育空地帶 的英文怎麼說

中文拼音 [yùkōngdedài]
育空地帶 英文
yukon
  • 育 : 育動詞1. （生育） give birth to 2. （養活; 培育） rear; raise; bring up 3. （教育） educate
  • 空 : 空Ⅰ形容詞（不包含什麼; 裏面沒有東西或沒有內容; 不切實際的） empty; hollow; void Ⅱ名詞1 （天空） s...
  1. We are likely to begin with subject and setoff, figure and sensation of movement, apace and entity, style of photography works these aspects to display application in falseness and truth, concealment and revelation this opposite and untied relation, thus making the pictures feel sense of movement, spatial sense and promulgating the relevant subject more profoundly

    在體育攝影中，我們可以從主體與陪襯、線條與動感、空間與實體，攝影作品風格等幾個方面來加以虛實藏露這一對立統一關系的運用，從而使畫面帶有動感，空間感，更加深刻地揭示主趣。
  2. The investigation and study showed that caused by the influencing factors of unit of tectonics, structures of floor rock stratum, conditions of landform, seismic intensities, fault, thickness of malan loess, the distribution of seismic loess landslides is very asymmetrical, which mainly show shapes of patch, belt, line, and there are different development characteristics in different regions

    現場調查顯示，受大地構造單元、基底巖層結構、地形地貌條件、地震烈度、斷裂構造和馬蘭黃土臨空厚度等因素影響，地震黃土滑坡的展布形態較為復雜，在空間上分佈很不均勻，常表現為片狀、帶狀和線狀展布，並在不同區域有不同的發育特點。
  3. Abstract : yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure

    文摘:陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲油田，儲集層主要為三角洲砂體，壓實作用和膠結作用強烈，儲層非均質性非常嚴重，因此預測次生孔隙發育帶是尋找油氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析，認為陜甘寧盆地延長統次生孔隙的形成除了受沉積有利相帶控制外，還與地層異常壓力的作用密切相關.研究認為隴東地區異常壓力的形成機理主要由於成巖過程中粘土礦物脫水作用.粘土礦物大量脫水時間正好與有機質脫羧期相一致，從而在異常壓力作用下將生油巖中的大量有機酸及co2帶到與之相鄰的儲集層中，並沿著有利儲集相帶運移，在酸性水經過的地方形成大量的次生孔隙，為後期油氣運聚提供有利通道及宿住空間，從現今的勘探結果來看，通過研究地層異常壓力縱橫向分佈特徵，並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法
  4. Yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure

    陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲油田，儲集層主要為三角洲砂體，壓實作用和膠結作用強烈，儲層非均質性非常嚴重，因此預測次生孔隙發育帶是尋找油氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析，認為陜甘寧盆地延長統次生孔隙的形成除了受沉積有利相帶控制外，還與地層異常壓力的作用密切相關.研究認為隴東地區異常壓力的形成機理主要由於成巖過程中粘土礦物脫水作用.粘土礦物大量脫水時間正好與有機質脫羧期相一致，從而在異常壓力作用下將生油巖中的大量有機酸及co2帶到與之相鄰的儲集層中，並沿著有利儲集相帶運移，在酸性水經過的地方形成大量的次生孔隙，為後期油氣運聚提供有利通道及宿住空間，從現今的勘探結果來看，通過研究地層異常壓力縱橫向分佈特徵，並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法
  5. Passed to on - site environmentally inspection on different communities, checked the related datum and drew lessons from the related research results of the recreational space system of abroad, this thesis joined together the realistic condition of our country, and it proposes the systematic conceptualization on community outdoor recreational space, whose main forms including different recreational spaces in different side residential area, also that between houses and so on

    通過對不同社區環境的實地調查，查閱相關歷史文獻，借鑒國外休閑空間體系的相關研究成果，文章結合我國國情的現實狀況，首次提出了社區級室外體育休閑空間體系化的構想。即以居民住宅和社區公共場所間的步道系統為紐帶，將居住區體育休閑場所、居住小區體育休閑場所、居住組團體育休閑場所有機地聯繫於一體。
  6. Xikuangshan type copper ore deposit named those fe - cu deposits hosted in yinmin formation, kunyang group, which located in kunyang rift valley and the edge of southwest yangzi platform. the best example is xikuangshan allotment, luoxue ore area, dongchuan, yunnan. the type deposit spread in south kunyang rift valley, include dongchuan, wuding - luoci, yuanjiang, yimen, huashengping, hongmenchang and so on

    稀礦山式銅礦是指賦存在昆陽群因民組地層中的銅鐵礦床，其大地構造背景屬于元古代裂谷帶，大陸裂谷是超大型銅等多金屬礦形成和分佈的有利環境，在裂谷下部常發育異常地幔和巖漿源，裂谷空間上的多層次性使礦床具有明顯垂向分帶特徵，其演化時間的長期性、脈動性和繼承性便於多期成礦作用相互疊加、礦質的高度聚集。
  7. To meet population and economic growth, it should be further modified to include more development areas, particularly those already with approved projects and those under active negotiations for past years, adequate space for the expansion of the hkust, the hi - tech research and development incubator zone together with its associated high class residential area, etc

    為了應付人口和經濟增長，這個方案應再作修訂，以包括更多發展地區，特別是已有項目獲得批準，或多年來一直積極進行磋商的地區、足以供科大擴展的空間、高科技研究及發展培育地帶，以及其相關的高級住宅區等。
  8. In this paper, relation between the dynamic evolution feature of gravity field and strong seismicity is studied, the result shows that, regional gravity field variation enjoys inhomogeneity of spatialand temporal distribution and gravity change in different regions

    摘要通過研究南北地震帶及青藏塊體東部地區多年來的重力場動態演化特徵及其與強震活動的關系，發現區域重力場變化既具有時空分佈的不均勻性和重力變化分區現象，同時又具有與活動斷裂構造密切相關並與地震孕育發展有著內在聯系的特徵。
  9. In each tour, an education ambassador takes you to a variety of facilities normally off - limits to the public. animal ed - venture includes visits to dolphin university, a unique chance to prepare meals for the giant pandas, and a rare chance to peek at what our trainers do behind - the - scenes. marine land ed - venture includes visits to atoll reef where youll see the fish being fed and the shark aquarium

    不妨為孩子報名參加幕後之旅的海陸空探索游或海洋天地探索游，由教育大使帶領參觀園內各種幕後設施，包括海洋館的大型水族館海豚學堂的獸醫院等，除了有機會探索雀鳥生活奧秘學習辨識魚類品種外，甚至可親手替熊貓準備食物，從中體驗自然世界真實有趣的一面。
  10. The key laboratory of orogenic zone and crustal evolution, ministry of education, school of earth and space sciences, peking university, beijing, 100871

    教育部造山帶與地殼演化重點實驗室，北京大學地球與空間科學學院，北京， 100871
  11. The study covers regional stratigraphy, regional geological structures and their evolution ; deep - large fracture system and building - moutain straps in the basin ; distributing of mineralization concentration area and mineralazition characteristics of different metal fields ; volcanic magmatic activity and magmatic distributing ; the petrology, element geochemistry features of the magmatic rock series ; the relationship between magmatic distributing and mineralization ; the relationship between magmatic forming - age and mineralization ; the relationship between magmatic form and mineralization ; source of mineral materials, source of hydrothermal solution and source of mineralizing agent ; transport forms of metal in the solution ; the ore - forming geochemical mechanism, etc. it turns out as follows : ( 1 ) lanping basin formed in the linkup of the plates and it was propitious to form deep - large fracture

    研究內容包括：區域地層及區域構造演化；盆地深大斷裂系統及造山帶；區域地球物理場；礦集區礦床的時空分佈、礦化特徵；巖漿巖活動與巖漿巖分佈；巖漿巖巖石學特徵；巖漿巖元素地球化學特徵；巖漿巖分佈與成礦的關系；巖漿巖成巖時代與成礦的關系；巖漿巖組成與成礦的關系；成礦物質的來源，成礦流體的來源；成礦物質搬運、富集的地球化學機理等。研究結果表明：蘭坪盆地發育于板塊的拼接地帶，有利於發育深大斷裂系統。
  12. Key laboratory of orogenic belts and crustal evolution, ministry of education, peking university ; school of earth and space science, peking university, beijing, 100871

    北京大學造山帶與地殼演化教育部重點實驗室北京大學地球與空間科學學院，北京， 100871
  13. As to the spatial distribution, the most typically developed danxia and karst areas are in tropic and sub - tropic humid regions in south china, but danxia scenery especially in southeast china, while karst scenery especially in southwest china

    在空間分佈上，兩者發育最典型的地區均在我國南方亞熱帶、熱帶濕潤區；其中，東南地區尤以丹霞景觀見長，西南地區更以巖溶景觀取勝。
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