澄江 的英文怎麼說

中文拼音 [dèngjiāng]
澄江 英文
chengjiang
  • : 澄動詞(使液體里的雜質沉下去) (of a liquid) settle
  • : 名詞1. (大河) (large) river 2. (指長江) the changjiang [yangtze] river 3. (姓氏) a surname
  1. But as a matter of fact, athropoda has some more complex characteristics than annelida, such as the exoskeleton, departmental body - plan and segmented appendages, which, as one parameter, results in the abundance of arthropod fossils in the chengjiang fossil lagerstatte

    但節肢動物還具有比環節動物更高級的特徵,如:身體分部、附肢分節;循環、生殖、排泄等系統均較環節動物復雜高級,這可能是澄江化石庫中節肢動物種數豐富的一個很重要的原因。
  2. During the primary research work of chengjiang biota, the paleontologists had an idea that the bivalved arthropod kunmingella douvilleiyas the dominant species because they found that eighty percent of the fossils they excavated in chengjiang fossil lagerstatte were kunmingella douvillei. and they also found that naraoia longicaudata, naraoia spinosa and isoxys auritus which belong to arthropoda were the sub - dominant species

    澄江生物群研究初期,雙瓣殼節肢動物朵氏昆明蟲( kunmingelladouvillei )化石數量占澄江化石庫中所有化石產量的百分之八十,因而古生物學家曾認為kunmingelladouvillei是該庫的優勢種。
  3. Since 1991, morphological and ecological investigation of the brachiopods in the early cambrian chengjiang lagerstatte has been done extensively and intensively

    澄江動物群腕足動物研究已進入了全面、系統的研究階段,對其生態學、形態學、分類學和埋藏學等不同方面均開展了深入而詳盡的研究工作。
  4. Based on a huge number of bachiopod fossils recently collected from haikou, kunming, the 5 known taxa of brachiopods in chengjiang fauna are further researched into and a new lingulid genus and a new species ( xianshanella haikouensis gen

    近些年來,隨著澄江化石庫研究的深入和大量化石的不斷發掘,澄江動物群腕足動物的形態解剖、生態和埋藏等各個方面均發現了許多新的信息。
  5. Is erected herein. a study of these brachiopod fossils demonstrates that the chengjiang lagerstatte has the potential to elucidate the character acquisition and character evolution of brachiopod in the early cambrian and to explore the earliest phanerozoic diversification of brachiopoda

    筆者在前人工作的基礎上,基於大量的野外觀察和室內整理,重點對澄江化石群中腕足動物的形態解剖和生態做出了進一步的解釋和補充。
  6. Helcionelloid mollusk from the lower cambrian heilinpu formation, chengjiang, yunnan

    雲南澄江早寒武世黑林鋪組軟體動物太陽女神螺
  7. The minerogenetic model of xikuangshan type copper deposit can be concluded that : in jinningian - chengjiangian, the activity of xiaojiang discordogenic fault form dextrorotation sub - structure in dongchuan ore area

    昆陽裂谷內的多數銅礦同位素成礦年齡多集中在9 . 0億6 . 5億年之間,屬于晉寧-澄江期,與rodina大陸裂解時限相當。
  8. A lagerst ? tte older than the burgess shale, in the chengjiang area of china ' s yunnan province, has yielded many important recent finds of soft - bodied organisms also characteristic of the cambrian explosion

    在中國雲南的澄江一帶,有著比伯吉斯頁巖更古老的特異埋藏點,已發掘出許多同樣具有寒武紀大爆發特色的重要軟體生物。
  9. Alkali basite, which came from upper mantle or lower crust, invaded through those structure, which not only bring cu et al mineralizing elements, but also the most important is that thermal energy. it cycled the formation water ( yinmin fonnation and luoxue formation ), and form alkali - rich, middle - high temperature and salinity fluid mixed with alkali - rich magmatic water. there were high rate of percolation and well voidage in the contact zone between yinmin purple stratum and yinmin rubblerocks, which is in favor of the transposition and mineralization of minerogenetic fluids

    因此,總結東川稀礦山式銅礦成礦模式為沉積( fe 、 cu ) ?熱液疊加( cu )改造:晉寧-澄江期,小深大斷裂發生走滑運動,在東川礦區造成右行旋扭及其派生構造,形成「 z 」字形落因破碎帶,同時來自深源(下地殼或上地幔)堿基性巖漿侵入,不僅帶來了大量cu等成礦物質,更重要的是提供了熱源,促使地層水(落雪組白雲巖和因民組紫色層)循環,與富堿( na和k )巖漿水混合,形成富堿中高溫高鹽度流體。
  10. D ) the invasion of jinningian - chengjiangian alkali basite were unambiguous, the distribution of those rocks form " z " in shape, which similar with luoyin fracture zone and the distribution of copper deposit. it shows that copper deposits were controlled by discordogenic fault and its derived sub - structure, and there are relationship between copper deposit and jinningian - chengjiangian alkali basite. e ) most of minerogenetic age of copper deposit, which located in kunyang rift valley, belongs to jinningian - chengjiangian ( between 900 - 650ma ), similar with the time limit of breaking - up of rodinia

    東川礦區晉寧-澄江期堿基性巖侵入活動明顯,常作為因民組復雜角礫巖膠結物和巖脈(體)產出,多分佈於深大斷裂及其派生的次級構造附近,明顯受南北向小深大斷裂走滑運動引起的右行旋扭及其派生構造控制,與「落因破碎帶」和「銅礦分佈」較吻合,均為「 z 」字形。
  11. This most intimate relationship between different genera has not been reported before in chengjiang fauna. 5. based on the material of chengjiang fauna, the evolution of introverts were discussed in chapter v. the early introverts have been divergent in the early cambrian

    在cricocosmiajinningensis表面發現附生的可能的腕足動物inquilinushaikouensisgen . etsp . nov . ,這種不同物種之間的迄今為止最為親密的關系在澄江動物群研究中尚屬首次報道。
  12. 5 ) the lophophores at trocholophe stage in heliomedusa orienta are tentatively interpreted here. 6 ) the mineralization of the animal took place gradually from outside to inside during their preservation before the fresh carcass were broken down, which could have given access to the preservation of the softy anatomy of organisms in chengjiang fauna

    第五章基於澄江動物群中的腕足動物化石,對腕足動物的演化做了初步的探討,認為腕足動物在早寒武世己經出現了大量的分異,其形態己經相當進化。
  13. According to a record written during the reign of qing dynasty s emperor kangxi, the stone which was used as the caves gate was like fungus and clouds, thus getting a name zhiyun

    康熙澄江府志路南州志雲: 「芝雲洞,硐門石似芝與雲,故名。 」
  14. The geological setting of chengjiang biota firstly, the pattern of chinese tectonic has been cited, which can help us to understand the place of china in the world clearly and easily. secondly, the lower cambrian of china and the early cambrian geomorph of eastern yunnan have been included

    澄江生物群的地質構造背景首先介紹了中國區域大地構造格局,其次是關于中國的寒武系和滇東地區早寒武世古地理概貌的論述,緊接著是澄江化石庫的古地理概貌。
  15. C ) copper ore body surrounded iron ore body ; iron ore were interpenetrated by copper ore stringer vein, which indicated that copper form late than iron. metallogeneti age is 826 230ma, similar with the age of alkali basite and age of other copper deposit in dongchuan ore area, which belong to jinningian

    黃銅礦單礦物的re - os同位素年齡研究表明其成礦年齡為826 230ma ,接近礦區堿基性巖年齡,與昆陽裂谷內其它類型銅礦成礦時代相當,均屬于晉寧?澄江期; 4
  16. The distribution of chengjiang biota in this part some new localities in wuding, anning, yiliang, haikou, and so on, which are discovered by eli field work team, are showed

    澄江生物群的分佈這一部分內容談及了武定、海口等幾個澄江縣以外的化石產地。
  17. 40ar - 39ar age spectrum of chengjiang fauna horizon

    澄江動物群產出層位
  18. No. 1 - 4, xiebei qianjia village, chengjiang town, jiangyin, jiangsu, china

    陰市澄江鎮謝北村錢家村1 - 4號
  19. It indicates there are close relationship between the forming of copper deposit in kunyang rift valley and the breaking - up of rodinia

    表明東川礦區銅礦形成與深大斷裂及其派生次級構造和晉寧?澄江期堿基性巖侵入活動關系密切; 5
  20. Jianshan section of haikou was measured and described and some monospecific layers were reported in chapter i. 2. several phyla of introverts are briefly introduced in chapter ii. 3

    第三章對澄江動物群化石中的蠕蟲化石的保存、埋藏、生態等方面作了進一步的研究探討。
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