結晶質礦物 的英文怎麼說

中文拼音 [jiējīngzhíkuàng]
結晶質礦物 英文
crystalline mineral
  • : 結動詞(長出果實或種子) bear (fruit); form (seed)
  • : Ⅰ形容詞(光亮) brilliant; glittering Ⅱ名詞1. (水晶) quartz; (rock) crystal 2. (晶體) any crystalline substance
  • : Ⅰ名詞1 (性質; 本質) nature; character; essence 2 (質量) quality 3 (物質) matter; substance;...
  • : 名詞1. (礦床) ore [mineral] deposit 2. (礦石) ore 3. (開采礦物的場所) mine
  • : 名詞1 (東西) thing; matter; object 2 (指自己以外的人或與己相對的環境) other people; the outsi...
  • 結晶 : 1 (析出晶體) crystallize2 (晶體) crystal 3 (成果) crystallization; fruit; product; quintess...
  • 礦物 : mineral
  1. On thebasis of describing mineralogy characteristics such as combination electron minro - form , crystallinity of clay minerals , the relationship between coal series clay minerals in themesozoic era in ningxia area and coal metamorphism was analyzed

    在概述粘土組合、電子顯微形態和度等學特徵的基礎上,探討了寧夏地區中生代煤系粘土與煤變的關系。
  2. The texture can be systematically classified as the six types : the felt - like texture, the micro - fibrous cryptocrystalline texture, the micro - fibrous texture, the micro - leaf - like cryptocrystalline texture, the micro - leaf - like texture and the radiated fibrous texture

    通過對青海軟玉顯微構的觀察與研究,按其主要透閃石組分的表現形式,較為系統地劃分青海軟玉的主要構類型為:毛氈狀構、顯微纖維隱構、顯微纖維構、顯微葉片狀隱構、顯微葉片狀構以及放射狀纖維構。
  3. The terminology classification codes of geology and mineral resources - the crystallography and mineralogy

    產術語分類代碼學及
  4. Secondly, based on the microbeam analytical technique, on the one hand, through investigating the characteristic of major elements in the mantle minerals the author acquired the static information from mantle ; on the other hand, through multi - point analysis of a part of the minerals from mantle, the auther got dynamic information from mantle. finally, generalizating the fruits of this study and predecessors, the autor holds that the constituents of lithospheric mantle possibly includes spinel lherzolites, clinopyroxenites, websterite, dunite, harzburgites, garnet lherzite, phlogopite lherzite, eclogites, clinopyroxene megacrysts ; compared with east china and north china platform, the research field mantle shows the characteristics of higher degree of partial melting processes and more depleted mantle ; the. upper mantle beneath north hetian area is heterogeneous, with a tendency of deficit in a12o3 and lree from kaliyang in west hetian to the river basin of kalakshi river and yulongkashi river ; the subduction of the crust beneath north hetian has ever occurred in geological history and caused the mixing of mantle - crust ; the depth of the origination of basaltic magmas beneath north hetian exceeds 73km ; the thickness of the lithosphere beneath the research area amounts to 204. 9km ; the mantle beneath north hetian has geological condtions for forming diamond deposits

    最後,綜合本區幔源和地幔巖石的特徵以及地球理資料,得出如下論:本區上地幔的組成有尖石二輝橄欖巖、二輝巖、單斜輝石巖、純橄欖巖、方輝橄欖巖、石榴石二輝橄欖巖、金雲母二輝橄欖巖、榴輝巖;與中國東部以及華北地臺上地幔相比,研究區上地幔具有富集主元素中相容元素和虧損其中的不相容元素的特徵,局部熔融程度較高;上地幔存在橫向和縱向的不均一性,從西部的克里陽到喀拉喀什河和玉龍喀什河流域, al和lree富集程度呈下降趨勢,不同來源的相同中主元素的含量差異較大;地歷史時期這里可能發生過地殼俯沖並產生殼幔混合作用;玄武巖漿的起源深度73km ;從幔源重砂的溫壓估算果,可以推斷出巖石圈厚度可達204 . 9km ;綜合巖石圈組成特徵、巖石圈熱狀態、地幔溫壓狀態、氧逸度以及幔源巖石和幔源的化學成分,認為研究區具備了金剛石成地幔地條件。
  5. By infrared spectrum study, the limonite ( feooh nh2o ) can be considered the main colorating mineral in the yellow and red jadeite, and the hematite is another colorating mineral in the red jadeite. the difference of color tone is due to the n value in the molecular formula feooh nh2o and the content of crystal water and adsorbent water. the iron ion came from the effloresced and eroded rocks, and formed fe ( oh ) 3 colloid reacted with the surface water

    周圍床的風化蝕變為表生水提供了鐵,形成弱酸性的含fe ( oh ) _ 3膠體的水溶液,表生水流經翡翠石時, fe ( oh ) _ 3膠體附著在巖石的表面,經過脫水和吸附,形成褐鐵膠體,褐鐵膠體沿裂隙或鬆散的顆粒進入翡翠巖石中,逐漸累積沉澱,形成次生色層。
  6. And apatite. by these analyses and comparison with general granite both in china and the world and with the granite in other au or cu belt in china, the characteristics of the granite in this area are concluded as follows. it belongs to magnetite - i or syntectic granite and has crust - mantle mixed characteristics ; it was formed mainly by crystallization differentiation of melting magma and multiphase varied intrusion ; the degree of differentiation evolvement is not high ; the granite and its enclaves p. re congenetic ; the range of temperature is about 500 - 700, the range of pressure is about 2. 50 gpa - 4. 35 gpa, and the range of oxygen fugacity ( lg fo2 ) is - 15. 53 - - 14. 00 ; most granite bodies formed before the collision of plates, and few formed after the collision of plates

    通過對測試數據的分析與綜合研究,並同中國和世界一般花崗巖類以及中國主要金、銅成巖體的花崗巖類進行對比,得出本區花崗巖類巖石具有以下特徵:屬磁鐵-型或同熔型花崗巖,其巖漿具殼幔混源特徵:主要由熔融態巖漿經分異作用,通過多期變速上侵而形成;其分異演化程度較低;寄主巖基和包體具有同源性;巖石的形成溫度范圍約為500 - 700 ,壓力大約為2 . 50gpa - 4 . 35gpa ,氧逸度值1gfo _ 2為- 15 . 53 ? 14 . 00 ;該巖帶主要形成於板塊碰撞前消減的活動板塊邊緣期,為燕山至喜馬拉雅早期的大陸邊緣火山弧環境的產
  7. Because of the absence of mantle xenoliths and xenocrysts, it is the first time that this paper looks on the native heavy minerals deriving from mantle, which were collected at the terraces of the two rivers, kalakshi river and yulongkashi river, as objects and takes into account the geochemical characteristics of the rocks deriving from mantle such as keliyang lamproite and so on to study the composition of lithospheric mantle, the characterics of palaeozoic era lithospheric mantle, mantle thermal state, and diamond metallogentic mantle geological conditions in research field

    為達到研究目的,本文首次以喀拉喀什河和玉龍喀什河沿岸階地的幔源重砂(單斜輝石、鉻尖石類、鈦鐵以及石榴石)為研究對象,合鉀鎂煌斑巖等區內已發現的幔源巖石及其中地幔對該區地幔的組成、古生代巖石圈地幔特徵、巖石圈熱狀態以及該區金剛石成地幔地條件做了嘗試性的研究工作。
  8. The mineral of the shell is almost pure calcium carbonate, with some magnesium, formed of radiating crystals.

    蛋殼的幾乎為純碳酸鈣,還有一些鎂,形成放射狀
  9. The physicochemical properties and behaviors of potassium and related substances, material sources of potassium salts, metamorphoses and crystallization speciation of bitterns, as well as formation conditions and mechanisms of potassium deposits were discussed

    摘要討論了鉀及其有關的理化性和行為規律,鉀鹽的來源,鹽鹵的變分異,成條件和機制,認為富鉀熱液是形成鉀鹽床的重要的來源之一。
  10. It is made up of inorganic crystal and organic matrix

    尿石是異常生化的產,由無機體和有機基組成。
  11. It ' s well - known that nucleation consisted of homogeneous nucleation and heterogeneous nucleation. the organic matrix used as the template to induce inorganic crystal growth and simulate the biomineralization is actually to promote heterogeneous nucleation and inhabit homogeneous nucleation. urinary stone is a kind of product of unusual biomineralization

    眾所周知,過程中的成核有均相成核和非均相成核兩種可能,利用有機基做模板,誘導無機體生長,模擬生體內的化過程實際是促進非均相成核而抑制均相成核。
  12. Abstract : based on the ahievement of epitaxial growth in several perovskite oxide films, we discuss the importance of substrate temperature ( ts ) and substrate material in the epitaxial growth of perovskite oxide thin films. influences of ts on growth orientation and epitaxial threshold temperature were observed. the results indicate that during the growth of the oxide films the phase formation and growth dynamics should be taken into consideration. the threshold temperature for epitaxial growth depends on the substrate materials. this demonstrates the influence of substrate material on the initial nucleation and epitaxial growth

    文摘:在成功地外延生長超導、鐵電、鐵磁等多種性的鈣鈦構氧化薄膜的基礎上,討論影響氧化薄膜外延生長的一些因素.考慮到相形成和薄膜生長動力學,在利用脈沖激光淀積法外延生長氧化薄膜中襯底溫度是十分重要的工藝參數.襯底溫度對成相和生長薄膜的取向都有影響.考慮到薄膜是首先在襯底表面成核、成相併生長.因此襯底材料格的影響是不容忽視的.觀察到襯底材料對薄膜外延生長溫度的影響.在適當的工藝條件下,利用低溫三步法工藝制備得到有很強織構的外延薄膜.這突出表明界面層的相互作用對鈣鈦構薄膜的取向有著相當大的影響
  13. Geologists refer to these trace elements as incompatible ? that is, they do not fit well into the crystal structures of common rock - forming minerals

    學家指出,這些微量元素不相容,意即它們不相容於一般形成巖石的構內。
  14. High - latitude calcareous phytoplankton and zooplankton might share a similar fate, although their declines would come decades later because their shells are formed from calcite, the less soluble form of calcium carbonate

    高緯地區的鈣浮游植和浮遊動可能有相似的命運,雖然它們受到影響的時間也許會晚數十年,因為鈣浮游生的外殼由方解石形成,這種碳酸鈣比較不容易溶解。
  15. The second stage is stage of the matter transfers the activated matter, that is to say, minerals build up their surface area after passing though physical weathering, maifan stone form a lot of clay mineral, oxide, oxhydroxide and collide mineral after passing though chemical weathering. it makes nutrition elements transform from crystal state to adsorption state and it expands the activation of mineral, in the latter stage, it makes maifan stone have many special physicochemical adjusting character, for example, ph and foi bi - directional absorptive and ion exchange character, so these characters expand maifan stone ' s uses

    第二階段為轉變的活性階段,即通過理風化增大表面積、通過化學風化形成大量粘土、氧化和氫氧化及膠體,使營養元素由態轉變為吸附態,從而大大增加了其活性。在後一過程中麥飯石還形成了許多特殊的理化學性,如ph值和f _ ( o2 )的雙向調節性,吸附性和離子交換性等,從而擴大了其用途。
  16. Comparing with the granitoid from jiaodong guojialing in mineralogy, the minerals in the granitoid in nimu - qushui granitoid crystallized in the environment of oxidization, the granitoid has a characteristic of rich volatile components and a high content of alkali, the rock - forming minerals and accessory minerals have a characteristic of i - type granite, and the granite shows a characteristic in favor of an and cu ore formation

    通過與膠東郭家嶺地區的花崗巖類的學進行對比,可知本區花崗巖類時處于氧化狀態,具有富含揮發分的特徵,堿含量高,造巖及副表現出型花崗巖特徵,具有殼幔混源,表現出有利於金、銅形成的花崗巖類的特徵。
  17. In australia, the aborigines believe the opal has a spiritual meaning. the wangkumara people have a legend which tells how their people gained fire from opal stones, with the assistance of a muda - a creator who switches from human form to pelican

    歐泊在學中屬蛋白石類,是具有變彩效應的寶石蛋白石,是一種含水的非的二氧化硅。內部具球粒構,集合體多呈葡萄狀、鐘乳狀。
  18. Hokutolite is a natural substance produced in the peitou creek about 90 meters downstream from the hot spring. as water from the spring flows into the stream it cools, and after a certain distance, when the temperature drops to around 80, the mineral - saturated water forms a crystalline deposit on the gravel bed of the stream

    北投石產于北投溪源頭下九十公尺處,當泉水與溪水混合流過一定距離后,在八十度左右的環境下,呈飽和狀態的就沈澱在河床礫石表面,形成
  19. 1. by means of the refining and purifying of sepiolite minerals, portions with low - crystallinity and impurity minerals which was not fit for being the catalyzer carrier were eliminated. the specific surface area of the refined sepiolite product increased to 236. 36m2 / g from the original 139. 66m2 / g

    通過對海泡石的精製提純,去除了中不適宜作催化劑載體的低部份和雜,使海泡石精製產比表面積由139 . 66m ~ 2 g提高到236 . 36m ~ 2 g 。
  20. In the past five years, however, geologists ? including my group at the university of wisconsin - madison ? have discovered dozens of ancient crystals of the mineral zircon with chemical compositions that are changing our thinking about the earth ' s beginnings

    然而,過去五年間,地學家(包括我們威斯康辛大學麥迪遜分校的團隊在內)發現了幾十個古代鋯石,它們的化學成份讓我們不得不改變對于地球起源的想法。
分享友人