閃巖 的英文怎麼說

中文拼音 [shǎnyán]
閃巖 英文
[巖] amphibolite
  • : 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 ...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  1. Albite - epidote - amphibolite facies

    鈉長簾閃巖
  2. 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、含硬玉霓輝石石英納長石、含霓輝石角長石英鈉長石、含霓輝石鈉長角、藍透石石英鈉長石、鎂鈉石石英鈉長石石類型。
  3. Amphibole - cholrite schist

    綠泥片
  4. In the course, the condition and the process of forming and changing of minerals, the typomorphic features of minerals, the characteristics of the distribution and the evolution of minerals and their paragenetic associations in the period and the space, the methods of mineral analyses and research, the geological thermometers and the geologicial barometers of minerals, mineral paragenetic associations and paragenesis analyses will be introduced, and the magnificent and the microscopic genetic characteristics of pyrite, quartz, garnet, pyroxene, amphibole, mica, feldspar, and other minerals will be dealt with particularly

    本課程主要講述礦物及其共生組合的形成和變化的條件和過程,不同物理化學條件下礦物的成分、結構、形態、物性等標型特徵以及它們之間的內在聯系,礦物及其共生組合在時間上和空間上的分佈和演化規律,礦物成分、結構、形貌、物性等的分析測試方法,礦物地質溫度計和地質壓力計對其形成環境的表徵,不同體系(封閉體系、開放體系)條件下,礦物的穩定范圍和彼此替代順序的共生分析,重點介紹黃鐵礦、石英、石榴石、輝石、角石、雲母、長石等礦物(族)在成因上的宏觀標志和微觀信息,以及其成因信息在成作用和成礦作用中的地質意義。
  5. Hornblende bearing varieties bridge the gap over to amphibolites which are in bands and dikes.

    含角石的變種填補了帶狀和脈狀角閃巖的中間相。
  6. The metamorphic process in the formation of garnet amphibolite along the china - pakistan highway profile, west kunlun orogenic belt

    西昆侖造山帶中巴公路段石榴角閃巖形成的變質地質過程
  7. Lots of information suggest that the metamorphism process of this area are from granulite facies to amphibolite facies and the retrograded metamorphic path is basically a cw nearly isothermal decompressional evolvement trend

    各種信息表明本區的變質作用是由麻粒相退變到角閃巖相。退變質軌跡基本上是一個順時針近等溫減壓型演化趨勢。
  8. 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、疊布斯格等地的低角閃巖相高綠片相的片、大理系釐定為色爾騰山群。
  9. All these rocks aforementioned are mainly parametamorphic rocks. milan, kaqiang and alamasi group underwent high - grade metamorphism of amphibolite facies, together with weak migmatism. they share the same geochemistry and total ree and many other chracters

    二者主要為副變質石,米蘭群和卡羌群、阿拉瑪斯群變質較深為角閃巖相,普遍弱混合化,它們具有非常相似的地球化學特徵,稀土元素總量及其它特點一致或相近。
  10. 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角閃巖相和綠片相退化變質條件下與逆沖上升有關的韌性剪切變形。
  11. Riebeckite aplite - granite

    細晶花崗
  12. Quartz diorite aplite

    石英長細晶
  13. The peak is composed of banded biotite tonalite of fine mediate grain developing in mengshan rock suit of fuping period of archean era about 2. 7billion years ago. it ' s very steep

    由27億年左右形成的太古代阜平期蒙山套條帶狀中細粒黑雲母英雲構成,柱狀節理發育,差異性風化剝蝕作用強烈,組成雲蒙「山」峰,俗稱「掛心崛子」 ,形容雲蒙峰之陡峻。
  14. Arequipa, the city at the foot of el misti, is the commercial and agricultural hub of southern peru. the city takes its gleam from volcanic building stone

    米斯提火山腳下的阿雷基帕城是南秘魯的商業及農業中心。用火山建成的城市爍著微弱的光芒。
  15. It was followed by the swift flashes of the rifles, which sent their leaden messenger across the rock in volleys, as though the assailants would pour out their impotent fury on the insensible scene of the fatal contest.

    緊接著,火光,槍彈越過雙方之間的石,成排地飛射過來,彷彿他們要把自己無可奈何的憤怒,全都發泄在進行這場殊死搏鬥的這片無知無覺的土地上似的。
  16. 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)依次為高角閃巖相? ?綠片相? ?低綠片相? ?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。
  17. 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組的性主要是各種角閃巖類和片麻類夾有片,偶有變粒、大理。 b組的性主要是各種片夾有大理、石英。 c組主要是一套大理,偶有片麻
  18. Most of the smaller hornblendite bodies contain about 5-10 percent magnetite, with only local sporadic enrichment.

    在小的角閃巖體中,磁鐵礦可佔510,僅有局部的散染狀富集。
  19. Most of the smaller hornblendite bodies contain about 5 - 10 percent magnetite, with only local sporadic enrichment

    在小的角閃巖體中,磁鐵礦可佔510 ,僅有局部的散染狀富集。
  20. The eyes and mouths of hawk - shaped stone are formed by the weathering and eroding of plagioamphibolite or other enclave rocks developing in the adamellite mass while the figure of the hawk is shaped by adamellit mass of taishan group aged 2. 4billion years

    24億年左右形成的二長花崗中的泰山群斜長角閃巖包體,石風化剝蝕后形成小孔如老鷹的眼睛和嘴部等,二長花崗球狀風化后形成老鷹的外形。
分享友人