斑玄武岩的英文

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• "斑"英文翻译    spot; speck; speckle; stripe ...
• "玄武岩"英文翻译    basalt
• "辉斑玄武岩" 英文翻译 :    augitophre; augitophyre
• "拉斑玄武岩" 英文翻译 :    tholeiite; tholeiitic basalt
• "变拉斑玄武岩" 英文翻译 :    metatholeiite
• "拉斑玄武岩浆" 英文翻译 :    tholeiitic magma
• "橄斑玄武岩的" 英文翻译 :    chrysophyric
• "倍长拉斑玄武岩" 英文翻译 :    bytownite-tholeiite
• "长橄辉斑玄武岩" 英文翻译 :    dunsapie basalt
• "长橄榄斑玄武岩" 英文翻译 :    dunsapie basalt
• "大洋拉斑玄武岩" 英文翻译 :    oceanic tholeiite
• "岛弧型拉斑玄武岩" 英文翻译 :    island arc tholeiite; islandarctholeiite
• "低钾拉斑玄武岩" 英文翻译 :    low-k tholeiite; low-ktholeiite
• "海洋性拉斑玄武岩" 英文翻译 :    oceanic tholeiite; oceanic tholeite; oceanictholeiite
• "拉斑玄武岩系列" 英文翻译 :    tholeiite series
• "钠钙拉斑玄武岩" 英文翻译 :    bytownite-tholeiite
• "深海拉斑玄武岩" 英文翻译 :    abyssal tholeiite; abyssaltholeiite
• "洋脊拉斑玄武岩" 英文翻译 :    oceanic ridge tholeiite; oceanicridgetholeiite; ridge tholeiite
• "洋隆拉斑玄武岩" 英文翻译 :    rise tholeiite
• "橄榄拉斑玄武岩" 英文翻译 :    olivine tholeiite
• "倍长拉斑玄武岩；钠钙拉斑玄武岩" 英文翻译 :    bytownite-tholeiite
• "拉斑玄武岩质辉长岩" 英文翻译 :    tholeiitic gabbro
• "拉斑玄武岩质粒玄岩" 英文翻译 :    tholeiitic dolerite
• "玄武岩" 英文翻译 :    basalt
• "玄武岩玄武岩玄武岩底" 英文翻译 :    basalt

• The tholeiite with late trassic age has been found in helanshan area on the north part of western margin of ordos basin
  在盆地西缘北部贺兰山地区，发现典型拉张环境形成的拉斑玄武岩，测年时代为晚三叠世。
• By studying , the main conclusions have been achieved as follows : i . the volcanic rocks , as the result of the partial melting of enriched mantle , comprise calc - alkaline andesite and dacite and a few tholeiite
  通过研究，得出以下主要认识： 1 、火山岩为一套以钙碱性安山岩为主，含少量拉斑玄武岩和英安岩。
• Two ree distributed pattern , lree - depleted and flat , which display a specific character of typical mid - ocean ridge tholeiite , indicate that primary magma may be derived from near primary or a typical large ion lithophile element ( lile ) - depleted mantle
  岩石稀土元素配分模式可分为lree平坦型和lree亏损型两类，指示了其原始岩浆起源于近原始或典型的大离子元素亏损型的地幔，为典型的大洋中脊拉斑玄武岩的特征。
• 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。
• Given their oib - type trace element pattern and depleted sr - nd isotop ic composition , the datong alkali basalts are interpreted to be generated within the asthenospheric mantle but at a shallow depth compared to the yangyuan alkali basalts . the datong tholeiitic basalts exhibit low snd values ( 1 - 4 ) . their sr - pb and nd - pb isotopic correlations are consistent with a mixing between the depleted mantle and emi - like component
  大同地区第四纪时期同时产出碱性和拉斑玄武岩，碱性玄武岩也主要来自于软流圈地幔，岩浆起源深度小于阳原样品；拉斑玄武岩具有较低的nd ( nd = 1 - 4 ) ， pb - nd以及pb - sr同位素相关关系暗示其可能是dm和型富集地幔( emi )组分之间混合的结果，反映了软流圈和岩石圈地幔之间的相互作用，岩浆起源较浅。
• On the basis of the study on the petrology , trace element , and isotopic geochemistry , the primary magma of volcanic rocks can be divided into two series according to their originated rocks and degree of partial melting . one is the basanite - alkaline basalt - olivine tholeiite magma series , which are generated by partial melting from spinel iherzolite ; the other is nephelinite magma - alkaline picritic basalt magma , which are generated by partial melting of the garnet iherzolite
  岩石化学、微量元素、同位素地球化学证据都表明，华北、华南地区的火山岩根据源岩和局部熔融程度的不同，可以分为两个原生岩浆系列：一个是源岩为尖晶石二辉橄榄岩，随着局部熔融程度的增加，形成的碧玄岩岩浆-碱性玄武岩岩浆-橄榄拉斑玄武岩岩浆；另一个是源岩为石榴石二辉橄榄岩，随着局部熔融程度的增加形成的霞石岩岩浆-碱性苦橄玄武岩系列。
• This important tectonic zone parallel to the isotopic geochemical steep zone , which represented a suture line between the yangtze and cathaysian blocks . the geochemical evidence of the jianshui volcanic rocks from the sw part of shizong - mile zone shows that their lithologic types are tholeiites with the comparative flat ree patterns and enrichment in th , depletion slightly in nb , ta , and flat hfse . thus , they may be formed in a back - arc basin with the characteristics between morb and island - a
  该构造带西南段的建水火山岩地球化学特征研究表明，该火山岩为拉斑玄武岩，具有较平坦的稀土分配型式， th较富集， nb 、 ta轻微亏损，高场强元素分布较平坦，具有介于岛弧和morb之间的地球化学特征，可能形成于弧后盆地环境。

• 斑玄武岩的日语：インニンモア岩 インニンモアがん