鹽臺 的英文怎麼說

中文拼音 [yántái]
鹽臺 英文
salt table
  • 鹽 : 名詞1. （食鹽; 鹽類） salt 2. （姓氏） a surname
  • 臺 : 臺名詞（指臺州） short for taizhou （in zhejiang province）
  1. Wangtsailiao and tingtoue sandbars reveal shocking evidence of the rapid degradation of taiwan s coasts. hsu hsien - ping, a guide at the salt country culture and history workshop, says that tingtoue sandbar used to be home for thousands of egrets and other birds, but noisy tourists frightened the egrets away, leaving only the signs explaining their natural history, erected next to the beefwood forest by the tainan county wild bird society, as a poignant reminder

    鹽鄉文史工作室導覽老師許獻平指出，以往頂頭額汕是成千上百的白鷺鷥等鳥類居住的樂園，由於來到頂頭額汕的遊客任意穿梭木麻黃林間，大聲喧嘩，使得白鷺鷥飽受驚嚇，最後只能遷移他處，剩下臺南縣野鳥協會過往于林邊豎立的白鷺鷥生態解說牌，令人不勝唏噓。
  2. In places on crationic edges, giant carbonate platforms may develop.

    在克拉通（穩定地塊）邊緣的某些地區，可發現巨大的碳酸鹽臺地。
  3. There are over 80 sets test apparatus in tech - innovation centre, including : anechoic chamber, vibration tester, vibration measurement analysis, impact instrument, constant temperature and humidity facilities. salt spary test case, circle insulation withstand voltage tester, insulation resistance tester, withstand voltage tester, electric lead tester, electrical leakage tester, earth resistance tester, chassis dynamometer, chassis dynamometer control system, high stability dc resistance tester, electrical capacity tester, temperature rise test system

    中心擁有各類分析測試儀器和試驗裝置80餘臺套，包括：消音室振動臺噪聲振動測試分析系統沖擊儀恆溫恆濕實驗儀鹽霧試驗箱匝間耐壓分析儀絕緣電阻分析儀對地耐壓分析儀泄露電流測試儀對地電阻測試儀測功機測功機控制系統高精度直流電阻測試儀電參數測試儀帶電溫升測試儀復合式三坐標測量儀萬分投影儀及電功測試分析系統等。
  4. Research on producing lithium sulfate by intercrystalline brines from jilaier lake of xitai to salt out

    西臺吉乃爾湖晶間鹵水兌鹵鹽析制取硫酸鋰的研究
  5. The towering salt mounds of the chiku salt pans are known as the " snowy mountains " of tainan. novel attractions at the salt pans include healthful brine baths and salty ice lollies

    七股鹽場的巍峨鹽山，有臺南長白山的美名鹽場尚有泡鹽鹵浴美容與品嘗咸冰棒，頗為新奇。
  6. 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。
  7. 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。
  8. 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。
  9. Was an old warehouse of taiwan salt company. it was fallen into disuse and the pagoda trees grown in there. over half century,

    為臺鹽舊倉庫，曾一度荒廢任由榕樹寄生，經過半世紀，形成特有的樹屋公生奇景
  10. After the restoration of taiwan, it was become the warehose of taiwan salt corp. it was fallen into disuse and the pagoda trees grown in there

    光復后改為臺鹽倉庫，曾一度荒廢任由榕樹寄生，經過半個世紀，形成特有的屋樹共生奇景。
  11. Reefs are well developed in western hubei and eastern chongqing. through sedulous research, the whole acquaintance on types of reef builders, types of reef carbonatite, development and evolution of reef organisms, division of reef facies, distributing regularities of reefs and diagenesis has been concluded. according to the comprehensive studies, the following results and conclusions have been obtained

    通過對鄂西渝東區上二疊統長興組生物礁造礁生物、沉積相、成巖作用的研究，認清了礁體的主要造礁生物類型、主要巖石類型、生長演化、相帶劃分、分佈規律以及成巖作用，可以得出以下結論和認識： 1生物礁主要分佈於晚二疊世碳酸鹽臺地內部和臺地邊緣，可分為三種類型。
  12. Based on the detailed research on the sedimentary rocks of northwest ordos basin in their textures, structures, vertical sequences and logging response, six kinds of sedimentary facies can be recognized in this work, i. e., alluvial fan, stream, fan delta, braided delta, delta, lake, barrier beach and carbonate platform, respectively, and more detailed classification of sedimentary subfacies and microfacies for each sedimentary facies are also made in the work

    本文通過對鄂爾多斯盆地西北部沉積巖沉積結構、沉積構造、垂向序列及測井響應的深入研究，識別出沖積扇、河流、扇三角洲、辮狀河三角洲、曲流河三角洲、湖泊、障壁海岸及碳酸鹽臺地等8種沉積相類型。在此基礎上，對每一種沉積相又進行了詳細的沉積亞相和微相的劃分。
  13. The palaeogeographic research indicate that the palaeogeographic outline of the study area recorded the evolution from a sedimentary basin in which the shallow - water carbonate platform sediments and deep - water terrigenous clastic submarine fan developed from southeast to northwest and northeast during the late triassic through a submarine sheet - like model composed of deep - water sandy turbidite and fine - grained turbidite during the early jurassic to a terrigenous clastic barrier coast during the middle and late jurassic and finally to the coal - bearing delta sediments during the late cretaceous

    古地理分析表明，研究區晚三疊世古地理輪廓是一個從東南向西北和東北方向由淺水碳酸鹽臺地及深水陸層海底扇沉積共同發育的沉積盆地；早中侏羅世，演變成為一個由深水砂質濁積巖和細屑濁積巖組成的水下席狀體沉積；進入中晚侏羅世，其古地理表現為一個陸屑淺海有障壁海岸；到了晚白堊世，研究區表現為以含煤沉積為特徵的三角洲相沉積。
  14. The reservoirs mainly exist in the oolitic bank facies in the carbonate platforms, which were deposited in high energy environment and mainly controlled by tidal action

    其沉積相屬碳酸鹽臺地的鮞粒灘相，為臺地潮下較高能環境沉積，主要受潮汐作用的控制。
  15. On the basis of lithofacies palaeogeographic map, the sedimentary and lithofacies palaeogeographic characteristics of the middle yangtze region during the late sinian and early cambrian are also described

    晚震旦世巖相古地理格局由碳酸鹽臺地（鄂中臺地）和南邊的臺緣盆地組成。
  16. The transitional facies can also be divided as estuarine, tidal flat and lagoon ; the depositional envirnononents of clastic rock marine facies include offshore, shallow water continental shelf, deep water continental shelf, slop as well as the deep water basin ; the carbonate facies can also be divided into a carbonate platform and ramp

    海陸過渡相又分為河口灣、潮坪、瀉湖；海相碎屑巖沉積環境包括濱海、淺水陸棚、深水陸棚、斜坡以及深水盆地；碳酸鹽巖海相又可分為碳酸鹽臺地、碳酸鹽緩坡。
  17. Based on the synthetic research of field outcrops, drilling section, well log and office compilation, combined with analyses of geological background, lithological association, sedimentary texture, sedimentary structure, geochemical and palaeobiological features, the researched area in the palaeozoic can be divided into deltas, braided deltas, lacus, barrier coast, continental shelf and carbonate platform etc. six kinds of sedimentary facies

    在野外露頭、鉆井剖面及測井曲線的綜合研究和室內編圖基礎上，綜合地質背景、巖性組合、沉積結構、沉積構造、地球化學及古生物學特徵，研究區古生界被劃分為三角洲、辮狀河三角洲、湖泊、障壁海岸、陸棚及碳酸鹽臺地等6種沉積相類型。
  18. Through the correlation of nww - see and sn, the thickness and limestone intervals of matuo formation gradually increase from west to east. this represent the center of sedimentation is possible located in east of the region. the matuo formation thickness gradually increase and then reduce from north to south

    通過北西西?南東爾向和南北向剖面對比，瑪托組地層橫向變化表現為由西往東，瑪托組地層厚度逐漸加大，灰巖夾層也增多，反映當時沉積中心在研究區東部，而由北往南，厚度先逐漸增大，后減小，灰巖夾層增多，由北往南的古地理格架為濱面?碳酸鹽臺地?斜坡環境。
  19. Main ore bodies of changba style lead - zinc - ( silver ) deposit lie in transitional position from carbonate plateform fades to basin argillic and fine clastic fades, while bijiashan style lead - zinc - ( silver ) deposit in the position from plateform margin shoal facies to basin argillic facies

    廠壩式礦床主礦體產在碳酸鹽臺地相向盆地相過渡處，盆地水體相對較深；畢家山式礦床賦存在生物灘相向盆地相的過渡部位。
  20. The land disappeared during the late canglangpu age and longwangmiao age ( early cambrian ) and the framework of palaeogeography consisted of tidal flat, open carbonate platform, platform - margin slopes and basin in the south

    早寒蟬寒武世中晚期巖相古地理格局由碳酸鹽潮坪、開闊臺地、臺緣斜坡和臺緣盆地組成，該地區主體進入碳酸鹽臺地演化階段。
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