積屑的 的英文怎麼說

中文拼音 [xiède]
積屑的 英文
hysterogenous
  • : Ⅰ動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
  • : Ⅰ名詞(碎末) bits; scraps; crumbs Ⅱ形容詞(瑣碎) trifling Ⅲ動詞(認為值得) think sth. worth doing
  • : 4次方是 The fourth power of 2 is direction
  1. Through the search of bourn of intraclast congeries silica rock, its earth and west side all grow consortium robble

    經對內碎硅質巖邊界研究發現,其東西兩側均發育有同生斷裂。
  2. While lixue produces the advantageous influence upon the chengzhaiti, it brings something disvantagesous. as follows : the narrow eyesight of poems, the lack of art chirm and the insignificant contents

    摘要在理學對誠齋體形成產生極影響同時,也給誠齋體帶來了一些負面效應,主要是詩歌視野狹窄;藝術魅力缺失;內容
  3. Ore area locate on, silver factory ditch - ancient tomb ditch in west branch river set lower bench, stratigraphic succession, rock assemblage are different with circumference. most is a set of intraclast congeries silica rock. in search of it, its distribution range in the silver factory ditch - ancient tomb ditch

    礦區所在部位銀廠溝?古墓溝一帶,西岔河組下段地層中,地層層序、巖石組合特徵與周邊地區存在明顯差異。主要為一套內碎硅質巖。
  4. Further research of lithofacies pvove : lode country output points belongs to tidal - flat facies. and the two sides belong to littoral facies - estuarine facies. ore area petrochemistry analyse also prove : intraclast congeries silica rock in basin have higher cu, ag abundance than circumference pena. the prominence inhomogeneity of the cu distribution indicates reconstruct of the late construction

    礦區內巖石化學測量也證明:盆地內發育內碎硅質巖比周圍巖石具有更高cu 、 ag元素地球化學豐度值, cu元素分佈顯著不均一性,表明了後期構造改造作用。
  5. Rapid melting of the snow saturated debris in a large landslide.

    急劇融化使大滑坡中飽和。
  6. Erlian basin is a rift lacustrine basin developed on the hercynian geosyncline folded base in early cretaceous, is featured by simple sedimentary feature, depositional cycle, small lacustrine transgressive, dry climate, salinization lacustrine water and multi - and - near sources

    摘要二連盆地是在海西期地槽褶皺基底上發育起來早白堊世斷陷湖泊群,具有湖盆湖浸規模較小、氣候條件乾燥、湖水咸化、沉旋迴單一,多物源、近物源和粗碎等沉特徵,以及發育巖性地層油氣藏為主油氣分佈特點。
  7. In the older rocks below these glacial deposits are detrital uraninite and pyrite, two minerals considered evidence for very low levels of atmospheric oxygen

    這些冰河沉物下方較老巖層,是瀝青鈾礦與黃鐵礦碎;這兩種礦物被認定為大氣中氧氣極為稀少證據。
  8. China is potential for gold mineral resources, especially for granite - greenstone hosted, meta - clastics - hosted, volcanics - subvolcanics - hosted gold deposit and sedimentary rock - hosted micro - disseminated gold deposits

    中國金礦找礦前景可觀,以產于花崗巖綠巖地體中金礦、產于沉巖中微細浸染型金礦、產于變碎巖中金礦和產於火山次火山巖中金礦最具找礦潛力。
  9. Many research such as clay minerals, suspend in the sea, the grain size trend analysis of surface sediment, poc 6 cu and 8 c13 in bottom sediments etc. showed that : the yellow sea warm current divided the south yellow sea into two, the terrestrial material of modern sediment on the west shelf plain mainly came from the modem yellow river suspend carried by the alongshore current, and the sediment difference between the west and east side of yellow sea trough was represented by the sedimentation thickness in postglacial period, sedimentation stratum, and oxygen isotope record

    粘土礦物、碳酸鹽、粗碎、海域懸浮體、表層沉物粒度趨勢分析、 poc c ~ ( 13 )及底質沉c ~ ( 13 )等多方面研究表明:以黃海暖流為主導,南黃海堆陸架平原西側現代沉物陸源物質主要源於黃海沿岸流攜帶現代黃河懸移物質,黃海槽東西兩側差異主要表現在冰消期以來沉厚度、沉層序、氧同位素記錄上。
  10. Based on the quantitative studies of siliceous microorganisms and terrestrial detritus in 12 surface sediment samples, which were recovered by the first chinese national arctic expedition team, in the bering sea, it goes without saying that diatom abundance is dominant within the microorganisms which consists of diatoms, radiolarians and sponge spicules

    摘要中國首次北極科學考察在白令海?取了12個表層沉物樣品,其中對矽質生物和陸源碎詳細研究發現,它們主要由矽藻、放射蟲和海綿骨針組成。
  11. Moreover, hrtem observations indicate that the process is very selective : even in apparently homogenous illite or i / s, some crystals went opening and some remain unchanged. and the replacement of k cations by alkylammonium cations is not restricted to crystal edges, but extends to entire interlayer. the above facts are the basis of alkylammonium cations method applied to the diagenetic age of sedimentary rock

    Iaa法是以沉粒度?年齡譜為基礎,利用這種方法可以獲得同一樣品不同粒級伊利石年齡,隨著粒級減小,樣品年齡也減小,當碎伊利石含量趨于零時,可以得到自生伊利石成巖年齡;烷基胺陽離子取代法是一種化學方法,利用烷基胺陽離子選擇性替代性,可以去除碎伊利石成分中k離子,從而能夠獲得自生伊利石年齡。
  12. The growth of larger objects from such small debris has long been one of the most puzzling questions regarding the accumulation of solid material.

    而由這些小粒長成較大天體,早已是關于固態物質最令人迷惑費解問題之一。
  13. The petrology revelas that the sedimentary environment of the study area is carbonate tide - flat and shallow sea which is also strongly affected by the volcanic materials and wind - brought clastics during the period of yangzhuang

    上述巖石特徵表明,研究區在中元古代薊縣紀早期楊莊期為淺海潮坪碳酸鹽沈環境,沈作用受中遠源火山物質和風攜碎強烈影響。
  14. As there are less such materials in loess as fossil, plants, slag, etc, which could be used for dating, luminescence dating, especially optically stimulated luminescence dating, was extensively applied to aeolian deposits, for its dating materials were minerals, such as quartz and feldspar

    由於黃土中所含化石、木質、炭等適于其它方法測年物質很少,同時,全新世黃土受年輕有機碳和無機碳影響較大,致使全新世黃土類沉測年迄今仍缺少理想方法。
  15. Based on the variation of light / heavy mineral components of sedimentary rocks, the typomorphic characteristics of various debris, the cathodoluminescence color of quartzes, the direction of paleocurrent and the extension of sedimentary facies, two source direction of the studied area in carboniferous and permian can be recognized, one is in bayanwusu, wulan ' ge ' er and hetaoyinshan area north of hangjinqi in the north margin of ordos, another is alashan area in the northwest margin of ordos

    在深入研究本區沉巖輕、重礦物組分變化、各種巖標型特徵、石英陰極發光顏色、古水流方向及沉相帶展布等基礎上,認為研究區石炭?二疊紀物源方向主要有兩個,分別為:北緣杭錦旗以北巴彥烏蘇、烏蘭格爾及河套陰山地區;以及研究區西北緣阿拉善地區。
  16. The thesis draws the following conclusion : ( 1 ) 11500 - 8500ab. p., through comprehensive analysis of these proxy climatic substitute indexes reveals : this was a period in which the temperature risen and the precipitation increased, but it was mainly still dry and cold ; the vegetation was prairie or forest prairie ; there were flood deposits in the dust sediments of late stage ; and it was the shifting period from the new stone age to the old stone age

    主要得到以下幾方面認識: ( 1 ) 11500 8500ab . p . ,綜合多氣候代用指標分析結果表明:本期氣候表現為溫度升高、降水增大好轉時期,但總體上仍以乾冷為主;結合很少發現較粗顆粒木炭情況推斷當時植被是草原或森林草原;研究發現在後期粉塵沉過程中有洪流沉
  17. But it is more fulfilling recognising our weakness and not dismissing it as just another irrelevant problem. the writer is a third year student of school of communication studies, ntu

    學習一種語文不是一件容易事,作法是認識我們弱點,不是不一顧,把它當成另一件無關緊要事。
  18. Two application softwares, the nmr calibration software and the fast nmr core analysis software, are programmed. the two softwares offer the specific calibration and fast measurement function of cuttings petrophysical parameters. the research results show that nmr technique has the advantage of fast, non - contact and independence of samples size and can be applied to the cuttings analysis

    研究結果表明,核磁共振分析技術具有快速、無接觸、與樣品外形體無關特性,不僅可以應用於規則形狀巖心樣品,同樣可以較好地應用於不規則小顆粒樣品,如巖分析。
  19. In support of this idea, later analysis of the sediment at wageningen university in the netherlands proved that many of the brown sand grains were indeed fragments of the dark - colored schists and other rocks that began washing away as the newborn andes rose up

    荷蘭瓦荷寧罕大學后來對于沉分析,證實了許多棕色沙粒確實是深色片巖及其他巖石,這些應該是新生成安地斯山隆起時沖刷下來
  20. With the failure of diamond coated cutting tools, built - up edge ( bue ) develops, and cutting force on the tool jumps immediately. so the failure is predictable by monitoring the devolop of bue and change of cutting force

    切削過程中刀具金剛石薄膜失效時,會產生瘤,且切削力驟然增大,通過監測產生和切削力變化,可以預報金剛石薄膜塗層刀具失效。
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