輝石組 的英文怎麼說

中文拼音 [huīdàn]
輝石組 英文
pyroxene group
  • : Ⅰ名詞(閃耀的光彩) brightness; splendour; brilliance Ⅱ動詞(照耀) shine
  • : 石量詞(容量單位, 十斗為一石) dan, a unit of dry measure for grain (= l00 sheng)
  • : Ⅰ名詞1 (由不多的人員組成的單位) group 2 (姓氏) a surname Ⅱ動詞(組織) organize; form Ⅲ量詞(...
  1. Mineral constituents consist mainly of jadeite, aegirine - augite, magnesio - riebeckite, winchite, magnesio - hornblende, actinolite, quartz, albite, rutile and sphene

    主要成礦物為硬玉、霓、鎂納閃、藍透閃、鎂角閃、陽起英、鈉長、金紅和榍
  2. 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、英、、角閃、雲母、長等礦物(族)在成因上的宏觀標志和微觀信息,以及其成因信息在成巖作用和成礦作用中的地質意義。
  3. The assemblage of garnet - diopside in the silicate alteration rocks is different from that in the skarn of traditional idea

    硅酸鹽蝕變巖中的「榴子合與傳統理解的「夕卡巖」內的相同合名同實異。
  4. The ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical ophiolite suite

    摘要該蛇綠巖帶的巖體由地幔橄欖巖成,主要巖類型是方橄欖巖和純橄欖巖,缺少典型蛇綠巖剖面中的洋殼單元。
  5. 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,綜合本區幔源礦物和地幔巖的特徵以及地球物理資料,得出如下結論:本區上地幔的物質成有尖晶橄欖巖、二巖、單斜巖、純橄欖巖、方橄欖巖、橄欖巖、金雲母二橄欖巖、榴巖;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,不同來源的相同礦物中主元素的含量差異較大;地質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 ;從幔源重砂礦物的溫壓估算結果,可以推斷出巖圈厚度可達204 . 9km ;綜合巖圈物質成特徵、巖圈熱狀態、地幔溫壓狀態、氧逸度以及幔源巖和幔源礦物的化學成分,認為研究區具備了金剛成礦地幔地質條件。
  6. 4. it is the first time that eclogite conglomerates are discovered in maotangchan and fenghuangtai formations. this suggests that ultra - high pressure metamorphic rocks in the dabie orogenic belt exhumed to the earth ' s surface in lower cretaceous. the geochemistry data indicates that the protoliths of the eclogite gravels formed in a structure setting of volcanic arc

    首次在毛坦廠、鳳凰臺中發現了榴巖礫,這一發現表明大別造山帶超高壓變質巖在早白堊世已經折返到地表,而且地球化學研究表明這些榴巖礫的原巖形成於巖漿島弧構造背景。
  7. Shock wave compression technique has play an important role in the understanding of the material composition thermodynamic state and physical properties of the earth ' s ulterior. in this article, the stabling of high - pressure phase of one of the main candidate materials of the earth ' s lower mantle ? enstatite ( mg0. 92, fe0. 08 ) sio3 were investigated through the experimented measurement of hugoniot equation of state, and together with thermodynamic calculation and analysis

    本學位論文以沖擊壓縮技術為手段,從測量其hugoniot物態方程入手,結合高壓物理和熱力學理論分析,較深入地研究了下地幔中的一種主要候選分頑火( mg _ ( 0 . 92 ) , fe _ ( 0 . 08 ) ) sio _ 3在與下地幔大致相當的溫度壓力條件下的相態-鈣鈦礦型結構的相穩定性。
  8. The ore ' s mineral component is simple, and its main association of minerals are leucocratic sphalerite - galenite ? iopsite ( epidot, chlorite ). leucoratic sphalerite and diopsite are the guide minerals in the ore

    主要礦物合為淺色閃鋅礦-方鉛礦-透(綠簾、綠泥) ,其中淺色閃鋅礦和透為該類礦的標型礦物。
  9. The ore minerals are mainly composed of marmatlte, galenit, pyrrhotite ( pyrite ), chalcopyrite, or marmatite, galenite, pyrite and hedenbergite. marmatite and hedenbergite are the indicated minerals of the ore

    主要礦物合為鐵閃鋅礦-方鉛礦-磁黃鐵礦(黃鐵礦) -黃銅礦或鐵閃鋅礦-方鉛礦-黃鐵礦-鈣鐵,其中鐵閃鋅礦和鈣鐵為該類礦標型礦物。
  10. At its height in the 12th century, the castle consisted of a gatehouse, a keep, two towers, and a vaulted chapel enclosed within two high stone curtain walls

    城堡在12世紀達到了煌的最高峰,由一座城樓、一座要塞、兩座城塔和一座被兩道高大的幕墻包圍著的拱狀小禮拜堂成。
  11. High - mg volcanic rocks approach the primitive mantle compositions, and their magmatic source is close to the composition of bse, derives from the lower mantle and formed by this type - mantle rocks " fractional melting highly ( > 25 % ). high - mg volcanic magma, formed in the axis of the emei mantle plume, underwent the crystallization differentiation of olivines and some pyroxenes ; some olivines reflect fair cumulus crystallization

    高鎂火山巖接近於原始巖漿的成,巖漿源區與地球平均成分bse的成分特徵相近,起源深度為下地幔,為該地幔巖較高程度的部分熔融( 25 )而形成的。高鎂火山巖處于地幔柱的軸部,經歷了橄欖及一定程度的分異結晶,並且橄欖顯示出一定的堆晶作用。
  12. In this thesis, a kind of reversible immobilization method based on the plasma - polymerized film ( ppf ) used for effective immobilization of active bio - molecules and easy reproduction of sensors is developed. the surface of quartz crystal microbalance ( qcm ) is firstly prepared with plasma - polymerized film of butyl amine by glow - charge technique and then covered with a negative - charged polyelectrolyte by self - assembling. through strong electrostatic attraction, antibodies ( antigens ) positive - charged are immobilized for the determination of antigens ( antibodies )

    本論文基於等離子體聚合膜,設計了一種既能固定生物活性物質又易於傳感器再生的可逆固定化方法,即採用光放電的等離子體沉積技術,先在英晶體上沉積一層正丁胺等離子體聚合膜,再在膜上自裝一層帶負電的聚電解質,用以靜電吸附固定抗體(抗原)測定抗原(抗體) 。
  13. A new species of jadeite - eclogitic jade from myanmar, consisting mainly of garnets and omphacites, has been identified, which is a new member of the sort of omphacitic jade, and is also a new type of eclogites

    摘要在緬甸發現一個翡翠新品榴翠,其主要成礦物為和綠,是綠質翡翠類的新成員,也是榴巖的新類型。
  14. Such features can be ascribed to lower degrees of partial melting and greater melting depths. in particular, the decoupling between the lowest nag and highest tig tends to indicate residual jadeite during melting process so that na behaved as a moderately compatible element to lower the naao concentration in these rocks. this is consistent with the ree patterns in the high - ti diabases that have the highest ( gd / yb ) cn ratios than other two groups, which suggest a more important role of residual garnet in generation of the primary magmas

    運用mgo = 8進行標準化,結合巖成因理論討論了三大系列綠巖的形成相對深度和熔融比例,其中高ti系列的原始巖漿形成深度大,熔融比例小,源區相對最為富集易熔分;低ti系列的熔融深度最淺,比例最大,源區相對虧損易熔分;過渡ti系列則介於前兩大系列之間。
  15. 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礦物(單斜、鉻尖晶類礦物、鈦鐵礦以及)為研究對象,結合鉀鎂煌斑巖等區內已發現的幔源巖及其中地幔物質對該區地幔物質的成、古生代巖圈地幔特徵、巖圈熱狀態以及該區金剛成礦地幔地質條件做了嘗試性的研究工作。
  16. Directions are obtained by two means : calculation and measure. our investigations are summed as follows : 1 the lpo relations between olivine and orthopyroxene are different from usually situations : 100ol 001opx, 010ol 100opx, 001ol 010opx ; 2 the seismic anisotropy of the ultramafic rocks in damaping is obvious. their characters are consistent with the structures of the rocks and fabrics of minerals, which means seismic anisotropy is mainly controlled by rocks fabrics ; 3 seismic velocities suggest that the composition of upper mantle in damaping region is resemble to the xenoliths, which major component is lherzolite

    不同2大麻坪地區幔源包體的波速各向異性顯著,巖的波速各向異性特徵與其宏觀構造和微觀構一致,說明巖構是造成地震波速各向異性的決定因素3由地震波速推測的大麻坪地區的上地幔成分與包體出露的情況一致,即主體為二橄欖巖。
  17. The healing power of purple jade is similar to the amethyst. it boosts production of hormones, tunes the endocrine system and metabolism, strengthens the immune system, and cleanses the blood. it eases headaches and releases tension, reduces bruising, injuries, and swellings

    一般常把紫玉誤認為紫玉髓,其實是兩種完全不同的東西,因為紫玉髓是紫色的瑪瑙,屬于英類,而紫玉是有連鎖顆粒結構的結晶成,屬于硬玉的一類。
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