镁铁质的英文

• mafic
  ◇镁铁质矿物 mafic mineral; mafite

• "镁"英文翻译    magnesium
• "多镁铁质" 英文翻译 :    domafic(c.i.p.w.)
• "过镁铁质" 英文翻译 :    permafic(c.i.p.w.)
• "镁铁质边缘" 英文翻译 :    mafic margin
• "镁铁质的" 英文翻译 :    mafic
• "镁铁质角岩" 英文翻译 :    mafic hornfels
• "镁铁质矿物" 英文翻译 :    mafic mineral; mafic minteral; melane
• "镁铁质岩" 英文翻译 :    mafic rock
• "镁铁质岩石" 英文翻译 :    mafic rock; maficrock
• "全镁铁质的" 英文翻译 :    holomafic
• "大陆镁铁质岩浆" 英文翻译 :    continental mafic magma
• "铁质" 英文翻译 :    human iron metabolism
• "铁质污；铁质粒" 英文翻译 :    iron-shot
• "镁铁的" 英文翻译 :    mafic
• "镁铁矿" 英文翻译 :    magnesioferrite
• "超铁质" 英文翻译 :    hyper ferric
• "胆铁质" 英文翻译 :    ferrin
• "核铁质" 英文翻译 :    ferratogen; ferricnuclein; karyogenic
• "肉铁质" 英文翻译 :    carniferrin
• "铁质的" 英文翻译 :    ferriferous
• "铁质化" 英文翻译 :    ferrugimation; ferruginization
• "铁质壳" 英文翻译 :    ferricrete
• "铁质泉" 英文翻译 :    chalybeate spring; ferruginous spring
• "铁质水" 英文翻译 :    chalybeate waters
• "铁质土" 英文翻译 :    ferruginous soil

• Biotite is a subordinate constituent of the mafic and ultramafic rocks generally .
  黑云母一般是镁铁质及超镁铁质岩石中的次要成分。
• With regard to the oxide minerals, chromite is almost entirely contained in the olivine-rich ultramafic rocks in the lower part of the intrusion .
  关于氧化矿物，铬铁矿几乎全部含于侵入体下部的富橄榄石的超镁铁质岩石中。
• Lithogeochemistry of the sulfide - bearing mafic - ultramafic rock at baimazhai , jinping , southern yunnan
  超镁铁质岩石有关的矿床类型
• Petrochemistry and ore potentiality of the mafic - ultramafic rocks in the yangliuping cu - ni - pgf mine , sichuan province
  超镁铁质岩型铜镍矿床成矿条件与找矿远景分析
• Strong compatible elements , as cr , ni , co , sc , from most samples is very low
  大多数样品的cr 、 ni 、 co 、 sc等强相容元素含量较低，也暗示了形成镁铁质岩石的母岩浆应属残余熔融体。
• Wenquan granite is composed of two end - member rocks , one is the host rock of the acid end - member , and the other is the microgranular mafic enclave
  摘要温泉花岗岩体由酸性端元的寄主岩石和暗色微细粒镁铁质包体群及基性岩墙群组成。
• There are over 30 mafic and ultramafic intrusions in the area and cu - ni sulfide ore bodies were found in no . 1 and no . 7 ultramafic intrusive bodies which exhibit obvious zoning and cumulate texture
  区内出露30多个镁铁超镁铁质岩体，其中1 、 7号超镁铁岩体中赋存铜镍硫化物矿（床）体。
• Layered mafic intrusions not only represent natural laboratories for studying processes of magmatic differentiation and assimilation within the crust , but also contain extensive precious and base metal mineralization
  层状镁铁质岩体不仅是研究岩浆分异演化过程和地壳混染作用的最佳天然实验室，其中还广泛赋存重要的稀有金属和贱金属矿床。
• Compared with jianchaling nickel sulflde deposit , jinchuan superlarge copper - nickel sulflde deposit mostly related with mafic - ultramafic complex that multiple intruded , spatially respected with old huabei block , which formed in marginal rift in middle - new proterozoic
  与煎茶岭镍矿床相比，金川超大型镍铜硫化物矿床主要与多次侵入的镁铁?超镁铁质杂岩有关，空间上与时代相对较老的华北地块关系密切，形成于中?新元古代的边缘裂谷。
• Substance of rock - forming and ore - forming in both jianchaling and jinchuan nickel deposit mainly derived from the upper mantle , but the former source is relatively depleted mantle . on the other hand , there exsisted the crustal contamination during the formation of the two mineral deposits , the later contaminated poorly and gave priority to deep contamination . ( 5 ) by the comparative study of jianchaling with jinchuan nickel sulflde deposit , it is pointed that small basic - ultralbasic complexes which dis
  ( 5 )通过对煎茶岭和金川镍矿床的比较研究，结合对国内外有关岩浆镍矿床的比较分析，根据我国的地质特点，提出沿较老地块边缘分布的特别是沿华北地块北缘分布的基性?超基性小杂岩体，是找寻大而富的硫化镍矿床之有利找矿方向；而对较老地块内部的镁铁质侵入体，亦应给予高度注意。