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浊沸石的英文

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"浊沸石"怎么读用"浊沸石"造句

英文翻译手机手机版

  • aedelforsite
  • efflorescing zeolite
  • hypostilbite
  • lauminite
  • laumonite
  • lomomite
  • lomonite
  • lomontite
  • magnesiolaumontite

例句与用法

  • Formation of laumontite of the upper triassic yanchang group in ordos basin and its effect on reservoirs
    靖安油田上三叠系延长统浊沸石的形成及对储层的影响
  • The axi gold deposit ; laumontitization ; epithermal gold deposit ; geothermal fluid minerogenetic system ; west tianshan
    阿希金矿浊沸石化浅成低温热液型金矿地热流体成矿系统西天山
  • The preliminary study of laumontitization of axi gold deposit and paleogeothermal minerogenetic fluid system in west tianshan
    西天山阿希金矿浊沸石化与古地热成矿流体系统的初步研究
  • They changed the porosity characteristics of sandstone , engendering new benefit storing beds consisted with secondary porosity
    浊沸石矿物是长6砂岩中普遍的胶结物,它的形成与火山物质水化有关。
  • The distinctness of rock for deep clastic gas layers in songliao basin is laumontitization , sericitization and water - bearing property of illite , and extensive albitization
    摘要松辽盆地深层碎屑岩储气层在岩石矿物方面的特殊性在于浊沸石化、伊利石的绢云母化及其含水性和广泛的钠长石化。
  • The cementation of laumonite , calcite and chlorite , compact and pressure solution , as well as the dissolution of laumontite , feldspar are also of main factors which affect reservoir properties
    方解石、绿泥石、浊沸石的胶结作用、压实压溶作用和浊沸石、长石的溶解作用也是影响储集性能的主要因素。
  • The metallic mineral has very few content ( 1 % - 2 % ) , the mineral of ore is mainly of pyrite , chalcopyrite , limonite , aurum and electrum etc . the gangue mineral is composed of chalcedony , micro grained quartz , calsite , sericite , adularia , aragonite , chlorite , laumontite , pyrophyuite , kaolinite and so on , which show the typical mineral assemblage of epithermal
    矿石为典型少硫化物型,金属矿物含量极少( 1 - 2 ) ,主要有黄铁矿、黄铜矿、褐铁矿和自然金、银金矿等。主要脉石矿物有玉髓、微粒石英以及方解石、绢云母、冰长石、文石、绿泥石、浊沸石、叶腊石、高岭石等,属典型低温矿物组合。
  • Through field investigation , microscopic study , x - ray phase analysis and mineral infrared spectrum analysis , the authors determine the laumontitization had occurred widely in the axi gold field . according to the development of laumontitization and its relationship to mineralization , authors reveal that the laumontitization appeared mainly at the top and periphery to ore - bodies . it befallen at the edge of the geothermal fluid system or happened in the late stage of geothermal fluid system evolution , hence can be assigned as an indicator to prospect for epithermal gold deposit . the fluid causing laumontitization in the axi gold deposit is similar to those causing hot spring type gold deposit or in modern geothermal field . the fluidization of the axi gold deposit happened in carboniferous , showing the west tianshan is a good district for epithermal gold mineralization and preservation . so west tianshan is prospecting for exploring epithermal gold deposit
    通过野外考察显微镜下薄片鉴定x射线物相分析和矿物红外光谱等研究,确定了阿希金矿浊沸石化的普遍存在根据浊沸石化发生的规律及其与矿床形成的关系,确定浊沸石化主要见于矿体的上部和外围,发育在地热流体系统的边缘和演化晚期,可作为寻找浅成低温热液型金矿的标志之一。导致阿希金矿浊沸石化的流体性质与热泉型金矿成矿流体和现代地热田类似,流体作用发生在石炭纪,证明西天山地区具有良好的浅成低温热液型金矿的形成和保存环境,因此找矿前景较好。
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其他语种

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