白晶白雲巖 的英文怎麼說

中文拼音 [báijīngbáiyúnyán]
白晶白雲巖 英文
baroque dolomite
  • : Ⅰ形容詞1 (似雪的顏色) white 2 (清楚; 明白; 弄明白) clear 3 (空的; 沒加他物的) pure; clear; ...
  • : Ⅰ形容詞(光亮) brilliant; glittering Ⅱ名詞1. (水晶) quartz; (rock) crystal 2. (晶體) any crystalline substance
  • : Ⅰ動詞[書面語] (說) say Ⅱ名詞1. (雲彩) cloud 2. (雲南) short for yunnan province3. (姓氏) a surname
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • 白晶 : jing bai
  • 白雲 : bai yun
  1. The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ), micritic limestone, grainstone and micritic dolostone which were laid down in the shallow - water to bathyal, high - salinity and enclosed to semi - enclosed lake systems

    五道梁群湖相碳酸鹽分為生物粘結灰(疊層石) 、泥、顆粒灰與泥四大類,反映出沉積環境為一個具有淺水半深水、高鹽度、半封閉封閉特點的綜合湖泊系統。
  2. The microfacies of carbonate rock of the wudaoliang group in hoh xil basin is divided for marl lithofacies, micrite facies, micrite ( spar ) scraps ash lithofacies, grain scraps micrite facies, dolimite rock lithofacies, and the stromatolite ash lithofacies

    可可西里盆地五道梁群碳酸鹽微相類型主要為泥灰相、泥相、泥(亮)粒屑灰相、粒屑泥相、相、疊層石灰相、核形石灰相等7種微相。
  3. The fluids upwelled to seafloor along fault thus ore - forming metals accumulated. 2. this paper indicated the definition the hydrothermal sedimentary rocks. the definition is a group of especial sedimentary rocks forming at the temperature ranging from 70 ? to 350 ? ( or more high ) through sedimentation and synsedimentary metasomatism in the seafloor

    區內的熱水沉積主要有硅質、鈉鉀長石、重、透閃石、碳酸鹽、綠泥石和鐵石斑點千枚,它們往往與熱水沉積礦體緊密伴生。
  4. We find that the petrology characteristic of all the samples have no characteristic of meteoric water such as geopetal structure, infiltrative sand, ( uniform cement and gravitational cement on base of the research of the dolomite in the regions. on the dot diagram of combination of mgco3 ( mol % ) and sr, the dot are all close to the line of seawater whether they are microlite - crystalline penecontemporaneous dolostone or diagenetic dolostone of various crystals. the 87sr / 86sr value of dolostone or matrix is less than the one of sparry calcite in cave or vein, and close to the value of seawater

    通過本區的研究發現:已有的樣品的石學特徵沒有顯示出如示底構造、滲濾沙、新月型膠結物和重力膠結物等大氣淡水作用的特徵;在石mgco _ 3mol百分數和石sr含量的投點圖中,無論是準同生成因的泥?微,還是粉?細(或中,或細以上的不等)的成,均投在海水線的附近;(或基質)的~ ( 87 ) sr / ~ ( 86 ) sr比值顯著低於與孔洞或脈中充填的亮方解石,且與海水值十分接近, ~ ( 13 ) c和~ ( 18 ) o值顯著高於孔洞或脈中充填的亮方解石,也偏向于海水值; mn含量則顯著低於孔洞或脈中充填的亮方解石。
  5. This paper emphasizes the effect of the dissolution of aluminosilicate during diagenesis may provide more radiogenic strontium which would result in a high content of strontium in carbonate rocks. so we should avoid the vein of carbonate and select the samples with less terrigenous clastic, less grain content and lacking calcite cementation collected as analysis samples. the microcrystalline limestone and micro - to fine - crystalline dolomite are rather fairly whole rock samples

    作者還強調了成過程中由長石等鋁硅酸鹽溶解提供殼源sr所造成的碳酸鹽礦物成蝕變可能表現為較高的sr含量;因此,在用全樣品進行旨在反映海水組成的各種分析時,應迴避碳酸鹽脈,選擇含陸源碎屑低、顆粒數量少、缺乏方解石膠結物的樣品,微或微?粉是較為理想的全樣品。
  6. The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures

    原生石為亮鮞粒石灰和泥鮞粒石灰石化作用使其石結構大多遭受破壞。
  7. The lower part is a micro - tidal range evaporative tidal sequence consisting of thin - bedded gypsum - bearing, muddy - limestone and dolomicrite

    下部為薄層的含石膏、硬石膏體、團塊及腸狀石膏層的泥、微組成的小潮差蒸發潮坪層序。
  8. The upper part is a set of evaporite quasi - tidal sequence with clear cycles which is made up of middle - thin - bedded, gypsum - bearing muddy limestone and dolomicrite

    上部為中薄層狀富泥的含石膏質夾層的泥質泥、微組成的旋迴性清楚的似蒸發潮坪層序。
  9. These biostromes and bioherms, together with tidal - flat dolomicrite and muddy dolostone, form circum - tidal flat meter - scale carbonate cyclic sequences with symmetrical facies sequences and fabrics

    它們與潮坪相泥和泥質構成具對稱相序組構的環潮坪型碳酸鹽米級旋迴層序。
  10. Crystalline dolostone is formed by seepage - reflux dolomitization and burial dolomitization

    有兩種成因:一為迴流滲透石化;二為深埋藏石化。
  11. According to whether remnant grains exist, post - penecontemporaneous dolostone can be divided into remnant grain dolostone and crystalline dolostone

    準同生后根據殘餘顆粒的有無可分為殘餘顆粒兩大類。
  12. Now, have ascertained preliminarily that the mineral resource in boundary has tin, alluvial gold, lead, zinc, crystal stone, mica, reasonable stone and the kind of white marble, animal resource has wild ox and blue sheep, dian golden monkey, little panda and black bear etc., medicine has yellow company and day flax with plant, fu ling, shellfish mother and ox night, qiang work

    目前已初步探明境內礦物資源有錫、沙金、鉛、鋅、水石、母、在理石、漢玉類,動物資源有野牛、羊、滇金絲猴、小熊貓、黑熊等,藥用植物有黃連、天麻、茯苓、貝母、牛夕、羌活。
  13. These characteristics have close relation with transgression from eastern to western. 4. reefs undermined various and complicated diagenesis, in which cementation, dolomitization and corrosion etc. play main roles in the history of reef diagenesis

    4礁的成作用具多樣性和復雜性,其中泥化、填積、膠結、化和溶蝕作用最為重要。
  14. The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement, while the cover has undergone the evolution of intra - continental rife in permian, down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary. the main sediments are huge - thick volcanic rock, shallow intrusive rock and tuff in early permian, dark mudstone, marl and muddy dolostone in lucaogou formation in middle permian, huge thick volcanic rock, intruder in tiaohu formation in middle permian, miscellaneous sandy gravel, sandstone and gray mudstone in triassic ( the red is under the gray, and huge - thick dark gray, gray sandy gravel, sandstone, mudstone with coal layer in jurassic

    盆地基底由前寒武紀結基底和古生代褶皺基底組成,盆地蓋層則經歷了二疊紀的裂谷盆地、三疊紀?堊紀的坳陷盆地和第三紀后的山間盆地的演化過程。盆地主要沉積了下二疊統巨厚火山、淺成侵入和凝灰;中二疊統蘆草溝組的暗色泥、泥灰石以及條湖組的巨厚層火山、侵入;三疊系雜色砂礫、砂及灰色泥(下紅上灰) ;以及侏羅紀厚層深灰、灰色砂礫、砂、泥夾煤層。
  15. Were found in the margin around the basin. lucaogou fm. was mainly composed of thick dark mudstone, micritic limestone, argillaceous dolomite, which reflected a shallow to fairly deep - lake sedimentary formation

    蘆草溝組在盆地內部發育厚層暗色泥、泥、泥質等,反映陸相淺一半深水沉積建造。
  16. The dolostones have experienced several types of post - depositional diagenetic modifications, of which dolomitization, dissolution, recrystallization and tectonic stress processes have exerted an important effect on porosity and permeability

    認為該在沉積期后變化中經歷了多種成作用改造,其中影響儲集性的作用主要有石化作用、溶蝕作用、重結作用和構造應力作用,對孔滲改善起了積極作用。
  17. In the scenic area, there is an exotic and beautiful underground cave, which is called white cloud cave or crystal palace, and is belonged to underground lava topography

    景區內還有神奇瑰麗的地下溶洞,人們稱之為洞或水宮,屬地下溶地貌。
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