铁质岩的英文

• ferruginous rock

• "岩"英文翻译    rock
• "碧玉铁质岩" 英文翻译 :    ja ilite; jasper bar; jaspilite; jaspilte; jaspilyte
• "铝铁质岩" 英文翻译 :    allite
• "镁铁质岩" 英文翻译 :    mafic rock
• "镁铁质岩石" 英文翻译 :    mafic rock; maficrock
• "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
• "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
• "镁铁质" 英文翻译 :    mafic◇镁铁质矿物 mafic mineral; mafite
• "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
• "铁质相" 英文翻译 :    ferric facies
• "血铁质" 英文翻译 :    hemosiderin; hemosiderosis
• "变质岩" 英文翻译 :    metamorfic rock; metamorhphic rock; metamorphic rocks; metamorphicrock; metamorphite; metamorphosed rock; metamorphosedrock
• "钙质岩" 英文翻译 :    calcarenite; calcareous rock; calcareousrock
• "硅质岩" 英文翻译 :    acidic rock; silica rock; silicalite; siliceous rock; silicilith; silicite
• "换质岩" 英文翻译 :    metasomatite

• 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
• 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。
• Cu - ni sulfided mine complex locate in baimazai of jinping county is sub alkali iron - super iron , it ' s zoning is clear and it ' s ni - cu - co melting first and enrichment , its rare earth is rich in right lean light rare earth , but eu in olive rock is serious to be bad , gd - tb is tittles negative abnormity . above - mentioned show that the mineral is cone from mantle , and didn " t mix with crustal substance , and continent tholeiite magma turning into continent tholeiite emplacement after by surging
  金平白马寨铜镍硫化矿床杂岩体分带明显、属亚碱性铁质-超铁质岩、具ni - cu - co三元素先熔离，后富集的规律、稀土配分为右倾斜轻稀土富集型，但橄榄岩铕亏损显著， gd - tb微小负异常，显示成矿物质来源地幔，与地壳物质无混染和大陆拉斑玄武岩浆上涌后变为大洋拉斑玄武岩浆侵位特点。
• The mesoproterozoic mafic dyke swarms are extensively distributed in the central north china craton , which are not deformed and metamorphic , emplacing the pre - existed fractures , so the dyke swarms become the conspicuous marks to reconstruct the mesoproterozoic tectonic stress field of the central ncc . the mafic dykes in the northern block are transtensional while the dykes in the central and southern blocks are extensional . the mesoproterozoic tectonic stress field could be simulated on the analysis of the distribution and mechanical origin of the mesoproterozoic mafic dyke swarms in the central ncc . the simulation result shows that the mafic dyke swarms were formed in the extensional tectonic setting in the ncc in the mesoproterozoic time , which are related to the extension of the mesoproterozoic yanliao - zhongtiao aulacogens cross the central ncc
  克拉通北部地块的镁铁质岩墙群为张剪性，而中部和南部地块为张性。根据华北克拉通中部中元古代镁铁质岩墙群的分布和成因机制分析，来恢复模拟中元古代的构造应力场。数值模拟结果表明镁铁质岩墙群在中元古代形成于伸展的大地构造背景，与横穿华北克拉通中部的燕辽-中条拗拉槽系的伸展作用有一定的联系。
• Throughout researching it has been found that three main types of copper deposits , which mafic - ultramafic rock , marine volcanic rock and porphyry , with middle proterozoic , paleozoic and mesozoic in gansu , china . the cu - bearing formation , deep major faults and late structural - magmatic zones formed in specific geotectonic setting are main ore - controlling and metallogenic factors for copper , gold and polymetallic minerals in this area , and their convergent positions are effective ones formed ore bodies in space
  通过研究认为：镁铁质-超镁铁质岩型、海相火山岩型及斑岩型三种铜矿类型，是甘肃的主要铜成矿类型，其主成矿阶段为中元古代、古生代以及中生代；特定大地构造背景下形成的含矿建造、区域性深大断裂以及后期斜向构造-岩浆活动带，是该区铜、金及多金属成矿的主要控矿因素，三者在空间上的复合是矿床体形成的有利部位。