角閃片巖 的英文怎麼說

中文拼音 [jiǎoshǎnpiānyán]
角閃片巖 英文
horn schist
  • : 角Ⅰ名詞1 (牛、羊、 鹿等頭上長出的堅硬的東西) horn 2 (古時軍中吹的樂器) bugle; horn 3 (形狀像...
  • : Ⅰ動詞1 (躲閃; 閃避) dodge; get out of the way 2 (扭傷) twist; sprain 3 (突然出現) flash 4 ...
  • : 片構詞成分。
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  1. The high - pressure metamorphic rocks in northeastern jiangxi province include such types of rocks as jadeite - bearing aegirine - augite albite amphibole schist, jadeite - bearing aegirine - augite quartz albitite, aegirine - augite - bearing amphibole quartz albitite, aegirine - augite - bearing albite amphibole schist, winchite quartz albitite, and magnesio - riebeckite quartz albitite

    摘要贛東北高壓變質包括含硬玉霓輝石鈉長角閃片巖、含硬玉霓輝石石英納長石、含霓輝石石英鈉長石、含霓輝石鈉長角閃片巖、藍透石石英鈉長石、鎂鈉石石英鈉長石石類型。
  2. Based on the 1 : 50000 regional geological survey, the sertengshan rock group is revised, involving the schist and marble of low - amphibolite to high - greenschist facies, which are distributed in middle and west inner mongolia

    摘要根據近年完成的1 : 5萬區域地質調查成果及綜合研究,將分佈於內蒙古中部色爾騰山、大青山、西部烏拉特后旗以及阿拉坦敖包、疊布斯格等地的低相高綠相的、大理系釐定為色爾騰山群。
  3. Based on the studies of petrotexture, structural deformation and the relevant metamorphism, this paper indicates that this peridotite massif is the product of ultramafic magma cumulated at the crust - mantle transtion zone and has undergone the early stage of plastic deformation under the condition of granulite facies ( 800 ) and late ductile shearing at amphibolite and greenschist facies in relevance to uplifting

    本文通過體的結構、構造變形及相應的變質作用研究,提出了該橄欖體是由超基性漿在殼幔過渡帶結晶而成,並經歷了與圍一致的麻粒相( 800 )條件下的早期塑性變形以及相和綠相退化變質條件下與逆沖上升有關的韌性剪切變形。
  4. Greenschist facies, low green schist facies and brittle shear deformation facies. the attitude of different structural element of the yagan mcc are keeping coordination. analysis of kinematics demonstrates the sse - directed shearing - off of the hanging wall relative to the footwall along the penetrative mylonitic lineation

    其變形相由變質核中心到上盤系(由深至淺)依次為高相? ?綠相? ?低綠相? ?脆性剪切變形相,顯示亞干核雜由中心向邊部變形層次遞減的特點。
  5. The lithology of c petrofabric is marble, accidental gneiss. by field attitude, rock association character, petrography and petrochemistry, we know that the protolith of a petrofabric is mainly composed of pelite, sandstone and basic to acidic volcanic, that of b petrofabric mainly a suite of pelite, sandstone ( maybe include volcanic ), and that of c petrofabric mainly limestone, impurity limestone, a few of pelite and pyroclastic rock

    A組的性主要是各種類和類夾有,偶有變粒、大理。 b組的性主要是各種夾有大理、石英。 c組主要是一套大理,偶有
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