鹽古 的英文怎麼說

中文拼音 [yángǔ]
鹽古 英文
shioko
  • 鹽 : 名詞1. （食鹽; 鹽類） salt 2. （姓氏） a surname
  • 古 : Ⅰ名詞1 （古代） antiquity; ancientry 2 （先哲的遺典、道統） books or orthodoxies of ancient sages...
  1. Archaeology research of salt industry at zhongba ruins

    中壩遺址的鹽業考古研究
  2. Such low levels of sulfate indicate that the archean atmosphere was virtually devoid of oxygen

    如此低的硫酸鹽濃度，表示太古代大氣中的氧氣極為稀薄。
  3. Many carbonate masses older than middle palaeozoic are of dolomite rather than calcite.

    中古生代以前的許多碳酸鹽類礦物是白雲石而不是方解石。
  4. Due to a lack of understanding salt - making method in ancient china, people tend to equate boiled salt with decocted salt

    摘要由於不諳古代制鹽法，人們往往將「煎鹽」與「煮鹽」混為一談。
  5. One of the oldest method of salt removal is dialysis.

    透析是最古老的去鹽方法之一。
  6. Abstract : based on the synthetical data from the remote images, geological section, geomorphologic landscape, ancient water system evolution and surface feature spectrum etc, the study indicates that there is an undersand lake in the northern peripberal belt of qarhan salt lakes of qaidam basin

    文摘:根據地球衛星遙感影象、地物波譜測定以及地貌景觀、古水系演化和地面地質調查等資料的綜合研究表明，柴達木盆地察爾汗鹽湖礦區北部外圍地帶存在一種新的成因類型的鹽湖? ?沙下鹽湖。
  7. A study on the holocene transgression and the xigang ancient seabar in the yancheng area

    全新世海侵與鹽城市西岡古砂堤研究
  8. These geomorphic units of paleogeography constitute the basic model of paleocontinent, littoral - neritic sea and carbonate plateform at that stage, and this depositional model is similar to the pattern of the east china continent and ocean, which is the result of evolution during the past long geologic age

    這些古地理地貌單元構成了湖北省泥盆紀時期古陸濱淺海和碳酸鹽巖臺地的基本沉積模式，這種沉積模式與現今中國東海大陸、海洋格局基本一致，亦是經過了漫長地質歷史時期演化，而形成現今這種格局的。
  9. According to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field, including lithology, size distribution, sedimenta ry structure, geochemistry and paleontology etc., the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt. it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal. the peat flat is the important paleoenviron ment for coal accumulation. the tidal channel destroys the coal bed. the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation

    根據肥城煤田石炭系太原組的巖性、粒度分佈、沉積構造、地球化學及古生物等沉積特徵，將該區晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環境，認為太原組形成於潮汐作用為主的陸表海海岸，泥炭坪是成煤的重要古地理環境，潮渠對煤層有一定的破壞作用，地殼的脈動性振蕩作用是控制沉積環境演化和聚煤作用的主要因素。
  10. Abstract : according to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field, including lithology, size distribution, sedimenta ry structure, geochemistry and paleontology etc., the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt. it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal. the peat flat is the important paleoenviron ment for coal accumulation. the tidal channel destroys the coal bed. the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation

    文摘:根據肥城煤田石炭系太原組的巖性、粒度分佈、沉積構造、地球化學及古生物等沉積特徵，將該區晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環境，認為太原組形成於潮汐作用為主的陸表海海岸，泥炭坪是成煤的重要古地理環境，潮渠對煤層有一定的破壞作用，地殼的脈動性振蕩作用是控制沉積環境演化和聚煤作用的主要因素。
  11. From studies of these characteristics of structures, palaeontology, drilling, well logging, seismic profile, salt chemistry and lacustrine sedimentary system, it is recognized that the new characteristics occur in of section pukou and in huaiyiri sag, and the huge thickness of salt rocks is formed by the crust salt materials upwelling along deep fracture in the form of hot bittern and entering lacustrine basin in this area

    通過該區構造、古生物、鉆井、測井、地震、鹽巖化學及湖盆內沉積體系等特徵的研究，認為淮陰凹陷浦口組二段和三段的沉積構造有其特殊性，巨厚的鹽巖層是殼深部鹽類物質沿深大斷裂上涌以熱鹵水形式進入湖盆的結果。
  12. The main results are following : ( 1 ) the variation of clay / silt ratio can indicate the secondary clay action of dust depositions ; the variations of magnetic susceptibility and total fe content are inferred to be records of the changeable intensity of bio - pedogenesis ; the variations of sr content and rb / sr ratio can indicate bio - pedogenesis, dissolving and leaching action ; the content of total organic carbon ( toc ) can reflect variation of climate and vegetation during soil formation, it indicates the intensity of weathering and bio - pedogenesis ; the content variation of caco3 can show the intensity of dissolving - leaching action and secondary deposit, which was noted as pseudomycilia in pores and fissures in the sediment, so it can indicate the intensity bio - pedogenesis quite well. these proxy indexes also reflect obvious regional difference of pedogenic environment and the intensity bio - pedogenesis ; namely, secondary clay action, dissolving - leaching action and bio - pedogenesis are all much stronger in south than that in north

    實驗結果表明：粘粒粉沙比值能很好地指示粉塵堆積物的次生粘化作用；磁化率和全鐵很好地指示生物風化成壤作用； sr和rb sr比值能很好的指示生物風化成壤作用和淋溶作用；總有機碳（ toc ）含量的高低，在一定程度上反應了土壤發育過程中氣候和植被狀況的變化，指示著成壤過程中腐殖質化的程度； caco3含量的變化，可以反映了黃土古土壤形成時的風化成壤作用的強弱程度，指示成壤過程中的淋溶作用和次生碳酸鹽化作用；並且各指標所指示的成壤環境和成壤強度存在明顯的區域差異，即渭河流域土壤的生物風化成壤作用、次生粘化作用和淋溶作用均表現出南部強于北部。
  13. Culture - dependent extremely halophilic archaea isolated from heijing ancient salt mine, yunnan

    雲南黑井古鹽礦可培養極端嗜鹽古菌初步研究
  14. Promoter function study of rm07 dna fragment in halophilic archaea

    片段在嗜鹽古生菌中的啟動子功能研究
  15. Development of the genetic transformation system in extremely halophilic archaea

    極端嗜鹽古菌遺傳轉化系統的研究
  16. Diversity of halophilic archaea in hypersaline lakes of inner mongolia, china

    內蒙古錫林浩特地區嗜鹽古菌多樣性的研究
  17. Microcalorimetric study on deletion mutagenesis of the gene promoter sequences from the extremely halophilic archaea

    極端嗜鹽古生菌啟動子序列缺失突變的微量熱研究
  18. The entire halcs gene is located on a megaplasmid and contains a 849 - bp open reading frame that encodes a polypeptide of 283 amino acids. the promoter is typically haloarchaeal, but the start site of transcription is only seven bases from the 5 ' end of the initiator aug codon, making the halcs transcript another example of a " leadless transcript " in the haloarchaea

    它的一29一24位置上是一「毛幻人」 box序列，為典型的嗜鹽古菌啟動子;它的轉錄起始位點距離「 atg 」只有7個核普酸，也是典型的嗜鹽古菌的「卜adless靦script 』 』 。
  19. The source of the water has been confirmed according to its geochemistry characteristics, reference formation water characteristic parameters and water classification by taking the carbonate buried hill reservoir of ordovician in lunnan area of tarim basin as an example

    以塔里木盆地輪南奧陶系碳酸鹽古潛山油氣藏為例，根據測試水的地球化學特徵，參考地層水標準參數和測試水分類，確定了測試水的來源。
  20. The purification of this halocin was achieved by combination of tangential flow filtration ( tff ), sephadex g50 and deae - sepharose chromatography. the n - terminal amino acid sequence was also determined by edman degradation

    Halc8對大多數的極端嗜鹽古菌（包括部分嗜鹽堿古菌）有抑制作用，但對細菌則無明顯的抑制作用。
分享友人
分享到 Line

分享到臉書