  • hot brine
  • hot hydrothermal brine
  • thermal brine

例句与用法

  • Practical applications for heat flow measurements in ocean floors are the location of hot brines .
    洋底热流量测量的实际目的是圈定热卤水的位置。
  • The geochemical characteristics reveal that the metallogenic elements are derived from the subaqueous ore - bearing hot brine
    地球化学特征表明成矿物质由含矿热卤水提供,属热水化学沉积型矿床。
  • The mineralizing fluid in lanping - baiyangping area is deep circulatory thermal brine as a whole , the mineralizing matter mainly comes from deep , and the genetic type of the deposit belongs to the low - to - moderate - temperature hydrothermal silver polymetallic ore deposit related to nappe structures
    因此,兰坪白秧坪地区成矿流体总体为深部循环的热卤水溶液,成矿物质主要来源于深部,矿床成因类型属于与推覆构造有关的中低温热液银多金属矿床。
  • There are two series of cu , au deposits , the stratiformed deposits and the intrusive - related ones in the mineralization belt of the middle and lower reaches of the yangtze river area . comparative studies on forming geodynamic backgrounds , geological and geochemical conditions of the ore - forming systems have been undertaken in this paper . the stratiformed deposits were formed in hercynian period by submarine exhalation - sedimentation sedex of hot brine through the synchronous basement faults in a tensional environmental , and the intrusive - related deposits were formed in yenshanian in a tensional or a transitional period to tensional environment during the upper mantle doming by water - rock interaction and complex transport - chemical reaction dynamic processes , the ore - forming fluids were mainly magmatic water from melt - fluid partition and some meteoric water
    成矿流体系统形成的地球动力学背景及地质地球化学条件对比研究表明,赋存于石炭系中的层状铜金矿床是海西期拉张背景下热卤水沿同生断裂经喷流作用形成的海底喷流热水沉积矿床与燕山期中酸性侵入岩有关的铜金矿床是在上地幔隆起张性或向张性过渡背景下形成的,是中酸性岩浆经熔体流体分离作用形成的岩浆热液与大气降水混合,经水岩作用等复杂的输运和化学反应耦合过程的动力学产物。
  • From studies of these characteristics of structures , palaeontology , drilling , well logging , seismic profile , salt chemistry and lacustrine sedimentary system , it is recognized that the new characteristics occur in of section pukou and in huaiyiri sag , and the huge thickness of salt rocks is formed by the crust salt materials upwelling along deep fracture in the form of hot bittern and entering lacustrine basin in this area
    通过该区构造、古生物、钻井、测井、地震、盐岩化学及湖盆内沉积体系等特征的研究,认为淮阴凹陷浦口组二段和三段的沉积构造有其特殊性,巨厚的盐岩层是壳深部盐类物质沿深大断裂上涌以热卤水形式进入湖盆的结果。
用"热卤水"造句  
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