泥坪 的英文怎麼說

中文拼音 [píng]
泥坪 英文
corcass
  • : 泥名詞1 (含水的半固體狀的土) mud; mire 2 (像泥的東西) any paste like matter; mashed vegetable...
  • : 名詞(平地) level ground
  1. The detritus stream in lanping jinding mine

    金頂礦山石流
  2. 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環境,認為太原組形成於潮汐作用為主的陸表海海岸,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。
  3. 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環境,認為太原組形成於潮汐作用為主的陸表海海岸,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。
  4. 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、硬石膏晶體、團塊及腸狀石膏層的晶灰巖、微晶白雲巖組成的小潮差蒸發潮層序。
  5. 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

    上部為中薄層狀富的含石膏質夾層的晶灰巖、微晶白雲巖組成的旋迴性清楚的似蒸發潮層序。
  6. 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

    它們與潮晶白雲巖和質白雲巖構成具對稱相序組構的環潮型碳酸鹽米級旋迴層序。
  7. However, for the less energetic, the carparks situated at tai au mun and tai hang tun barbecue areas are excellent starting points for more leisurely walks. one can spend the entire day at the tai hang tun barbecue area, where barbecue and picnic facilities are provided and there are some magnificent vistas out over the open sea. the grassy slopes are ideal playgrounds for children but visitors should beware of the very steep cliffs which run down sheer to the sea in some places

    北潭涌自然教育徑全長9公里,沿途可考察灘、紅樹林、林地及散石灘等生態;其終點為一所博物館,名為上?民俗文物館,原是一條建於19世紀末的客家村,現仍保存著房舍、曬、廚房、豬舍、牛欄和一幢六米高的更樓,並陳列了村民的傢具及農具,重現了上?昔日的鄉村風貌。
  8. My dad shouted me house down when our dog walked across the wet cement he had just laid

    我們的狗竄過我爸爸剛鋪好的未乾水時,我爸爸就大聲叫嚷了起來。
  9. " each location has its highlights such as the mai po inner deep bay ramsar site in tsim bei tsui ; reedbed and relic of salt pans in tai o ; mudflat wildlife in to kwa peng and kei ling ha ; mangroves in lai chi wo ; and egretry in luk keng. " tour guides are all experienced interpreters of the hong kong wetland park. they will brief visitors on wetland wildlife and a code when touring wetlands

    發言人說:各個濕地旅遊點均有其特色,例如尖鼻咀的米埔內后海灣拉姆薩爾濕地、大澳的蘆葦沼澤和鹽田遺跡、土瓜和企嶺下的多種灘生物、荔枝窩的紅樹、鹿頸的鷺鳥林等。
  10. Suddenly i slowed, stopped and stared at the lawn. muddy grass and small gray mounds of melting snow. and there, bravely waving in the wind, was one pink crocus

    我猛地放慢了速度,停下車注視著草。草上粘滿污,一個個灰色小雪堆正在溶化。就在這里,有一株粉紅色的番紅花卻在不屈地迎風搖曳著。
  11. T c tower, jointly financed by thun - in construction co., and chen - tai cement co., is located in the kao - hsiung harber area. this 384 meter - high building is the highest building in asia, and the fourth highest in the whole world

    T c大樓由東雲建設與建臺水斥資興建,建築面積達幾十萬,雄峙于高雄市港區,樓高八十五層384m ,為亞洲第一,全世界第四支摩天大樓。
  12. T & c tower, jointly financed by thun - in construction co., and chen - tai cement co., is located in the kao - hsiung harber area. this 384 meter - high building is the highest building in asia, and the fourth highest in the whole world

    T & c大樓由東雲建設與建臺水斥資興建,建築面積達幾十萬,雄峙于高雄市港區,樓高八十五層( 384m ) ,為亞洲第一,全世界第四支摩天大樓。
  13. 90 ' s it was found in shizishan, yimen, indicated that the type deposit is well explorative prospect in dongchuan - yinmen. by sum up the data of trace elements, isotopic elements, fluid inclusions and minerogenetic age et al.,

    稀礦山式銅礦以落雪礦區稀礦山礦段最為典型,主要分佈在因民落雪大喬地?稀礦山、濫山、磨子山,濫泥坪6 ? 4巷、白錫臘和拖布卡地區。
  14. Initial enquiries revealed that shortly before 3. 30 am, officers attached to the enforcement and control division of traffic new territories north set up road blocks on tai po road and intercepted suspected vehicles travelling towards shatin near chek nai ping

    初步調查顯示,清晨約三時三十分,隸屬新界北交通部執行及管制組的警員在大埔公路設置路障,在赤泥坪附近截查往沙田方向行駛的可疑車輛。
  15. Through the analysis of the stratigraphy and sedimentary facies of the research areas, the description model between the stratigraphic framework and deposite environment can be set up firstly by the transition from the " three horizons sandstone with two intercalated limestone horizons ' mn yanshiping area to shale and marl in amdo - zigetang co, and to oil shale in bilong co, then by the transition of the shallow water platform facies to the deep water continental shelf, slope, and to the deep water basin

    通過對研究區地層和沉積相分析,建立起一個從北向南由雁石地層類型「三砂夾兩灰」過渡為安多?茲格塘錯地層類型頁巖、灰巖,最後到比洛錯地層類型黑色油頁巖,由淺水臺地相過渡到深水陸棚、斜坡,最後到深水盆地相的地層格架與沉積環境解釋模式。
  16. Remove paint, sealing layer ( protection layer ), resin emulsion cement ( wear - resisting flooring ), protruding part, rain trace, trowel mark, rough surface, uneven joint etc

    去除油漆、密封層(保護層) 、膠脂水(耐磨地) 、高出部分、雨跡、鏝刀痕、粗糙表面、不平接縫等。
  17. Sedimentary environment in benxi stage from east to west were respectively shallow - sea muddied continental shelf, barrier island, lagoon and tidal flat. most area in taiyuan stage was distributed by shallow - sea continental shelf, but the northern and southeastern part were scattered by clastic tidal flat and carbonate tidal flat. sedimentary environment in shanxi stage, in the middle and late shihezi stage was deltas and lake

    馬5晚期研究區發育蒸發臺地相和局限臺地相;本溪期自東而西發育淺海質陸棚、障壁島、瀉湖及潮相;太原期大部分地區發育淺海陸棚沉積,北部和西南部則發育碎屑巖潮和碳酸鹽潮沉積;山西期和石盒子中晚期為三角洲和湖泊沉積環境;石盒子早期廣泛發育辮狀河三角洲和湖泊沉積。
  18. Li, c. x., fan, d. d., deng, b., korotaev, v., 2003. the characteristics of chinese coastal zone in response to sea level rise. proceeding of international symposium on climate change, 294

    范代讀、李從先、陳美發, 2001 。長江三角洲質潮層序完整度的定量分析。 21世紀海洋科技與資源開發學術研討會論文摘要集, 56 - 57 。
  19. Furthermore, sixteen sedimentary subfacies are identified. respectively, the sedimentary subfacies are delta plain, delta front, prodelta, braided delta plain, braided delta front, braided prodelta, coastal lake, saucer lake, tidal flat, barrier island, lagoon, carbonate continental shelf, muddy continental shelf, open platform, local platform and evaporate platform

    並進一步識別出16種沉積亞相,分別為:三角洲平原、三角洲前緣、前三角洲、辮狀河三角洲平原、辮狀河三角洲前緣、前辮狀河三角洲、濱湖、淺湖、潮、障壁島、瀉湖、碳酸鹽陸棚、質陸棚、開闊臺地、局限臺地和蒸發臺地。
  20. The lithofacies can be grouped into three types : structure upward deeping of tidal flat - shoreface dominated by tidal ; structure upward deeping of tidal flat - shoreface dominated by sandstone ; structure upward shallowing and then deeping of tidal flat - shoreface

    瑪托組垂向巖性序列可以分為三種類型,即以巖為主的向上變深的潮?濱面結構、向上變深的濱面結構和向上變淺后變深的潮?濱面結構。
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