造山運動期 的英文怎麼說

中文拼音 [zàoshānyùndòngqī]
造山運動期 英文
orogenlic phase
  • 造 : Ⅰ動詞1 （做; 製作） make; build; create; produce 2 （假編） cook up; fabricate; concoct 3 [書面語...
  • 山 : 名詞1 （地面形成的高聳的部分） hill; mountain 2 （形狀像山的東西） anything resembling a mountain...
  • 運 : Ⅰ動詞1 （物體位置不斷變化） move; revolve 2 （搬運; 運輸） carry; transport 3 （運用） use; wield...
  • 期 : 期名詞[書面語]1. （一周年） a full year; anniversary 2. （一整月） a full month
  • 運動 : 運動[舊時用語] arrange things or get things done through pull
  1. The petrophysical properties of volcanic rock reservoirs in junggar basin are generally characterized by the following : the acidic lava and auto brecciated lava are the best, especially the petrophysical properties of auto brecciated lava and andesites after the tectonic movement and denudation process in the later stages are superior to those of basalts

    準噶爾盆地火山巖儲層物性一般特點是：酸性熔巖、火山角礫巖最好，特別是經後期構造運動和溶蝕作用改造后的火山角礫巖；安山巖的物性總體優于玄武巖。
  2. K - ar age of an illite from alteration rock in the contact zone around lianhuashan porphyry is 38. 6ma. with referencing to the main metallogenic period of yulong copper metallogenic zone and of ailaoshan gold metallogenic zone, it is suggested that the time of formation of deposits in the district studied is probably in a period of time from 38. 6ma at earliest to 20ma at latest. this time is equivalent to the origination time of two important tectonic events, i. e., lanping movement and the turning point when ailaoshan - red river fault turned from sinisteral into dextral

    獲得了蓮花山巖體周圍接觸帶蝕變巖中伊利石k - ar年齡38 . 6ma ，參考玉龍銅礦帶和哀牢山金礦帶的主要成礦期（分別為30ma左右及26ma ） ，釐定本礦集區成礦年齡下限為38 . 6ma ，上限為20ma ，與兩次重要的構造事件?蘭坪運動的起始時間及哀牢山?紅河斷裂由左旋轉為右旋的時間相當。
  3. The period was one of general emergence and orogeny.

    這個時期是全面的上升和造山運動。
  4. Based on the geological, hydrogeological and hydrochemical information, the genesis of the underground hot water in qi county of shanxi has been analyzed. it is concluded that the formation of underground hot water is related to the magmatic activity in yanshan period, the goup of the base fault block forming in new tectonic period, the large depth and fast variety to underground water cycle

    從地質、水文地質、水化學等方面，分析了祁縣地區地下熱水成因，得出該地區地下熱水形成與燕山期巖漿活動、新構造運動形成的基底斷塊隆起及地下水循環深度大、交替迅速有關。
  5. Alpine age orogeny

    阿爾卑斯期造山運動
  6. The study results on hydrocarbon preserving conditions have suggest ed that influenced by latter tectonic movements, especially by the yanshan ~ himalayan tectonic movement, obviously different hydrocarbon preserving conditions occur between the eastern and the western parts bounded by the qiyue mountain. the whole lower paleozoic hydrocarbon enclosing and preserving conditions for the shizhu synclinorium - fangdoushan antici inorium to the west of qiyueshan mountain have the advantage over those of the qiyueshan antici inorium - lichuan synclinorium to the east of qiyue mountain

    通過油氣保存條件的研究認為：受後期構造運動的影響，尤其是燕山期?喜山期構造運動的影響，造成區內以齊岳山為界東西油氣保存條件存在明顯差異，齊岳山以西的石柱復向斜?方斗山復背斜下古生界油氣整體封存條件明顯優于齊岳山以東的齊岳山復背斜?利川復向斜。
  7. Tncyclic diterpanes c20, c21 and c23 distribution also has relationship with oil gravity, oil and gas production, as well as oil pool formation timing and oil source. rising - patterned oil originates from fengcheng formation, while peak - patterned oil from xiawuerhe formation. four types of migration and accumulation models are put forward : ( l ) fault controlled migration and accumulation along ridge far from source region ; ( 2 ) fault and unconformity controlled migration and accumulation around source region ; ( 3 ) fault controlled migration and accumulation in the slopes within source region ; ( 4 ) biogenetic and low temperature catalyzed gas migration and accumulation in middle and shallow formation

    受擠壓背景控制，研究區內海西期形成的斷裂，全部為逆斷裂，活動期長，可以延續到印支期和燕山期，斷開層位可以從石炭繫上延至誅羅系，它們對區域構造、沉積、油氣運聚有顯著的控製作用；而燕山期形成的斷裂多為小型正斷裂，部分為株羅系和白要系內部斷裂，部分從徐羅系斷至白聖系。
  8. Because there are several periods of tectonic movement and several tectonic zones " development and complex superposition at da gangshan hydropower staion, geological structure in dam area is great complex and water - bearing media has the characteristic if inhomogeneity, which make it difficult to further clarify the burial condition of different bearing aqueous structure and the development of ground water system at the dam area

    由於大崗山水電站壩區存在多期次的構造運動以及多個構造帶的共同發育、復合疊加，使得壩區地質構造顯得錯綜復雜以及含水介質的不均一性，使得進一步闡明壩區不同承壓儲水構造埋藏條件和壩區地下水系的發育特點變得很困難。
  9. According to these results combined with exploration practice, foot favorable exploration zones are selected, these are the integrated anticline traps below the tertiary gypsum halite, gypsum mudstone in kuqa foreland thrust belts, the second and the third row structural bells in southern junggar foreland thrust belt, the unconventional natural gas pools in die yanshan palaeohigh in north and south of western sichuan basin, the gentle fold structural belt in central sichuan basin and the deep depression in sichuan basin, and the cold take and nanbaxian structural belt in northern margin of qaidam basin

    依據理論分析及勘探實踐，優選出4個有利的勘探區帶，它們是：庫車前陸沖斷帶古近系、新近系膏鹽巖、膏泥巖之下的完整背斜圈閉；準南前陸沖斷帶第二、第三排構造帶；川西北部及南部燕山運動期古隆起、川中平緩褶皺構造帶以及深坳陷內部的非常規天然氣；柴北緣冷湖南八仙構造帶。
  10. There existed several strong reformation of late - yanshan movement and himalaya movement the generation, development, disappearance and reformation are tightly related to tarim block, tianshan belt and tethyan tectonic zone, especially tianshan belt, which makes the great difference between present and original basin

    該盆地形成后經歷了燕山晚期和喜山期構造運動的多期強烈改造；其產生、發展和消亡以及改造與塔里木地塊、天山構造帶、特提斯構造域的演化息息相關。其中尤以天山構造帶的活動影響最大，從而造就盆地今古面貌差異巨大。
  11. According to the analysis of the structure deformation variant direction the structure superposition during late period, and the tectonic stress field and deformation variant field, the cover extended nearly sn direction in early stage ( d - c ), maybe changed the direction in pernian ( especial the late permian ), and developed some new half - graben along sn direction except the succession activity at great fault zone. the direction of compression deformation variant, however, was nearly sn direction in indo - chinese epoch, ne - sw direction in early yanshan movement epoch, nne - ssw direction in late yanshan movement epoch, and transformed from ew to sn direction in himalayan movement epoch

    根據不同構造層中變形方向及後期構造疊加的分析，對本區的構造應力場及變形場進行了探討，本區蓋層早期階段（ d - c ）為近南北向的伸展拉張，二疊紀（特別是晚二疊世）的伸展方向可能發生了改變，除在各斷裂帶繼承性活動外，沿南北方向又新生了一些半地塹。而在擠壓變形時，印支期主要為近南北向擠壓，燕山早期為nw - se向擠壓，燕山晚期為nne - ssw向擠壓，而喜山運動可能經歷了從ew向向sn向方向擠壓的轉變。
  12. Detailed studies of tectonic unit and mineralized pedigree in each tectonic unit and each period provided that tectonic evolution passed an evolutionary sequence from early extension - transition - late compression that correspond to mineralization - sediment and submarine eruption - exhalation mineralization - moderate to acid magma and tectonic hydrothermalism that are relevant to mantle - derived magma and volcanic activities ; the mineralized pedigree can be indicated as mantle derived - inner basin and deep source - crust source ore - forming materials

    對各時期、各構造單元的成礦譜系進行了詳細研究，提出構造運動演化從早期拉張過渡晚期擠壓的演化序列，分別對應于以幔源巖漿和火山活動有關的成礦作用沉積及海底噴流?噴氣成礦作用中酸性巖漿及構造熱液成礦作用；在成礦物質上由幔源盆內及深源殼源的成礦譜系。
  13. Alkali basite, which came from upper mantle or lower crust, invaded through those structure, which not only bring cu et al mineralizing elements, but also the most important is that thermal energy. it cycled the formation water ( yinmin fonnation and luoxue formation ), and form alkali - rich, middle - high temperature and salinity fluid mixed with alkali - rich magmatic water. there were high rate of percolation and well voidage in the contact zone between yinmin purple stratum and yinmin rubblerocks, which is in favor of the transposition and mineralization of minerogenetic fluids

    因此，總結東川稀礦山式銅礦成礦模式為沉積（ fe 、 cu ） ?熱液疊加（ cu ）改造：晉寧-澄江期，小江深大斷裂發生走滑運動，在東川礦區造成右行旋扭及其派生構造，形成「 z 」字形落因破碎帶，同時來自深源（下地殼或上地幔）堿基性巖漿侵入，不僅帶來了大量cu等成礦物質，更重要的是提供了熱源，促使地層水（落雪組白雲巖和因民組紫色層）循環，與富堿（ na和k ）巖漿水混合，形成富堿中高溫高鹽度流體。
  14. The qiongzhong granite should have been formed at orogenic relaxing stage after the peak of indosinian orogeny, and the danxian granite were formed at the latest orogenic phase

    瓊中巖基可能形成於「印支期」碰撞造山運動峰期后的鬆弛階段，而儋縣巖基則可能形成於造山運動的結束階段。
  15. The lingnan school has played an important role in the development of modern chinese painting. the artistic origins of the school can be traced back to the jiansu painters song guangbao and meng jinyi, who lived in guangdong during the middle of the qing dynasty, and their students ju chao and ju lian, also from guangdong, in the late qing

    嶺南畫派的淵源可追溯至清代中期寓居廣東的江蘇畫家宋光寶及孟覲乙以及隔山派的居巢居廉中心人物高劍父高奇峰及陳樹人力倡新國畫運動，他們引西潤中的理論和實踐，當時造成了巨大的回響。
  16. From the viewpoint of method, the first step is to determine the available investment options or opportunity set of the locations of crude oil tankers zone involving some six representative factors such as the unit engineering expense, unit operating cost, constructing period, the location land features, unit constructing engineering amount, unit land opportunity cost. these factors stem from the economic, societal and environmental regulations and rules. the second step is to specify how to choose among these available options

    從方法上來看，首先確定以單位工程造價、單位運行成本、建設期、地形特徵、單位土建工程量、單位土地機會成本等六個綜合經濟、社會及環境指標為代表的原油罐區方案決策目標集，其次制定桃園、西山、填海三個決策待選方案，然後建立基於優先關系的相對優屬度矩陣及各影響因素的權重集，從而進行模糊動態規劃評價，最後優選出最佳的桃園方案。
  17. The area has experienced complicated and various structural movements since the indosinian stage, of which the most important thing is the massive yanshanian structural - magmatic event

    自印支運動以來，板內構造演化復雜而多樣。最引人注目的無疑是燕山期廣泛而強烈的構造-巖漿熱事件。
  18. Under the effect of regional tectonics, there develop many raws drape anticline and active fault in the front of mountain, and they have especial motion fashion

    由於受區域構造長期作用的影響，在北天山山前地區逐步發育形成了多排褶皺背斜及活動斷裂，且運動方式具有獨特性。
  19. The relief of high mountain area surrounded by deep valleys and recently active neotectonic movement resulted in various geological hazards in the westnorth of hubei province area

    鄂西北地區山高谷深，加上近期新構造運動活躍，導致地質災害頻繁。
  20. The basin was undergone multi - period of tectonic movement such as hercyniann indo - chinav yanshanian and himalayan. sangtanghu basin is a superimpose basin which deposited terrestrial sediments of mesozoic cenozoic and has a complicated structural evolutionary history

    盆地經歷海西、印支、燕山、喜山多期次構造運動，是一個以中新生代為主體的經歷了復雜演化歷史的疊合性盆地。
分享友人
分享到 Line

分享到臉書