晚發活動 的英文怎麼說

中文拼音 [wǎnhuódòng]
晚發活動 英文
late activity
  • : 名詞1 (晚上) evening; night 2 (姓氏) a surname Ⅱ形容詞1 (時間靠後的; 遲) far on in time; la...
  • : 名詞(頭發) hair
  • : Ⅰ動詞1 (生存; 有生命) live 2 [書面語](救活) save (the life of a person):活人無算 (of a goo...
  • 活動 : 1 (運動) move about; exercise 2 (動搖) shaky; unsteady 3 (不固定) movable; mobile; flexible...
  1. The fault controlled the magmatism and metallization relevant to the contact zone, and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene. the fault zone deformed right - laterally under ne - sw striking transtention, and new joints zone was produced at the end of the two main faults because of local stress concentration. the fault produced inchoative cataclastic rocks, and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks, which was during the himalayan movement

    其後的繼承性在斷裂帶內形成碎裂程度最強達到碎裂巖的碎裂巖系列構造巖,變形帶兩側育兩組典型的共軛剪節理;第二次在白堊世?始新世,斷裂在北東?南西向近水平擠壓作用下右行張扭性,斷裂帶兩主斷裂在斜列重疊的端部由於局部應力集中進一步擴展形成節理帶,而斷裂在巖體區也育兩組典型的共軛剪節理,斷裂內形成初碎裂巖為主的構造巖;第三次是喜山期以西側抬升、東側下降的強烈升降為主的,在基巖中,主斷層兩側圍巖出現微破裂。
  2. Until now, only the culex mosquito, which is active at night, has been shown to transmit west nile virus to humans

    迄今為止,現只有在夜頻繁的庫蚊能將西尼羅河病毒傳播給人類。
  3. The investigation and study for the structure of sports population in mo rning or evening in xian city, the need of the palaestra and other sports place for people, the lengthen and the master of spare time for the resident in xian city, the proportion of sports population in xian city, the focus of sports popul ation for the item of sports, the influence factors of the increase in sports po pulation are made by author, these results will contribute to the development of the sports for all movement in healthy and orderly way in xian city

    針對晨、練人群的隊伍結構組成、晨、練人群對體育場所的要求,西安市居民閑暇時間的多少和支配,西安市體育人口的比重,體育人口對體育項目的選擇,以及影響體育人口增長的因素等進行調查研究,旨在全面推西安市全民健身健康有序的展。
  4. The hotel also has restaurant, meeting room, multifunctional banqueting hall and can offer you and your friends the large service reception work, such as the large banqueting hall, news release, working meeting, team dinig, wedding party and evening sodality

    酒店還設有餐廳會議室多功能宴會廳,可以為你和您的朋友提供大型宴會新聞布辦公會議團隊用餐婚禮慶典聯誼會等到大型的接待服務工作。
  5. The main conclusions are as follows ; firstly, under the influence of three phases of episodic activities, three two - order sequences is composed of three depositional cycles and three regional unconformities ; secondly, under the control of structure activities such as fault - block activities and the influence of three - order climate cycles and source recharge, lower cretaceous can be divided into six three - order sequence ; thirdly, because fault activities is weak and fault slope is gently, fan deltas exist in steep slopes in early and later stages and subaqueous fans exist and turbidite fans exist in troughs in middle stage

    主要的結論為:其一,受三期幕式影響,斷陷形成了3個大的沉積旋迴和3個區域不整合面,構成了下白堊統3個二級層序;其二,受斷陷內翹傾和塊斷等構造的控制,以及三級氣候旋迴和物源供給因素的影響,下白堊統劃分出6個三級層序;其三,在單斷斷陷湖盆中,湖泊階段的早、期由於凹陷邊界斷層較弱,斷面較緩,陡坡可以育扇三角洲,在湖泊階段的中期主要為水下扇砂礫巖體,並在窪槽區育濁積扇。
  6. 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期和喜山期構造運的多期強烈改造;其產生、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影響最大,從而造就盆地今古面貌差異巨大。
  7. We have collected a mass of stellar activity and rotation data of late - type stars. combining with the results of hipparcos satellite, we reserch the relation between stellar activity and rotation ( include rotation period and rossby number ), and discuss the distribution of stellar rotation period and the evolution of angle momentum of late - type stars

    因此,我們收集了型恆星的色球和冕球的指數以及恆星自轉方面研究表的大量的觀測資料並結合hipparcos衛星的觀測結果,對型恆星的磁與恆星自轉間的相關性進行細致的研究。
  8. 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(特別是二疊世)的伸展方向可能生了改變,除在各斷裂帶繼承性外,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,燕山期為nne - ssw向擠壓,而喜山運可能經歷了從ew向向sn向方向擠壓的轉變。
  9. The most widely used opportunities of generating publicity are sponsorship of cultural activities, benefit evenings.

    揮公共宣傳作用最有利的時機是贊助文體、義演會。
  10. Tian shan extends east - west in central asia, the tian shan range was formed in later paleozoic, and a few intramontan basins appeared in mesozoic. it uplifetd again in early miocene because of the north - south compression induced by the india - asia collision, so many active structures can be found in tian shan. active tectonics took actions during last ten thousands yeas, and surface traces of fault scarps, detached gullies and folds in alluvial deposit are apparent, so it is easy to distinguish them from other geological phenomema

    天山位於亞洲中部,天山造山帶形成於古生代,到中生代時,在天山內部形成了一些山間盆地,印度板塊在始新世向北與歐亞板塊碰撞,天山受南北向擠壓力的作用再度于早中新世隆起,由於板塊碰撞的持續進行,在天山山間及山前育了許多的構造。
  11. During my master " degree investigation, i mainly focused on the coarse - grain stratigraphy within mesozoic basins in chengde and pingquan districts, the eastern yanshan, and did systemic provenance analysis and paleo - current direction measurement and studied the relationship among basin evolution, volcanism and tectonism. then i summarized the mesozoic basin development and the coupling characters of basin and mountain. the evolution of basin and mountain in this area can be divided into several stages : the stage of compression uplift and flexural basin during the triassic through the early jurassic, the stage of structural compression - volcanism and foreland basin during the middle and late jurassic and the stage of rift basin in the cretaceous

    在野外典型路線調查的基礎上,對燕山地區東段承德、平泉地區的中生代盆地中育的粗碎屑沉積層,進行了系統的物源分析與古流測定,並在此基礎上重點剖析了盆地的育、火山、構造變三者之間的關系,總結了本區中生代盆地育規律及盆山耦合特徵,並將盆山演化劃分為:三疊紀?早侏羅紀的構造擠壓隆升與撓曲盆地育階段階段,中侏羅紀的構造擠壓?火山與類前陸盆地育階段,早白堊世的拉張斷陷盆地育階段。
  12. When may came, nearby initiates reported that the flowers and trees in the area took on a flourishing look under the warm sunshine ; although it was still relatively cold early and late in the day. the japanese initiates decided to hold a one - day retreat at master s cabin while they were there and to prepare it for future group meditation sessions

    到了今年五月,住在附近的同修現,雖然群馬縣早氣溫仍舊很低,但在暖陽的照射下,此地的花草樹木已呈現欣欣向榮的景象,同修們便決定在師父的原木屋舉辦禪一,一方面也為日後在此地舉行的共修揭開序幕。
  13. Day care centres for the elderly provide a range of centre - based care and support services during daytime to enable the frail and demented elders suffering from moderate or severe level of impairment to maintain their optimal level of functioning, develop their potential, improve their quality of life and to enable them to live in their own homes wherever feasible and possible

    長者日間護理中心提供一系列以中心為本的日間照顧和支援服務,幫助身體機能中度或嚴重受損的體弱和癡呆癥長者,維持最高程度的能力展他們的潛能,和改善他們的生質素,以協助他們在可能的情況下,在家安享年。
  14. In the light of tectonic evolution stage and metallogenesis, these metallogenic system ( assemblage ) could be classified as follows : ( 1 ) the pre - divergent metallogenic system in the southwest margin of north china paleocontinent in the archean - meso proterozoic : dongdashan iron, jinchuan nickel - copper. ( 2 ) the divergent metallogenic system in the northern margin of the qaidam paleoplate in the middle - late proterozoic : huashugou - liugouxia iron. ( 3 ) the metallogenic system in the active margin in the early paleozoic : the metallogenic assemblage in the island arc - rift in the early stage ( baiyinchang - qingshuigou copper - polymetallic ) ; the metallogenic assemblage in island arc in the middle - late stage ( honggou - jiaolongzhang copper - polymetallic ) ; the back - arc extensional basin ( zhuzhuiyaba - jiugequan - shijuli copper ) ; the metallogenic assemblage in connection with subduction and magmatic - hydatogenesis ( taergou - xiaoliugou wolfram ; huashugou - liugouxia copper ; dadonggou - diaodaban lead - zinc ) ; the metallogenic assemblage is related to the oceanic crustal shards ( dadaoerji chromite ; yushigou chromite ). ( 4 ) the metallogenic system has something to do with collision - type orogeny : the metallogenic assemblage in foreland basin ( tianlu copper ) ; the metallogenic assemblage with the intracontinental orogeny and ductile shear ( hanshan - yingzhuishan gold )

    根據構造展階段和成礦作用特點,確定本區成礦系統及組合如下: ( 1 )華北板塊西南邊緣太古宙中元古代裂解期前成礦系統:東大山鐵成礦組合,金川鎳銅成礦組合; ( 2 )柴達木板塊北緣中、新元古代裂解成礦系統:樺樹溝柳溝峽鐵成礦組合; ( 3 )加里東期大陸邊緣成礦系統:早期島弧裂谷成礦組合(白銀廠清水溝銅及多金屬成礦組合) ,中、期島弧成礦組合(紅溝蛟龍掌銅及多金屬成礦組合) ,弧后擴張盆地成礦組合(豬咀啞巴九個泉石居里銅及多金屬成礦組合) ,與俯沖作用有關的巖漿熱液成礦組合(塔爾溝小柳溝鎢成礦組合,樺樹溝柳溝峽銅成礦組合,大東溝吊大坂鉛鋅成礦組合) ,洋殼殘片成礦組合(大道爾吉鉻成礦組合,玉石溝鉻成礦組合) ; ( 4 )碰撞造山成礦系統:前陸盆地成礦組合(天鹿銅成礦組合) ,陸內造山韌性剪切成礦組合(寒山鷹咀山金成礦組合) 。
  15. The cover faults in daqing region are mainly developed in formation of huoshiling member late jurassic and its cover formations. according to their formation period, activity characteristics and penetrating relationship, four types of faults were divided, that is fault - depression faults, depression faults, inverted - strike - slip faults and inverted - extension faults ; according to the activity history of the faults, five types of faults were divided, that is long - term active faults, early active faults, early - medium - term active faults, medium - term active faults and terminal active faults

    大慶地區內育在侏羅世火石嶺組及其以上的沉積蓋層中的蓋層斷裂,依斷層形成時期、特徵及切割層位可將蓋層斷層細分為四種類型,即斷陷期斷裂、坳陷期斷裂、反轉走滑斷裂和反轉張性斷層;按其歷史可以分為五種類型:即長期斷層、早期斷層、早-中期斷層、中期斷層和斷層。
  16. By evening this activity had been carried by the adjutants in all directions into every part of the army, and in the night of the 19th the multitude of the eighty thousands of the allied army rose from its halting - place, and with a hum of talk moved on, a heaving mass nine versts long

    間這項就由副官傳布到軍隊的各個部門。十九日更殘漏盡,八萬人馬的聯軍部隊從宿營地起身,笑語喧闐,人頭攢,有如一幅十里路長的巨型油畫,浩浩蕩蕩地出了。
  17. Field investigation reveals that the latest time when yumen fault, western part o f qilian mountains was active is the end of the late pleistocene, and that the fa ult is coincident with other faults around west jiuquan basin. it is also found t hat yumen fault had not simply restricted to dip - slip motion , strike - slip moti on is indicated. the results suggest that west jiuquan basin block might have rot ated clockwise

    新的證據顯示,位於祁連山西段酒西盆地南部的玉門斷裂的最新時代為更新世末,併兼有一定的走滑分量這一結果表明,酒西盆地塊體周邊斷裂的具有同時性的特點,酒西盆地塊體可能生過順時針旋轉
  18. The eastern yantai - weihai segment is a mid pleistocene segment on which no late pleistocene offset has been found

    東段煙臺威海段為中更新世段,沒有更新世地層錯斷現象。
  19. It is possible for the terminal activity faults to penetrate to the quaternary, but their scale is generally small and the penetrating distance is short, therefore, they can not induce earthquakes on a large scale. the remote sense images of last thirty years in daqing region show that the linear tectonics have not changed remarkbly, in the meantime, the earthquake timing figure shows that the probability of the faults inducing earthquakes, which ms is no less than 5, is little, though some terminal active faults have penetrated to the quaternary

    斷裂有可能斷至第四系,但規模小,延伸的距離短,不會引大規模地震,遙感解譯分析表明, 30多年來衛星遙感影像顯示的大型線性構造並無明顯變化;另外結合大慶地區地震時序圖認為,斷裂即使斷至第四系,其5級以上地震的可能性也極小。
  20. Thus, a group of non - governmental organizations and enterprises in chiayi, formosa, sponsored a benefit entertainment party entitled, " love in chiayi - show our concern for the youth " to raise funds to help these youngsters return to school

    福爾摩沙嘉義市各民間社團及企業因此起愛在嘉義-關懷青少年愛心慈善,以籌措經費,協助中途輟學之青年學生返回學校,繼續求學。
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