deposit area 中文意思是什麼

deposit area 解釋
棄土區
  • deposit : vt 1 放置,安置。2 使淤積,使沉澱。3 儲蓄。4 付保證金。5 寄存,委託保管。6 (把硬幣)放入(自動售...
  • area : n. 1. 面積;平地;地面。2. 空地;〈英國〉地下室前的空地。3. 地區,地方;〈比喻〉區域;范圍。
  1. The pathology characteristic that liver fiber changes is collect there are many fibre hyperplasia and deposit inside abbacy and liver flocculus, but have not form the interval inside flocculus, liver cirrhosis has false flocculus to form, central vein area and collect abbacy occurrence interval, the normal structure of liver is destroyed, liver fiber changes further progress to be liver cirrhosis namely

    肝纖維化的病理特點為匯管區和肝小葉內有大量纖維組織增生和沉積,但尚未形成小葉內間隔,肝硬化則有假小葉形成,中心靜脈區和匯管區出現間隔,肝的正常結構遭到破壞,肝纖維化進一步發展即為肝硬化。
  2. Under the guidance of theories of sedimentology, petroleum geology and sequence stratigraphy, and through the comprehensive analysis of outcropsrock, cores, well logs and testing outcomes of rock gas, this paper studies the depositional systems of neopaleozoic and the character of aeration zone in tabamiao area of ordos basin. the result indicates that the object layers are divided into two depositional systems, the barrier seacoast depositional systems are recognized on upper carboniferous taiyuan phase with tidal flat, lagoon and barrier bar sedimentary deposit

    本文根據沉積學、石油地質學和層序地層學理論,綜合利用地表露頭、鉆井巖芯、測井曲線資料和試氣成果資料,對鄂爾多斯盆地塔巴廟區塊晚古生代沉積體系及含氣層特徵進行了研究。結果表明,研究區內目的層段可以劃分為2個沉積體系: ( 1 )上石炭統太原期為有障壁海岸沉積體系,發育潮坪?瀉湖?障壁砂壩沉積。
  3. Based on the observation and statistics on the calcareous sandstone in the ore host layer in shihongtan uranium deposit, this paper finds that the calcareous sandstone occurs on and off near the top or wash surface of the sandbody as beads - strings lens along the layer and concentres in the area where the orebodies are rich

    摘要通過對十紅灘鈾礦床容礦層鈣質砂巖的觀察和統計,發現鈣質砂巖呈順層、斷續的串珠狀透鏡體分佈,產出空間位置為砂體的頂底部或沖刷面,而且較集中的分佈在礦體發育區。
  4. ( 7 ) rainfalls can " deposit " the co2 in air, making it to take part in the process of karst, to dissolve and corrade carbonate rock. co2 concentration in soil become lower after heavy rainfall and become higher after general rainfall. ( 8 ) the value of chemical characteristic of soil water in the high elevation area is lower than that in the low elevation area

    ( 7 )降雨可以對coz產生影響, 「沉澱」大氣中的co : ,使其參與到巖溶作用中,溶蝕碳酸鹽巖;降雨對土壤空氣中coz的影響與雨強、雨量有關,降雨量、雨強較大時,土壤空氣中的c02產生受到抑制,降雨量和雨強較小時,土壤空氣中的coz濃度升高。
  5. The minerogenetic model of xikuangshan type copper deposit can be concluded that : in jinningian - chengjiangian, the activity of xiaojiang discordogenic fault form dextrorotation sub - structure in dongchuan ore area

    昆陽裂谷內的多數銅礦同位素成礦年齡多集中在9 . 0億6 . 5億年之間,屬于晉寧-澄江期,與rodina大陸裂解時限相當。
  6. The lithologies of intrusive rocks were re - determined, for example, the rock previously named as diorite in southern area was renamed as gabbro, and the dike rock distributed along nnw as spessartite which was related to formation of the zhulazaga gold deposit to some extent

    對礦區各類侵入巖重新釐定了它們的巖性特徵,如礦區東南部原閃長巖重新確定為輝長巖,確定nnw向分佈的脈巖為閃斜煌斑巖,且認為後者和朱拉扎嗄金礦的形成有一定的關系。
  7. Assemblage ) represented the coastal shallow - water environment ; factor 2 ( protelphidium tuberculatum assemblage ) represented the alongshore cold - water current area or cold shallow sea environment ; factor 3 ( elphidium magellanicum assemblage ) represented the sh allow sea ( < 20 - 30m depth ) deposit ; factor 4 ( ammonia ketienziensis assemblage ) represented the shallow - sea water more than 50m depth ; and factor 5 ( buccella frigida assemblage ) represented the colder - water sea environment ; and the distribution of factor load accorded with the character of benthic foraminifer community

    Q型因子分析揭示ey02 - 2孔5種有孔蟲組合,分別對應濱岸鹽沼環境、黃海沿岸流冷水分佈區、高潮坪淺海沉積環境、水深大於50m的現代淺海環境及較冷的沉積環境。因子載荷的分佈與有孔蟲群落特徵吻合較好。南黃海有孔蟲含量? ?水深轉換函數關系式有一定的局限性,並不能在南黃海陸架地區推廣使用。
  8. The studied deposit area is located on a monocline geotectonic unit divided by several groups of faults. therefore, the secondary widen transverse and lognitudinal drapes may have great influence on ore forming and location

    礦區基本構造為一個被幾組斷裂破壞的單斜構造,其上發育的次一級的開闊型橫向和縱向褶皺對礦床的形成和空間定位起著十分重要的作用。
  9. Jadeite deposit geology in pharkant area, north myanmar

    緬甸北部帕敢地區翡翠礦床地質
  10. Liihe palynological data indicate a vertical paleovegetational landscape : evergreen broad - leaved forest dominated by castanopsis, lithocarpus, cycobalanopsis and anacardiaceae etc occurred on the slopes near the deposit site ; mixed coniferous / broad - leaved forest and coniferous forest occurred on the area of high elevation, and main elements were tsuga, podocarpus, pinus, picea and abies etc. seven paleoclimatic parameters of liihe area estimated include mat ( 13. 3 - 20. 9c ), wmt ( 22. 5 - 27. 5c ), cmt ( 2. 5 - 12. 6c ), dt ( 12. 1 - 24. 8c ), map ( 803. 6 - 1254. 7mm ), mmap ( 179. 4 - 281. 9mm ) and mmip ( 10. 2 - l8. 5mm ). yangyi palynoflora comprises of 52 palynomorphs belonging to 32 families. the percentage of angiosperms is 61. 5 %, gymnosperms 9. 6 %, pteridophytes 25. 0 %, algae 3. 9 %

    呂合孢粉植物群的組成反映該地區在沉積時期植被具有垂直分帶特徵,沉積地附近分佈有常綠闊葉林,包括殼斗科的青岡屬、栲屬、石櫟屬和漆樹科等植物,以及多種亞熱帶和溫帶闊葉成分;林中混生少量針葉樹(如松屬和杉科等) ;林內蕨類植物較少;距沉積地較遠的海拔較高的地區分佈由鐵杉屬、冷杉屬、雪松屬和雲杉屬組成的針闊混交林或針葉林。
  11. On the basis of the types of sand stone, light and heavy mineral associations, planimetric map of sedimentary facies and directions of palaeoflow, it is considered that detrital material of terrigenous deposit of chang6 - 8 oil - beds in this area come from southwest provenance, northeast provenance, west provenance and south provenance, respectively, which are the denudation area of huating - longxian county in southwestern, yinshan ancient land in the northern, the denudation area of yantong mountain and tongxin to the west of yangjiajuzi - yinjiacheng county and qinling ancient land in the southern

    根據砂巖類型、輕、重礦物組合、沉積相帶平面展布及古水流方向等特徵的分析,認為研究區延長組長6 ? 8油層組陸源碎屑物質來自西南、東北、西部和南部四大物源區,分別為西南華亭?隴縣一帶剝蝕區,北部陰山古陸,西部的楊家咀子、殷家城以西的煙筒山、同心地區剝蝕區和南部秦嶺古陸。
  12. We can apply these digital tenor models to solve problems confronted during deposit exploration. those models can help study shape, scale and distribution of different ore bodies in the deposit area, reveal the relationship between tectonics of the deposit area and copper deposit realization, they can also offer some information for deposit exploration and laneway digging

    應用數字品位模型( dtm )可以形象直觀地反映礦區銅元素分佈規律及不同礦體的產狀、規模;展示礦區構造與銅元素礦化的關系;可以為礦山開采和巷道開拓提供重要的參考資料;還可以由已知推未知,為礦區外圍找礦提供輔助性信息。
  13. The neogene is a key stage of terrestrial environmental evolution in yunnan. three stratigraphic sections including luhe ( late miocene ), yangyi and longling ( late pliocene ) were selected to reconstruct vertical landscape of paleovegetation in these areas, based on palynological data. according to principle of the coexistence approach, seven quantitative paleoclimatic parameters of each deposit area were obtained by using meteorological data ( 1951 - 1980 ) of the distribution area of extant taxa found each palynoflora in china

    晚第三紀是雲南地區環境演變過程中的關鍵地質歷史時段,本論文以晚第三紀晚中新世(呂合) 、晚上新世(羊邑和龍陵)地層中的孢粉為研究對象,結合同層位大化石植物證據,參照現代植被,恢復了雲南三個化石出產地區的古植被垂直分佈景觀,並定性地描述了古氣候;同時運用共存分析方法( theco - existenceapproach )定量化地重建了三個地區的古氣候參數值;初步推測了沉積地可能的古海拔。
  14. The distributing patterns of the eulerian residual currents of the four major tide constituents ( i. e. m2, s2, ol and kl ) imply that fine - grained sediment transport over the central mud of the northern yellow sea is weak. the eulerian residual currents of kl and s2 respectively form an anti - clockwise eddy near the coastal mud - deposit area of northern shandong peninsula, which may increase the deposition rate of mud

    各分潮歐拉余流總的分佈趨勢表明北黃海中部泥區細顆粒沉積物輸運的量值很小, k1和s2分潮歐拉余流各自在山東半島北側近岸泥質區形成的順時針渦漩可能促進了該處的泥質沉積。
  15. Effect of geochemical prospecting method in the shabaosi gold deposit area, heilongjiang

    用化探方法在黑龍江砂寶斯金礦區找礦的效果
  16. Application of static pressure grouting and shotcrete piles in control of surface subsidence in karstal deposit area

    高壓噴射注漿在人工挖孔樁護壁工程中的應用
  17. Discussion of ore control condition in nuluerhu gold deposit area, inner mongolia to liaoning

    遼寧努魯爾虎金礦帶控礦條件分析
  18. Ne - nee orientation faults are the most important ore - controlling tectonic, as is especially the case for fl fault, which traversing the whole deposit area. 3

    Ne ? nee組斷裂是礦區最主要的控礦構造,特別是f1斷裂,橫貫整個礦區,是最大的控礦構造; 3
  19. After considering practical conditions of deposit, we applied gamma spectrometry ( gs ) methods to the whole deposit area and shallow seismic exploration ( sse ) methods to the west of no. 63 prospecting line of vii ore - body

    在此基礎上,結合礦山實際情況,在整個礦區進行了伽瑪能譜的測量,並著重在號礦體63勘探線以西開展淺層地震勘探的應用研究。
  20. As results of mix of deep mantle - source materials and shallow metallogenic materials, and tectonic movement of south unit and north unit, dongxiang copper deposit become a multi - metal deposit especially enriching cu, together with fe, w, s, ag, au, bi, cs and te etc. 2. ore - forming of copper deposit has much to do with the geotectonic of deposit area

    深部的幔源物質與淺部的成礦物質混合,南北兩大構造單元各自的成礦特徵又在此集中體現,使東鄉銅礦成為一個以銅為主,伴生鐵、鎢、硫、銀、金、鉍、銫、碲等元素的多金屬礦床; 2
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