弧形帶 的英文怎麼說

中文拼音 [xíngdài]
弧形帶 英文
arcuate zone
  • : 名詞1. [數學] (圓周的任意一段) arc2. (古代指弓) bow
  • 弧形 : arc; curve弧形避雷器 arc-arrester; 弧形槽 arc wall; 弧形構造 arc structure; 弧形閘門 [水文] radial gate
  1. Distant effect of jurassic collisions of qiangtang terrane, lasa terrane and paleo - pacific land onto the eurasian land made east qinling - dabie mountains in a compressional circumstance for a long time, and suppressed its orogenic extension ; whereas, cretaceous late - collisional extension and appearance of west pacific trench - arc - basin system relieved east qinling - dabie mountains of external compression, instantly result in violent orogenic lithosphere delamination - extension and depressurized - calefactive melting, and consequently, led to the formation of large scale early cretaceous granitoids and intermediate - acidic volcanic rocks

    羌塘地體拉薩地體和西太平洋古陸在侏羅紀與歐亞大陸拼貼碰撞的遠距離效應使東秦嶺大別造山長期處于擠壓環境,伸展作用被抑制白堊紀的碰撞晚期伸展和西太平洋溝盆體系的遠距離效應使東秦嶺大別地區的外部擠壓消失,導致造山巖石圈迅速強烈拆沉伸展和減壓增溫熔融,從而成大規模早白堊世花崗巖類和中酸性火山巖。
  2. The author suggests that the three lithosphere - scale faults, lancangjiang fault, jinshanjiang - ailaoshan fault and axis fault in the middle of the basin, are the main geological structures that control the formation of basin, magmatism and metallogenic congregate district. the anticline structure with an axis of triassic strata and the related fault system within the basin, and gonglang arch - shaped folding structure in the south of the basin are the geological structure controlling the formation of ore fields. junctions of two or more faults with different orientation, interlayer cataclastic structural zone and oxidation - reduction ( redox ) boundary were the favorable position for the formation of ore bodies

    認為瀾滄江斷裂、金沙江-哀牢山斷裂及盆地中軸斷裂這三條巖石圈斷裂是主要的控盆-控巖(巖漿巖)構造及礦集區尺度的控礦構造;盆地中以三疊系為軸的背斜構造及相關的斷裂系統、盆地西南緣公郎構造等是礦田尺度的控礦構造;多組斷裂的交叉、層間破碎及地層柱中的氧化還原界面是成礦體的有利部位。
  3. Chagan sag is a secondary tectonic unit in chagandelesu depression, northeastern yingen - eji ' naqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate, with the character of erogenic belt. in working area and its adjacent area, the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase

    查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元,其盆地基底為古生代時期華北板塊、哈薩克斯坦板塊和塔里木板塊交接部位成的陸緣或島褶皺,具有古生代造山的性質。研究區及鄰區印支期侵入巖成於造山強烈擠壓陸內俯沖的構造環境;燕山早期侵入巖成於由擠壓轉向拉伸、造山的增厚陸殼開始發生伸展垮塌的構造環境;早白堊世火山巖成於造山期后進一步發生伸展垮塌的區域構造環境。
  4. In this case during paleozoic, nearly east west trending arc structures resulted from the interaction between china plate and siberian plate. in mesozoic the westward subduction of kula - pacific plate under the china continental plate resulted in the nne and ne trend structures ( duimadao fault, diaoyudao fault, okinawa fault, uplifts belts and subsidence belts ) as well as volcano - magmatic belts in eastern of china plate

    本文所涉及近東西向展布的構造成於古生代時期中國板塊與西伯利亞板塊的碰撞,而在中生代,中國板塊下的kula - pacific板塊向西俯沖導致了北北東向和北東向構造(如duimadao斷層、 diaoyudao斷層、 okinawa斷層、隆起和沉降)以及位於中國板塊東部的火山巖漿
  5. 4. it is the first time that eclogite conglomerates are discovered in maotangchan and fenghuangtai formations. this suggests that ultra - high pressure metamorphic rocks in the dabie orogenic belt exhumed to the earth ' s surface in lower cretaceous. the geochemistry data indicates that the protoliths of the eclogite gravels formed in a structure setting of volcanic arc

    首次在毛坦廠組、鳳凰臺組中發現了榴輝巖礫石,這一發現表明大別造山超高壓變質巖在早白堊世已經折返到地表,而且地球化學研究表明這些榴輝巖礫石的原巖成於巖漿島構造背景。
  6. With the eggshell trim. - as many capes as you iike

    飾邊的那件-任由您挑選,將軍大人
  7. - with the eggshell trim. - as many capes as you iike

    -飾邊的那件-任由您挑選,將軍大人
  8. And apatite. by these analyses and comparison with general granite both in china and the world and with the granite in other au or cu belt in china, the characteristics of the granite in this area are concluded as follows. it belongs to magnetite - i or syntectic granite and has crust - mantle mixed characteristics ; it was formed mainly by crystallization differentiation of melting magma and multiphase varied intrusion ; the degree of differentiation evolvement is not high ; the granite and its enclaves p. re congenetic ; the range of temperature is about 500 - 700, the range of pressure is about 2. 50 gpa - 4. 35 gpa, and the range of oxygen fugacity ( lg fo2 ) is - 15. 53 - - 14. 00 ; most granite bodies formed before the collision of plates, and few formed after the collision of plates

    通過對測試數據的分析與綜合研究,並同中國和世界一般花崗巖類以及中國主要金、銅成礦巖體的花崗巖類進行對比,得出本區花崗巖類巖石具有以下特徵:屬磁鐵礦-型或同熔型花崗巖,其巖漿物質具殼幔混源特徵:主要由熔融態巖漿經結晶分異作用,通過多期變速上侵而成;其分異演化程度較低;寄主巖基和包體具有同源性;巖石的成溫度范圍約為500 - 700 ,壓力大約為2 . 50gpa - 4 . 35gpa ,氧逸度值1gfo _ 2為- 15 . 53 ? 14 . 00 ;該巖主要成於板塊碰撞前消減的活動板塊邊緣期,為燕山至喜馬拉雅早期的大陸邊緣火山環境的產物。
  9. And its special tectonic conditions contribute to the development of the deep - thick - incompact slopes growing in badong formation

    三峽庫區位於大巴山構造與八面山構造的接合部,構造變強烈,構造樣式多樣。
  10. 5. yulong - mangkang and leiwuqi - zuogong metallogenic belts are formed in collision - orogeny circumstance, and the ore - forming process is related with lava - thermal fluid tightly

    張性火山島環境下成了德格?鄉城成礦,成礦與火山沉積作用密切相關。
  11. The two tremendous continental countries shared a frontier of 4, 000 miles in a vast arc from the frozen tundras of siberia to the stark deserts of central asia.

    這兩個遼闊的大陸國家的共同邊界從西伯利亞凍土地到中亞細亞荒漠劃出一個大,長達四千多英里。
  12. 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,主要受東吳運動成的欽防造山的控制,屬大陸邊緣造山或島造山環境。
  13. The independent jiangda tectonic belt has appeared since late carboniferous, following the jinshajiang ocean crust of subducted beneath the changdu continental crust and the continental margin arc formed in east of changdu terrane

    自晚石炭世金沙江洋洋殼開始向昌都陸殼地體邊緣下俯沖,成陸緣以來,獨立的江達構造就得以產生。
  14. Fig. 1 - 1 a, straight ( rectangular ) tourniquets fit optimally on cylindrical limbs. b, curved tourniquets best fit conical limbs. ( from pedowitz ra, gershuni dh, botte mj, et al : clin orthop 287 : 237, 1993

    圖1 1a直(長方)止血最適合用於柱狀的肢體。 b止血適用於圓錐的肢體。
  15. The research result has suggested that in the southern and northern sides of the kangmar - hajinsangre dome zone, the east - west direction lineral structure forms outstanding arc - shaped of south, throughout all the region from west to east

    研究表明,在康馬?哈金桑惹隆起南北兩側,近東西向線構造呈向南突出的,自西向東貫穿全區。
  16. Northern three - river metallogenic belt is one of the most important nor - ferrous metal metallogenic belts in our country. reserves of cu, pb, zn, ag are very large. the area locates in arc bend of himalayan tectonic region, and is of unique tectonic character

    西南三江北段成礦是我國最重要的有色金屬成礦之一, cu 、 pb 、 zn 、 ag儲量豐富,並且地處喜馬拉雅構造域的拐彎地段,構造位置獨特。
  17. Outer dimension w1512 d1112 - 550 h760 2068 customized design, it helps you make full use of your room space, especially the arc shaped desk brings your room more colorful element, also sets of drawers, rack for host computer and keyboard, bookshelf including doors, drawer divider would be attached

    尺寸: w1512 d1112 - 550 h760 2068 ;合理利用空間,量身定做,圓的線條美設計,為您的家居空間增添亮麗的色彩。可配置抽屜櫃主機架鍵盤架書架可掩門格子架等
  18. Arc - shaped fault break slope system and its control on low stand systems sandbodies in dongying depression

    東營凹陷斷裂坡折系統及其對低位域砂體的控制
  19. Formed by passive emplacent of crust - mantle mixed type of magma and controlled by nearly ns - trending baodu - boluo arcuate fault zone, the himalayan porphyry belt in ninglang area tends generally to plunge northward

    摘要寧蒗地區喜山期斑巖受近南北向的包都波羅斷裂控制,由殼幔混源型巖漿被動侵位而成,總體上呈向北逐漸傾伏的趨勢。
  20. Outer dimension w1208 d600 h760 2068, customized design, it helps you make full use of your room space, especially the arc shaped desk brings your room more colorful element, also sets of drawers, rack for host computer and keyboard, bookshelf including doors would be attached

    尺寸: w1208 d600 h760 2068 ;合理利用空間,量身定做,圓的線條美設計,為您的家居空間增添亮麗的色彩。可配置抽屜櫃主機架鍵盤架書架可掩門等
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