硅質玄武巖 的英文怎麼說

中文拼音 [guīzhíxuányán]
硅質玄武巖 英文
tholeiite
  • : 名詞[化學] silicon (14號元素符號 si)
  • : Ⅰ名詞1 (性質; 本質) nature; character; essence 2 (質量) quality 3 (物質) matter; substance;...
  • : Ⅰ形容詞1 (黑色) black; dark 2 (深奧) profound; abstruse; recondite 3 (不實在; 靠不住) unrel...
  • : Ⅰ形容詞1 (關于軍事的) military 2 (關于技擊的) connected with the art of attack and defence in...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • 玄武 : 1 (烏龜) tortoise2 (二十八宿中北方七宿的合稱) seven constellations of northern sky3 (道教所...
  1. The two early carboniferous fragments are composed of basalt and ash - black, fuchsia radiolaria silicalite, siliceous mudstone, tuff

    早石炭世兩個斷片由和灰白色、紫紅色放射蟲、凝灰組成。
  2. The lower member of typical ophiolite suit is exposed at outsides of the qimanyuter ophiolite melange and in between, there distribute the basalt, deep sea limestone and silicalites. these different litho - members contact to each other with ductile shear zones

    帶內蛇綠套下部單元出露于兩側,和相關的深水灰等分佈於中部,各單元間均以韌性剪切帶接觸。
  3. 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(變輝橄) 、橄欖輝石、層狀輝長、輝長、輝綠席、枕狀、塊狀、杏仁狀,與之共生的沉積為紫紅色、深灰色、薄層灰等。
  4. The lower paleozoic strata in the south kunlun massif are kulafuhe group of cambbrian - ordovician. they consists of metamorphic detrital rocks, limestone, magnetite - bearing basalt, quartzite ( meta - silicalite ), which suggests that they might form at active continent margin. the geochemical characteristics of volcanic and detrital rocks do indicate that they might form at an active marginal environment such as island arc etc. associated with the qimanyuter ophiolite suit, there are lots of early paleozoic granitic plutons

    在昆南地塊上的早古生代地層為寒?奧陶系庫拉甫河群,由變碎屑、灰、含磁鐵礦、石英(變)等組成,顯示其比昆北地塊有較大的活動性,火山和碎屑石地球化學特徵也反映為島弧及活動邊緣環境。
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