寒武系的 的英文怎麼說

中文拼音 [hánwǔxìde]
寒武系的 英文
cambrian
  • 寒 : Ⅰ形1 （冷） cold 2 （害怕; 畏懼） afraid; fearful; tremble （with fear） 3 （貧困） poor; needy 4...
  • 武 : Ⅰ形容詞1 （關于軍事的） military 2 （關于技擊的） connected with the art of attack and defence in...
  • 系 : 系動詞（打結; 扣） tie; fasten; do up; button up
  • 的 : 4次方是 The fourth power of 2 is direction
  1. 2. tazhong ancient uplift originated from normal fault in paleozoic, hydrocarbon formed in ordovician period, structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period, and it provided geologic background for the deposit of silurian - devonian stratum. tazhong uplift formed at the end devonian, ancient reservoir was destroyed and asphaltum sandstone formed, structure deformation more destroyed ancient reservoir in early permian, after then the major of structure deformation is regulation

    塔中隆起源於早古生代拉張背景下的正斷層，寒武-奧陶紀為其烴源巖形成的重要時期；早奧陶世末-晚奧陶世末的構造反轉是塔中隆起的主要形成期，同時也為志留系形成地層及復合圈閉提供了古地理背景；志留?泥盆紀塔里木盆地南北緣均轉為活動大陸邊緣，形成了大量的斷裂和不整合；泥盆紀末塔中鼻狀隆起基本定型，古油藏遭受破壞，形成了瀝青砂巖；早二疊世晚期的構造變形使古油藏遭受進一步的破壞；二疊紀后構造變動主要以調節為主。
  2. A new global chronostratigraphic subdivision of cambrian system into 4 series and 10 stages has been developed to replace the tripartite traditional framework of the system, which has been used for more that 170 years

    摘要重新劃分全球寒武系年代地層為4統和10階，取代了國際地學界沿用了近170年的上、中、下3統的傳統劃分框架。
  3. The status of cambrian system in the 2004 version of the international stratigraphical chart is reviewed with comments on the gssp for the base of the system and the current subdivision of the system, the gssp for the newly ratified furongian series and paibian stage, and the time span of the system and its series

    摘要評述了國際地層委員會最新公布的2004年版「國際地層表」的寒武系部分，包括它的底界全球層型和點位的確定和存在的問題、寒武系當前的再劃分情況、芙蓉統和排碧階及其底界全球層型剖面和點位、寒武系的時代跨度。
  4. Eight aspects related to the study of early precambrian metamorphic stratigraphy are dealt with in this paper : general situation of the study ; complexity of the stratigraphy and difficulties of the study ; thoughts and methods of the study ; division of rock suite, rock group and complex rock ; researches on important regional discordances ; types and characteristics of protolith and recovery of palaeoenvironment ; correct differentiation of the metamorphic strata, ttg rock system and other metamorphic plutonic rocks ; determination of the ages of the metamorphic strata

    摘要主要論述了與早前寒武紀變質地層（學）有關的8個方面的問題：早前寒武紀變質地層的研究概況；早前寒武紀變質地層的復雜性和研究難度；早前寒武紀變質地層研究的思路和工作方法；早前寒武紀變質巖石地層單位巖群、巖組和雜巖的劃分問題；重要區域性不整合的研究；鑒定變質地層的原巖類型、巖石性質和恢復古環境；正確區分變質地層和ttg巖系以及其他變質深成巖；變質地層時代的確定。
  5. The causes are discussed from aspects of oil - gas source beds, trapping and storing space, oil - gas migration channel and thick proofing layers, oil - gas maturity stage and allocation of effective trapping stage, suggesting the searching of primary oil - gas pool of the cambrian and lower ordovician at the relatively shallow layers and surrounding places with faults developed

    從油氣源層、圈閉與儲集空間、油氣運移通道與巨厚隔層、油氣成熟期與圈閉有效期配置等四個方面探討了未獲油氣之原因，提示在滿加爾坳陷腹地，相對較淺部位及周邊斷裂發育部位尋找寒武系和下奧陶統的原生油氣藏。
  6. But in contrast of the research of chemical weathering of other rocks, such as granites and basalts, the research of chemical weathering of black shales both in width and depth still remains much to advance. after reading and investigating widely, we selected lower - cambrian black shales and their weathering profiles in hunan province as research objects of our work at first. then, based on field investigation of weathering status of lower - cambrian black shales and it ' s relationship with soil composition and human activities in hunan, we studied changes of chemical composition such as major and trace elements before and after weathering of black shales by comparison

    根據文獻閱讀和野外調查，本文選擇了湖南安化、桃江、望城等地下寒武統黑色頁巖及有關風化剖面作為研究對象，並在查明湖南下寒武統黑色頁巖的風化現狀及其與土壤組成、人類活動的關系的基礎上，對比研究了黑色頁巖風化前後主量和微量元素等化學組成的變化，探討了元素的富集和遷移轉化機制以及黑色頁巖風化與區域環境質量的關系，得出了如下幾點主要成果和認識： （ 1 ） ti是黑色頁巖風化過程中的「不活動」元素，可作為參照元素，對其它元素的活動性進行質量平衡計算。
  7. Reservoir capacity of cambrian carbonate of foreslope facies in danzhai and sandu, eastern guizhou

    黔東三都-丹寨地區寒武系斜坡相碳酸鹽巖的儲集性
  8. The key point of this thesis is the strontium isotope composition and control factors of cambrian marine carbonate, upper yangtze platform, which the samples were collected from xiushan section in chongqing

    論文研究重慶市秀山溶溪寒武系海相碳酸鹽的鍶同位素組成及主要控制因素。
  9. This paper also discusses the strontium isotope evolution curve published over the world, present strontium isotope results of the section of cambrian in xiushan of chongqing

    本文評述了國際上已有的寒武系海相碳酸鹽的鍶同位素演化曲線，公布了重慶秀山寒武系海相碳酸鹽的鍶同位素分析結果。
  10. The lower paleozoic continent marginal sedimentary strata in the north kunlun massif are sinian - cambrian alajiaoyi group and ordovician pishigaisayi formation. the former is composed of high maturity flysch deposit, the later consist of continental shelf deposit such as carbonate and slate and sandstone. these rocks implies that they might form at passive continental margin

    與其曼于特蛇綠巖相關的早古生代邊緣沉積巖在昆北地塊上為震旦?寒武系阿拉叫依巖群、奧陶系皮什蓋薩依巖組，前者為一套成熟度較高的陸源碎屑復理石沉積，後者為碳酸鹽巖和含碳板巖砂巖等陸棚沉積，顯示其具被動陸緣性質。
  11. The section of the cambrian in xiushan of chongqing has been well re - appraised over again by studying its stratigraphy, sedimentary petrology, sedimentary facies and environment in this thesis

    通過較系統地研究重慶秀山溶溪寒武系剖面的地層學、沉積巖石學、沉積相及環境，本文對該剖面進行了重新認識。
  12. 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。
  13. It is believed that the distribution of gold deposits in fujian is controlled by regional deep - seated structure and precambrian volcanic flysch formation containing charcoal is main gold source rock. the accumulation of gold is closely related with yanshan granitic magma intrusion

    金礦空間分佈受一定的區域深部構造單元所制約，前寒武系富含炭質的火山復理石建造是福建省金礦的主要礦源巖，金的富集成礦與燕山期花崗巖類巖漿侵入作用密切相關。
  14. By the analysis for cambrian stratum in xiushan of chongqing, according to the mn / sr value of the marine carbonate of different structural components, the 28 % samples that ca n ' t stand for the original seawater in different structural components of the marine carbonate had strongly undergone diagenetic alteration

    按照碳酸鹽結構組分的mn sr比值，秀山溶溪剖面寒武系海相碳酸鹽的各種結構組分中有28的樣品具有較強的成巖蝕變性，其組成不能代表海水。
  15. Based on the test of cathodolummescence and the analyses of mn, sr, fe and mg of the marine carbonate samples collected from the sedimentary section of cambrian in xiushan of chongqing, southwest china, this paper assesses the preservation of different structural components for the information of cambrian sea water

    通過對重慶市秀山寒武系剖面海相碳酸鹽的陰極發光性和mn ， sr ， fe ， mg等元素分析，評估了寒武紀地層中各種碳酸鹽結構組分對海水信息的保存性及主要控制因素。
  16. According to petrology, biological assemblage and structural features of carbonate rocks, the sedimentary environments of formations of the carbonates in yichang area are reconstructed

    根據本區寒武系的巖石學特徵、生物組合特徵和沈積構造特徵重建了各組段的沈積壞境。
  17. Samples for strontium isotopic screened were selected by way of the test of cathodoluminescence, observation of thin sections, and analysis of sr and mn. the mn / sr value of all samples presented in this paper are less than 2, and the cathodoluminescence is dull, however, the samples from the cambrian underwent diagenetic alteration to a certain degree, and the plotted points of the thickness and 87sr / 86sr value are somewhat discrete. the strontium isotope evolution curve drawn from the data with relatively low 87sr / 86sr value are consistent with other curves based on samples from different areas of the world, supporting the notion of global consistency of strontium isotope composition of marine carbonates

    根據鋸同位素地層學的基本原理，利用已有的鋸同位素演化曲線，筆者確定重慶秀山寒武系剖面寒武系底界、下一中寒武統界線和中一上寒武統界線都應適當下移；另外嘗試確定了重慶秀山寒武紀剖面一些關鍵點的年齡，累積厚度1380m處的年齡為503 ? 509ma ，累積厚度1900m處的年齡約為500ma ，這對秀山寒武系剖面下、中寒武統和中、上寒武統界線的確定具有參考價值。
  18. The framework has been approved in a vote of the international subcommission on cambrian stratigraphy and adopted on 2005 and 2006 editions of " international startigraphic chart " by the international commission on stratigraphy

    該成果已被國際地層委員會寒武系分會表決通過，並在《國際地層表》採用，它的正式公布將加速寒武系內「金釘子」的確立的進程。
  19. Notes are also given on the problem related to the regional and local chronostratigraphic subdivisions of china

    討論了與我國寒武系年代地層的劃分和建立地方性、區域性年代地層系統的相關問題。
  20. In the third chapter, the paper describes the conceptual model of research area : in plane, the range and boundary of the model accords with that of tong - pu - he karst - groundwater sub - system ; in vertical, the model ranges from the bottom of cambrian to the phreatic surface

    第三章，確定研究區概念模型如下：在平面上，模型範圍與銅蒲合巖溶水系統范圍一致。銅蒲合巖溶水系統的邊界就是該模型的邊界。在垂向上，上至潛水面，下至寒武系底面。
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