輝綠輝長巖 的英文怎麼說

中文拼音 [huīhuīzhǎngyán]
輝綠輝長巖 英文
diabase gabbro
  • : Ⅰ名詞(閃耀的光彩) brightness; splendour; brilliance Ⅱ動詞(照耀) shine
  • : 綠形容詞(像草和樹葉茂盛時的顏色) green
  • : 長Ⅰ形容詞1 (年紀較大) older; elder; senior 2 (排行最大) eldest; oldest Ⅱ名詞(領導人) chief;...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  1. Based on an analysis of geochemical characteristics of rocks and trace elements as well as rare earth elements, this paper holds that they are products of crystallization differentiation of the same magma, that the major ore resource of this area is copper, and that gabbro - diabase is the main ore - bearing horizon

    通過對石化學特徵和微量元素、稀土元素地球化學特徵的剖析,表明其是同一漿結晶分異的產物,本區主要礦產應為銅,是主要的含礦層位。
  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

    基性脈主要包括(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熔融的產物。
  3. All these ductile shear zones are characterized by northward thrusting. the u - pb dating on zircons from the bedded gabbro of the qimanyuter ophiolite melange gives an age of 526 ? 1 ma ( early cambrian )

    在其曼于特蛇的層狀細粒中獲得了鋯石u - pb年齡值為526 1ma (早寒武世) ,它被晚奧陶世花崗侵入。
  4. The geochemical characteristics of gabbros from the jinshajiang ophiolitic melange indicate that they were derived from a mantle source different from that of volcanic rocks, which may be a product in the ocean rift in the earlier stage

    東竹林蛇混雜地球化學特徵表明,它與火山不同源,可能是洋盆裂谷初期的產物。
  5. As they drew near the island seemed to lift from the sea, and the air was so clear that they could already distinguish the rocks heaped on one another, like cannon balls in an arsenal, with green bushes and trees growing in the crevices

    當他們接近那個島的時候,它象是從海底里冒出來的一個龐然大物,透過明凈天際下的薄暮余,他們辨得出石一塊一塊地堆積在一起,象一座彈藥庫里的炮彈一樣石縫里則生著青色的灌木和小樹。
  6. Qimanyuter ophiolite melange crops out 1 - 3 km in width and extends ew - nee about 50 km, parallels to the kunlun mountains. qimanyuter ophiolite melange is composed mainly of serpentinite ( metapyrolite ), peridotite, bedded gabbro, grbbro, diabase sheet and pillow - like and massif basalt as well. associated sedimentary rocks with this ophiolite melange include silicalite, dark gray silicalite and thin - bedded limestone

    該混雜帶所包含的主要性單位包括:蛇紋(變) 、橄欖、層狀席、枕狀、塊狀、杏仁狀玄武,與之共生的沉積為紫紅色硅質、深灰色硅質、薄層灰等。
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