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铜厂的英文

音标:[ tóngchǎng ]  发音:  
"铜厂"怎么读用"铜厂"造句

英文翻译手机手机版

  • copper works
  • hernan videla lira

例句与用法

  • Geology and origin of tongchang gold deposit in yunnan province
    云南金平铜厂金矿床地质特征和成矿物质来源
  • Generally magmatic hydrothermal cu and au deposits enrich cl and s , but w and sn deposits are rich f systems . in this paper , in order to study the relationship between the cu , w and
    本文以著名的江西德兴铜厂超大型斑岩铜矿床和大吉山钨矿床作为研究对象,研究f 、 cl与w 、 cu成矿的关系。
  • In this paper , the present produce situation on five plants is used as example , to explain the development level , investment , benefit and forecasts developing tread of this technology in china
    文章以5个铜厂的生产现状为例,对该工艺目前在中国的发展水平、投资、效益及发展趋势作了简单的分析。
  • ( 4 ) the trace elements and ree geochemistry of the tongchang granodiorite porphyry indicate , there exists the reaction between the porphyry and the hydrothermal fluid . the hydrothermal fluid was cl - enriched solution , and flowed from the porphyry center to contact zone
    ( 4 )德兴铜厂斑岩体微量元素和稀土元素地球化学特征表明,该岩体发生了流体?熔体作用,分异出来的流体是一种相对富氯的流体,同时成矿流体的流向是从岩体中心向接触带方向流动。
  • Log ( fh2o / fhcl ) fluid and log ( fhf / fhcl ) fluid ) , tongchang porphyry copper deposit system is enriched in chlorine , however dajishan tungsten deposit system is relatively enriched in fluorine , which transport w , sn , nb , ta , et al . ( 8 ) according to the characters of the porphyry copper deposits , copper is transported by chlorine , such as cucl0 and cucl2
    忍l ) flu , d 、 109 ( / hr州el ) fluid )发现,铜厂斑岩型铜矿床的成矿体系是相对富氯体系,而大吉山石英脉型钨矿床成矿体系相对富氟,同时氟可能主要迁移w 、 sn 、 nb 、 ta等金属元素。
  • This process was propitious to enrich , activate , transport the copper . in different alteration granodiorite porphyry , sio2 , k2o , cu , mo are depleted in the fresh and weakly altered rock , and are enriched in the strongly altered rock , cl is also enriched in the strongly altered rock . but na2o and fe are extracted from the porphyry into the ore - forming fluid , especially the presence of fe is in favor of cu deposition
    铜厂岩体不同的蚀变带中, sio _ 2 、 k _ 2o 、 cu 、 mo等从新鲜斑岩甚至弱蚀变带中带出,而在强蚀变带强烈富集, cl同样有在强蚀变岩石中富集的趋势;而na _ 2o 、 fe从斑岩体中带出,进入流体相中,流体中大量fe的存在,有利于铜的沉淀、富集成矿。
  • The heishishan anomalies better reflect the known dome and the baiyinchang anomalies are identical to xiaotieshan , zheyaoshan - huoyanshan , tongchanggou , lapaigou , and ganggou deposits ( or mineralization spots ) , meanwhile , the lijiadagou anomalies are situated in an unknown forecasting area where its mineralization background is similar to that of the formers
    黑石山异常较好地反映了已知的火山穹隆;白银厂异常则与已知的小铁山、折腰山?火焰山、铜厂沟、拉牌沟、缸沟矿床(点)吻合;而李家大沟异常位于具有与前者相似成矿地质环境的预测区,预测其下部存在着隐伏火山穹隆和矿床。
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