礦源 的英文怎麼說

中文拼音 [kuàngyuán]
礦源 英文
mineral resources
  • 礦 : 名詞1. （礦床） ore [mineral] deposit 2. （礦石） ore 3. （開采礦物的場所） mine
  • 源 : 名詞1. （水流起頭的地方） source （of a river）; fountainhead 2. （來源） source; cause 3. （姓氏） a surname
  1. The ore - forming material is mostly from volcanic rock, and sub volcanic rock provides the main thermal and some mineral materials. the ore - forming fluid is from meteoric water. as a result, it should be a kind of adularia - sericite type of epithermal gold deposit

    成礦物質主要來自礦區火山巖圍巖，次火山巖提供了主要熱源和部分礦源，成礦流體來自大氣降水，礦床成因類型為低硫化物冰長石?絹雲母型淺成低溫熱液型金礦。
  2. It is argued that the magmatic activities of quartz - monzonite - porphyry and alkaline porphyry presumably played an essential role in mineralization of this district, that is, the porphyry system could be important sources of both ore - forming metals and ore - forming fluids, as well as a thermal engine that drived cycling of metallogenic fluids

    初步認為石英二長斑巖與堿性斑巖巖漿活動對本區成礦有重要作用，既是重要的礦源和流體來源，又是驅動成礦流體循環的主要熱源。
  3. The conclusion is that the enrichment of pt, pd is controlled by big and deep fractures, that emeishan basalt is one of the sources of pt and pd, and that basic - ultrabasic rock offers the ore - forming elements and the ore forming energy

    指出研究區的深大斷裂對鉑族元素的富集表現出很好的控製作用，峨眉山玄武巖為鉑族元素的礦源層之一，巖漿巖為鉑族元素的富集提供了成礦物質及成礦能量。
  4. Dongzigou ag deposit and jianbaoshan au deposit are hosted in the sandstone of middle - proterozoic suberathem, which are developed from the proterozoic sediment metal source - rocks formed during the meso - proterozoic volcanism and reworked by the mesozoic tectono - magmatism during the formation of the metamorphic core complexes in eastern hebei. the dongzigou ag deposit has the characteristics of reformed strata - bound origin, the jianbaoshan au deposit, located in the detachment fault, is the alterated rock type. both deposits have the similar wall - rock alteration, and show the same trace element behavior, and ree patterns. they are the results of the multi - stage tectono - magmatism in the environment of continental extension in eastern hebei region. their mineralization depended on their wall rocks and relative location in metamorphic core complexs

    賦存於中元古宙長城系常州溝組的洞子溝銀礦床和尖寶山金礦床是由密雲-都山變質核雜巖構造體系所控制的一組礦床。其成因為中元古宙火山巖漿活動形成的沉積礦源，后經中生代的變質核雜巖構造巖漿體系疊加改造而成。洞子溝銀礦床具有層控迭加改造的特點尖寶山金礦床則具有破碎蝕變巖型礦床的特點。
  5. It seems that submarine magmatism and hydrothermal activity provided abundant ore - forming material for partly strata of mogaganri and yanshiping formations during the extension of bangongcuo - nujian marginal sea in early - middle jurassic. therefore parts of jurassic mogaganri and yanshiping formations became original source of ore - forming material. in later early jurassic, the collision and collage between qiangtang block and nianqing - tanggula block made favorable conditions in geological structure, magma and ore - forming fluids for the formation of gold deposits

    在早-中侏羅世班公錯?怒江邊緣海擴張過程中，海底巖漿及其熱液作用，為侏羅系木嘎崗日群和雁石坪群部分層位提供了大量的礦源，使其成為初始礦源層；早白堊世晚期，羌塘地塊和岡底斯?念青唐古拉地塊碰撞拼貼，造成了有利的構造條件、巖漿條件、成礦流體條件，形成礦床。
  6. According to the study of the mineral evolving, origin analysis etc., it is considered that the source of minerals etc mainly comes from the pyritization sources of the submarine volcano eruption

    認為含礦巖系的物源主要來自海底火山噴發作用形成的黃鐵礦化礦源層。
  7. The research for metallogenic evolution mechanism in the region indicates that gold ore formation has undergone three stages : gold elementary source bed formation stage from the neo - archean to the paleo - proterozoic and meso - proterozoic, regional metamorphism - migmatization gold reenrichment stage at the late meso - proterozoic, structure - fluid - gold mineralization stage at the yanshan period

    對礦帶成礦演化機理的研究表明，金礦形成經歷了3個階段：新太古至古、中元古代金初始礦源層形成階段；中元古代末期區域變質混合巖化金再富集階段和燕山期構造流體金成礦作用階段。
  8. A great deal of statistic data illustrates that the mesozoic strata, especially the upper triassic immature sediments, are presumably an important source of ore - forming metals

    大量統計表明，中生代地層、特別是晚三疊世低成熟度沉積巖是重要的礦源層。
  9. 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

    經燕山期構造熱液的疊加，驅使礦源層中的成礦元素活化、遷移，在有利的構造部位富集成礦。
  10. The average chargeability value of 798 sedimentary rock specimens is 2. 4 %, that of 1149 igneous rock specimens is 2. 99 %, and that of 436 metamorphic rock specimens is 3. 59 %, which implies that the metamorphic rock might be the source of metallic ore deposits

    數值統計結果顯示， 798件沈積巖的平均極化率為2 . 40 % ， 1149件火成巖的極化率為2 . 99 % ， 436件變質巖的極化率為3 . 59 % ，因此，變質巖是本區較好的金屬礦礦源。
  11. Gold ore source beds and geochemical blocks of hebei

    河北省金的礦源層和地球化學塊體
  12. The mine was closed owing to exhaustion

    這個煤礦因礦源枯竭而被關閉。
  13. This concludes that the concept of source rocks or source beds is ambiguous and non - specific

    因此，礦源巖和礦源層並不是人們所想像的那些特定的巖石或地層。
  14. Muhuding granodiorite is one of the mine resources, what ' s more, it supplies dynamical heat

    牧虎頂巖體既是該區的au 、 ag成礦的礦源巖之一，亦為成礦提供了熱動力條件。
  15. The jingshan and jiaodong groups metamorphic green formation is the source bed of the gold mineralization in this region

    區內荊山群和膠東群變質綠巖建造是金礦化的礦源層。
  16. The granite and strata with high au abundance have been considered to the source of gold by many geologists

    摘要許多研究者認為，金豐度高的花崗巖和地層就是金礦床的礦源巖和礦源層。
  17. 26, 000t y of kaolin mine is supplied from laoyaogou, yangjiayao, yulincun and other mines nearby. the kaolin mine resources will be richer when weijiagou coal mine is put into operation

    可由郊區的老窯溝楊家窯榆林村各礦點供貨，將來魏家溝生產后，高嶺山礦源更加富足。
  18. Materials : 26, 000t y of kaolin mine is supplied from laoyaogou, yangjiayao, yulincun and other mines nearby. the kaolin mine resources will be richer when weijiagou coal mine is put into operation

    可由郊區的老窯溝楊家窯榆林村各礦點供貨，將來魏家溝生產后，高嶺土礦源更加富足。
  19. Through the analysis of geological characters in huanglianken manganese ore district, such as ore potentiality, ore controlling structures, ore depositing structures, orebody characteristics, ore type and so on, the author concluded that sinian stratum is the " primary source bed ", detachment structure is the migrating channel of ore - forming materials, favorable concentration and hosting place

    通過對黃連坑錳礦區地層的含礦性、控礦構造及容礦構造、礦體特徵、礦石類型等地質特徵的論述，認為震旦系地層是「初始礦源層」 ，滑脫構造對成礦物質起遷移、富集及容礦作用。
  20. It is believed that the distribution of gold deposits in fujian is controlled by regional deep - seated structure and precambrian volcanic flysch formation containing charcoal is main gold source rock. the accumulation of gold is closely related with yanshan granitic magma intrusion

    金礦空間分佈受一定的區域深部構造單元所制約，前寒武系富含炭質的火山復理石建造是福建省金礦的主要礦源巖，金的富集成礦與燕山期花崗巖類巖漿侵入作用密切相關。
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