晶岩的英文

• pegmatite

• "晶"英文翻译    brilliant; glittering
• "岩"英文翻译    rock
• "变晶岩" 英文翻译 :    metacrystalline rocks; metacrystallinerocks
• "尖晶岩" 英文翻译 :    spinellite
• "结晶岩" 英文翻译 :    crystalline rock; crystallinerock
• "颗晶岩" 英文翻译 :    phanerite
• "蓝晶岩" 英文翻译 :    disthenite; kyanitite
• "全晶岩" 英文翻译 :    isomerite
• "微晶岩" 英文翻译 :    microcrystalline rock
• "伟晶岩" 英文翻译 :    pegmatite
• "矽晶岩" 英文翻译 :    aplite
• "细晶岩" 英文翻译 :    granitine; haplite
• "显晶岩" 英文翻译 :    phanerite
• "隐晶岩" 英文翻译 :    aphanide; aphanite; cornean; cryptocrystalline rock; cryptomere; kryptomere
• "重晶岩" 英文翻译 :    baria
• "隐晶岩；非显晶岩" 英文翻译 :    aphanite
• "伟晶岩状 似伟晶岩的" 英文翻译 :    pegmatoid
• "白岗细晶岩" 英文翻译 :    alaskite aplite
• "变伟晶岩" 英文翻译 :    metapegmatite
• "磁铁伟晶岩" 英文翻译 :    magnetite pegmatite
• "带状伟晶岩" 英文翻译 :    zonal pegmatite; zonalpegmatite
• "淡歪细晶岩" 英文翻译 :    bostonite
• "多斑晶岩" 英文翻译 :    pleistophyric rock
• "二长细晶岩" 英文翻译 :    monzonite-aplite
• "方解伟晶岩" 英文翻译 :    calcite pegmatite

• Quartz diorite aplite
  石英闪长细晶岩
• Soda syenite aplite
  钠正长细晶岩
• A dense , homogeneous rock with constituents so fine that they cannot be seen by the naked eye
  隐晶岩，非显晶岩一种成分细密肉眼不能看到的致密同质岩石
• Chen p . r . , chen x . m . , ni p . , wang w . c . et al . , 1997 , discovery of chalcopyrite daughter mineral in polyphase fluid inclusions from yanyuan porphyry copper deposit , sichuan province
  朱金初，李人科，周凤英，王汝成等， 1996 ,广西栗木水溪庙不对称层状伟晶岩?细晶岩岩脉的成因讨论。
• Detail mapping shows that the yagan mcc consists of crystallized metamorphic core ( low plate ) , detachment zone and upper plate . the metamorphic core consists of can be further subdivided into two level parts low - level high metamorphic and upper - level shallow metamorphic structural slice and between them there exists a ductile shear zone . thus the whole texture of the mcc is characterized by " three layers and tow zones " this reveals a process of extensional uplift of poly - level slices by poly ductile shear zones , a characteristics of poly - level extensional structural systems . the deformational environments change vertically in a sequence of high amphibolite facies
  亚干变质核杂岩由下盘结晶岩系变质核、拆离带和上盘岩系构成，其中，变质核由四个单位及许多花岗岩体(脉)组成，可进一步分为中深和中浅变质两个构造单位(岩片) ，之间发育次级韧性拆离带(花岗质糜棱岩带) ，加上上盘总体构成“三层两带”的结构特点。