煤田區 的英文怎麼說

中文拼音 [méitián]
煤田區 英文
coal field area
  • : 名詞(黑色固體礦物) coal
  • : Ⅰ名詞1. (田地) field; farmland; cropland; land 2. (姓氏) a surname Ⅱ動詞[書面語] (打獵) hunt
  • : 區名詞(姓氏) a surname
  • 田區 : tract
  1. The qitaihe coal resources isadvantageous, the coal field total area 8, 000 square kilometers, haveverified the geological reserve 1. 7 billion tons, the prospectivereserves 4. 2 billion tons, the coal plant completely, has the cokingcoal, 1 / 3 coking coal, the gas coal, the anthracite and so on 10varieties, by coking coal primarily ; excellent in quality, has theespecially low phosphorus, especially low characteristic and so onsulfur, high heat value, high ash melting point, high silicon content, most is suitable for the coal chemical industry product thedevelopment, is national one of three big protections mining rare coalfields, is the heilongjiang province most important anthraciteproduction base, also is the national important coking coal and thenortheast area biggest high quality coke production base

    七臺河炭資源得天獨厚,總面積8000平方公里,已探明地質儲量17億噸,遠景儲量42億噸,種齊全,有主焦、 1 / 3焦、氣、無煙等10個品種,以主焦為主;品質優良,具有特低磷、特低硫、高發熱值、高灰熔點、高硅含量等特點,最適于化工產品的開發,是全國三大保護性開采稀有之一,是黑龍江省最重要的無煙生產基地,也是國家重要的主焦和東北地最大的優質焦炭生產基地。
  2. Under general geological study of exploratory development of coalbed gas and underground gasification of coal bed in eastern depression of liaohe basin, authors apply the basic principle of coal geology and the data of vitrinite reflectance and technical analysis of coal to ascertain that coal classification are dominantely the lignite, long - flame coal and gas coal of coal - bearing upper section of third member of shahejie formation, and then dissertate the variational regularity between coal rank and buried depth in vertical and otherness of vertical limit of coal rank in different coal - rich regions

    摘要運用地質學基本理論和的鏡質組反射率值及工業分析等有關數據,確定了遼河盆地東部凹陷古近系沙三段含亞段的種主要為褐、長焰和氣;進而闡述了該段垂向上級與埋深的變化規律性、不同賦級垂向界限的差異性。
  3. 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,泥炭坪是成的重要古地理環境,潮渠對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作用的主要因素。
  4. 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,泥炭坪是成的重要古地理環境,潮渠對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作用的主要因素。
  5. Application of coalfield slalom seismic prospecting data acquisition technique in loess tableland

    黃土塬彎線地震勘探採集技術的應用
  6. Analysis of sulfur in coal and coal facies in yinajia exploration area, zhina coalfield, guizhou

    貴州織納以那架勘探中硫與相分析
  7. Analysis of parameters of coal pillar in bulianta mine

    補連塔井柱參數分析
  8. Application of multisource remote sensing technique in rujigou coalfield fire area dynamic monitoring

    多源遙感技術在汝箕溝動態監測中的應用
  9. Application of seismic inversion based on model for igneous distributing in coalfields

    火成巖分佈地震反演技術的應用研究
  10. The higher - permeability region for cbm exploration are panzhuang - yangcheng, yangquan - shouyang and taiyuan xishan coalfield in qinshui basin

    預測結果顯示,沁水盆地有利於層氣開發的高滲,主要集中在南部的潘莊陽城、北部的陽泉壽陽及太原西山等地
  11. The system is utilized to store and manage the basic geographical information, coal field exploration materials, coalbed methane exploration materials and regional geological survey achievement of qinshui basin interactively

    運用該系統對沁水盆地的基本地理信息、勘探資料、層氣勘探資料及域地質調查成果進行了一體化存儲管理。
  12. In order to speed up the development of juye coal field and the coal chemical industry, shandong province people ' s government promotes the qing hill - longgu road for the provincial level road which pass through juye carbonificated garden ; with the opportunity of the xinxiang - shijiu railway electrification transformation , juye has planned area railroad private line to the garden ; the sewage treatment factory will go to the operation in 2007 year ' s end, zhushui river route, daye reservoir project are in the advancements

    為加快巨野的開發和化工產業的發展,山東省人民政府將貫穿巨野化園的青龍路升級改造為省級公路;藉助新石鐵路電氣化升級改造的機遇,規劃了通往園的鐵路專用線;污水處理廠2007年底投入試運營,洙水河航道、大野水庫等工程正積極推進。
  13. On the trouble frontiers of coal, however, they met fierce resistance and defeat that spelled eventual disaster.

    可是,在麻煩的邊界地,他們遇到兇猛的反抗,而且最後招致災難性的失敗。
  14. An analysis on structure and its coal - control action in longxian region, huanglong jurassic coalfield

    黃隴侏羅紀隴縣地構造及控作用分析
  15. A study on deposit water filling factors of yilan coalfield

    青海省魚卡尕秀西段礦供水與礦井充水水文地質條件分析
  16. Optimum design and constructin for the upper air - returning system at the sixth mining area, no. 1 well, yaojie coal field

    窯街一號井六采上部回風系統優化設計與施工
  17. Laws of collapse columns and prediction of non - mining areas ximing well field of xishan coal field

    西山西銘井陷落柱規律及未采預測
  18. With the rapidly development of minefield and the rapidly increase of coal output, the excavation scope and depth will extremely rise, the excavation work is under the overlying by the thin rock strata, and under the thick loose bed, the population in mine field will be more and more, the relevant basic industries will also develop rapidly. the mines will discharge more water from the underground, and the production and living will also consume more water. so the original water resource balance system in the minefield will be broken, the ecological environment formed by the nature will be destroyed in some degree

    隨著礦迅速發展而炭產量的快速增長,既定在薄基巖厚鬆散層下的神東開采范圍和深度勢必急劇增大,相應的人口也增加,與其相匹配的其它基礎工業一併迅猛發展,導致礦井外排水和生產生活用水直線猛增,這一系列生產和生活巨量用水必然會打破礦原始的水資源平衡體系,不同程度的破壞自然形成的脆弱的生態環境。
  19. Based on synthetic analysis of gravity, magnetic and seismic data as well as geological and drilling data of central southern cangxian uplift, together with a comparison with the proved dacheng coalfield, the authors hold that there exist a lot of coal seams and coal strata in this area

    摘要通過綜合分析滄縣隆起中南段上的重磁與地震資料,結合域地質與鉆探資料,並通過與已知的大城的比較,認為本大面積賦存系地層與層。
  20. Abstract : because the shenfu - dongsheng mine area is located in intermediate of arid and semiarid zone, its ecological environment is very fragile. based on the fragileeco - environmental, the coal mining and construction have brought out some new environmental problems. man - made debris flow problems is the most serious of them which caused by coal mining, construction of railway and highway as wellas exploiting stone. through a great deal of experiments of artificial simulation setting water rushing to two types of slope debris flow and debris flow gully in shenfu - dongsheng mine site, the characteristics is favourable to formation of debris flow ; ( 2 ) the waste gangue is easy to initiate and is main solid material of debris flow in this area ; ( 3 ) the whole debris flow process could be observed through the model simulation experiment of debris flow gully. at present, this experiment method is the best way to analyze debris flow genesis and process

    文摘:神府東勝礦位於黃土高原北部乾旱半乾旱過度地帶,由於的大量開采,誘發了大量的環境問題,尤以人為泥石流最為嚴重.本文以神府-東勝礦人為泥石流為研究對象,採用人工放水沖刷模擬實驗的方法,分析了坡面型和溝谷型泥石流源地鬆散體起動、產沙、泥石流過程的特性,所得結論為: ( 1 )放水歷時長、強度大,有利於泥石流的形成; ( 2 )棄土石渣易起動,是該泥石流固體物質的主體; ( 3 )溝道型泥石流放水沖刷模擬實驗,便於觀測泥石流的全過程,坡面型泥石流放水沖刷模擬實驗,利於統計產沙、觀測侵蝕形態
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