活動構造帶 的英文怎麼說

中文拼音 [huódònggòuzàodài]
活動構造帶 英文
active structure zone
  • 活 : 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...
  • 構 : Ⅰ動詞1 （構造; 組合） construct; form; compose 2 （結成） fabricate; make up 3 （建造; 架屋） bui...
  • 造 : Ⅰ動詞1 （做; 製作） make; build; create; produce 2 （假編） cook up; fabricate; concoct 3 [書面語...
  • 活動 : 1 （運動） move about; exercise 2 （動搖） shaky; unsteady 3 （不固定） movable; mobile; flexible...
  • 構造 : structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constituti...
  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

    其後的繼承性活動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，變形帶兩側發育兩組典型的共軛剪節理；第二次在晚白堊世?始新世，斷裂在北東?南西向近水平擠壓作用下右行張扭性活動，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，而斷裂在巖體區也發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活動，在基巖中，主斷層兩側圍巖出現微破裂。
  2. Geotectonically, the youjiang sedimentary basin was referred as youjiang yindosinian folded belt. triassic turbidites accumulated in the basin were derived from surrounding ancient lands including yuebei, jiangnan, and yunkai. tectonic setting of the sedimentary basin was in between an active continental margin and a continental island arc

    賦礦濁積巖系的主要物源區為盆地周圍的「越北古陸」 、 「江南古陸」和東邊地區包括欽防海西褶皺帶在內的「雲開古陸」 ，沉積構造背景介於大陸島弧和活動大陸邊緣之間的過渡構造環境。
  3. Having analyzed preliminarily formation mechanism of these common characteristics of anomaly, it concludes that : these are results, controlled by basically united tectonic stress field of large - range, caused by stress - strain accumulation and certain phase strong earthquakes, according to deformation difference brought about in tectonic position along the boundary zone and within second - order faults of active blocks resulted from unstable and inharmonious features for movement of block system at different levels and deformation of boundary

    分析這些異常共性特徵的形成機制，初步認為：是在基本統一的大區域構造應力場控制下，不同層次塊體系統運動及其邊界帶變形的非平穩、非協調性，在活動地塊邊界地帶和地塊內部次級斷裂構造部位產生變形差異而導致應力-應變積累、孕育強震到一定階段的結果。
  4. It includes plan on human resources, employment, development and training, achievement and assessment, reward and encouragement, building - up enterprise culture, and so on. this passage is divided into four sections : first, it analyses human resources management theory in order to maintain close ties with reality. second, through perspective of present human resources management status in huaxia bank, shenyang branch and comparison with that of foreign capital banks, in the end we get human resources management methods to huaxia bank, shenyang branch, we resist impulsion of foreign capital banks and catch hold of some points like organization design, position management, application and lection, training and development, performance management, compesation management

    全文共分四個部分：首先分析人力資源管理理論，目的是為了更好地聯系實際，其次通過透視華夏銀行沈陽分行人力資源管理現狀，以及與外資銀行的人力資源管理進行比較，最後得出華夏銀行沈陽分行人力資源管理對策，對策的提出是為了對抗外資銀行帶來的沖擊，本著與國際慣例接軌的原則，抓住組織設計、職位管理、招聘選拔、培訓發展、績效管理、薪酬管理幾個環節，提出全新人力資源管理理念，完成人力資源管理實踐活動，形成人力資源管理戰略，達到員工期望和需要，最終構建出以實現企業戰略和企業文化及價值觀為根本目的的人力資源問題解決方案，以應對入世后國內外銀行的激烈競爭，使華夏銀行能在未來的幾年內，建立起以「用真誠凝聚人才，用培訓提高人才，用利益驅動人才」的人力資源管理機制，構築人才高地，積極引進潛力，滿足華夏銀行入世后轉型再造和創新發展對人才的需要。
  5. The results indicate : ( 1 ) the distribution of magmatic rocks shows the feature that in the middle and western part of the study area basic igneous rocks dominate, and in the middle - eastern part intermediate rocks are predominant, while in the southeastern part acid ones are developed. ( 2 ) in the area west to the shiwandashan basin, intermediate magmatites were controlled by deep ne - striking and nw - striking faults, especially at the conjunction site of these two group faults, magmatic activity was strong ; and its tectonic background can be attributed to extensional continental rift

    其中，在十萬大山盆地以西地區的偏基性巖漿活動受北東和北西向深斷裂控制明顯，尤其以此兩組斷裂交匯處的巖漿活動強烈，盆地構造背景屬大陸伸展裂谷環境；在十萬大山盆地以東地區為偏酸性巖漿活動，主要受東吳運動形成的欽防造山帶的控制，屬大陸邊緣造山帶或島弧造山帶環境。
  6. A study of the tectonic activity of shenzhen fracture zone

    深圳斷裂帶構造活動性分析
  7. Strong earthquake activities in kekexili - east kunlun mountains active fault zone, northwest china

    東昆侖活動構造帶強震活動研究
  8. 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。
  9. 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，天山造山帶形成於晚古生代，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，在天山山間及山前發育了許多的活動構造。
  10. Active structure zone

    活動構造帶
  11. Based on the study of tectonic framework and seismicity in the north china plain, main seismotectonic belts are determined, and earthquake capacities of the belts are evaluated

    摘要本文分析了華北平原第四紀主要構造格局和強震活動特點，劃分了主要強震構造帶，並對其發震能力作了評價。
  12. Through the regional background analysis in which western structures developed, it suggested that there did not exist a united and steady block to the west of ordos basin. alashan block neighboring on the north of the western margin was largely influenced by the action of qilian and tianshan - xingmeng folded belt which is respectively to the south and north of alashan block, was narrow in the steady block and was limited by the longshou mountain - zhongwei strike fracture in the south area

    通過對鄂爾多斯盆地西緣構造發育的區域構造背景分析，認為在鄂爾多斯盆地之西，一直沒有一個統一的穩定地塊相鄰，與盆地西緣北部相鄰的阿拉善地塊，受南北相鄰的祁連褶皺帶和天山興蒙褶皺帶活動的影響，較穩定地塊的范圍比較狹窄，其南又有龍首山-中衛走滑斷裂構造帶存在。
  13. The analysis of structural movement and expression shows that qinqi tectonic active area is a volcano - sendimentary compressional depression formed by several times of compression movement from lower proterozoic, and spreaded in the direction of north step by step till the forming of xiangshan and miboshan group in mid - later period of ordovician, bearing hardly with volcanical rock

    從秦祁構造活動帶的構造形跡分析認為，該構造帶是自下元古以來多期擠壓環境下形成的火山一沉積壓陷，並一期又一期向北蠶食，于奧陶紀中後期形成基本不含火山巖的米缽山組、香山群壓陷巖系。
  14. The north - eastern structural zones which become intensity from the western part to the eastern one in gansu show a influence of marginal - west pacific indosinian - yanshan tectonic - magmatic belt on the western part of china ' s continent, and not only a important regional metallization had developed but also early - formed minerals were intense changed and enriched with the tectonic - magmatic activity

    甘肅境內由西向東增強的北東向構造帶，是我國東部濱西太平洋印支-燕山期構造巖漿活動帶向大陸西部的延伸表現；伴隨該期構造-巖漿活動，區內發生了重要的區域性成礦作用，並使處于該期構造活動帶的先期金屬礦產遭受了較強的疊加與再生改造。
  15. Therefore, the relationships of macroseismic epicentres and seismic epicentres of 133 main earthquakes in china and 66 events in north - south seismic belt with the active faults around these events are analyzed at detail in this paper. according to such results, a practical method to identify the most possible location of macroseismic epicentre has been proposed by the active faults around the instrumental epicentres

    本論文通過對全國133個及南北地震帶66個地震的宏觀震中及微觀震中與活斷層構造分佈背景關系的詳細分析，提出了可以根據定位震中周圍的活動構造背景來估計可能的宏觀震中的方法。
  16. Mesozoic to cenozoic magmatic activities in the cuoqin area of the gangdise belt were intensive and display temporal cycling and spatial zoning

    岡底斯構造帶措勤地區的中新生代巖漿活動強烈，從侏羅紀到第四紀均有不同程度的表現。
  17. It is concluded that the thrust structure formed in late - jurassic. faults with high angles appeared in hengshanbu structure part which is also developed in late - jurassic deduced by strata contact relationship. middle district includes two parts which

    橫山堡構造帶發育由東向西逆沖的高角度斷裂，根據地層接觸關系，推斷該構造帶的逆沖活動發生於晚侏羅世。
  18. We have also studied fracture formation and moving period by means of growth triangle zone and equilibrium section technology. the result is that fracture formation period in diffirentt struture zone are very d ' rffirent. the basic law is that from the north to the south, the fracture formation period is later and later

    利用生長三角帶和平衡剖面技術對斷裂形成時期和活動時期進行了研究，結果表明，不同構造帶斷裂形成時期存在很大差異，基本規律是從北到南斷裂形成時間越來越晚，但斷裂主要活動時期則在庫車期?第四系。
  19. Active tectonic zone

    活動構造帶
  20. The observation data of both leveling and base line from 32 sites located in yunnan and sichuan faults are processed. the active characteristics, the active quantities and directions about several of main faults are summarized

    通過對四川及鄰區（雲南省境內）的32個地殼形變跨斷層短水準、短基線測量場地觀測資料進行處理、分析，研究四川及鄰區主要是川滇塊體內各活動構造帶的斷層活動習性、量級和時序變化特徵。
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