熔巖脈 的英文怎麼說

中文拼音 [róngyánmài]
熔巖脈 英文
lava streak
  • : 動詞(熔化) melt; fuse; smelt
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • : 脈名詞1. (動脈和靜脈的統稱) arteries and veins2. (脈搏的簡稱) pulse 3. (像血管的組織; 連貫成系統的東西) vein
  1. Mountains and ridges of rough lava are furrowed with narrow valleys of alkaline soil sheltering a few grasses and shrubs

    形成的山和山脊間,狹窄山谷內的鹼性土壤上零星散布著草叢和灌木。
  2. The mafic dikes also formed by the partial melting of enriched mantle, include gabbro, diabase ( distributing mainly in luxi ) and lamprophyres ( camptovogesite, odinite and hornblende lamprophyres ) ( mainly in ludong ). for all the rocks, crustal contamination was absent when magma emplaced. 2

    基性主要包括輝長、輝綠(主要分佈在魯西地區)和煌斑(以斜閃煌斑為主,同時含部分拉輝煌斑和角閃煌斑) (主要分佈在魯東地區) ,都為富集石圈地幔部分融的產物。
  3. Such lavas also once came from the volcanoes in the cascade range in washington.

    在華盛頓州的喀斯喀特山的火山也噴出過這樣的
  4. The pges abundance patterns of residual mantle rock with a peleo - subduction background is characterized by pd, pt depletion and ir, ru relatively enrichment, while the basalt and basic dyke by the processing of partial melt in the same background take an opposite feature of pd, pt enrichment and ir, ru depletion. the existence of fluid in the subduction zone increases the degree of partial melt on the one hand, and on the other, activates the activity of pd, pt compare to ir, ru, and thus reduces the pd ir and pt ru in residual mantle rock. the pges patterns for basalt and basic dyke from two carboniferous volcano zones to south qoltag and north turpan - hami basin, xinjing uigur autonomous region, take a shape of gentle positive inclined curve with lower pt and pd differentiation and lower pges. all these features are obviously different from that of basic dyke and basalt from typical ophiolite and therefore the author believe that their fluid - rich paleo - subduction zone environment can be ruled out

    古俯沖帶背景下的殘餘地幔的pges配分以pd , pt明顯虧損和ir , ru相對富集為特徵,而部分融產物的玄武和基性則呈現相反的ir , ru明顯虧損和pd , pt相對富集特徵。俯沖帶中流體的參與一方面增加了部分融程度,有利於pd , pt從原始地幔進入融相另一方面,流體的作用使得pd , pt相對于ir , ru遷移活動性效率提高,造成地幔
  5. The southern hainan mafic dykes are strongly enriched in lile with high nb / ta ratios, indicating a magma source reconstructed by silicic - melt through partial melting of ancient subducted slides. however, the northern hainan mafic dykes with chondritic nb / ta ratio should be derived from the fiuid - metasomatized mantle related to ancient subduction zone

    瓊南基性強烈富k _ 2o等lile和具有較高nb ta比值,其地幔源區應受到了古俯沖板片部分融形成的硅質體的改造;而瓊中基性的nb ta比值接近於球粒隕石和morb值,應為古俯沖帶含水流體交代的地幔源區的產物。
  6. This paper points out that the ore - forming pattern of this mineral deposit is ore - bearing basic - superbasic magma melting - crystalline different and ore magma impulse injection in turn. it indicates there maybe has a ore shoot in the bottom of iii rock body ( interrupted below 650m ), and advises to geophysical prospecting in the mining shaft

    並指出本礦床為含礦基性-超基性漿離-結晶分異和礦漿依次沖式貫入的銅鎳硫化物礦床成礦模式,指明號體下部( 650m以下中斷)可能存在一富礦體,並建議進一步做井中物探證實。
  7. A hairline fracture in the cola coloured veneer which seperated my cup of tea from the throbbing liquid lava of red disco heaven beneath the surface of the table

    在可樂色薄板上的細裂紋,它從桌子表面之下的動的紅色迪斯科天堂的液體分開了我喜愛的東西。
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