板塊擠壓 的英文怎麼說

中文拼音 [bǎnkuāijǐyā]
板塊擠壓 英文
plate jams
  • 板 : Ⅰ名詞1 （片狀硬物體） board; plank; plate 2 （專指店鋪的門板） shutter 3 [音樂] （打拍子的樂器） ...
  • 塊 : 名詞（古時佩帶的玉器） penannular jade ring （worn as an ornament in ancient china）
  • 擠 : 動詞1 （人、物緊緊挨在一起; 事情集中在同一時間內） crowd; pack; cram 2 （使勁用身體推開人或物） j...
  • 壓 : 壓構詞成分。
  • 板塊 : [地] plate板塊邊緣 plate margin; 板塊構造 plate tectonics; raft tectonics; 板塊假說 plate hypothe...
  • 擠壓 : cirmp; squeeze; mouthpiece pressing; nobbing; extrusion; squeezing; battering
  1. 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形成的陸緣或島弧褶皺帶，具有古生代造山帶的性質。研究區及鄰區印支期侵入巖形成於造山帶強烈擠壓陸內俯沖的構造環境；燕山早期侵入巖形成於由擠壓轉向拉伸、造山帶的增厚陸殼開始發生伸展垮塌的構造環境；早白堊世火山巖形成於造山期后進一步發生伸展垮塌的區域構造環境。
  2. Mountain building occurs during rapid subduction of one plate under another

    當一個板塊迅速地擠壓到另一個板塊下面時會發生造山運動。
  3. Areas beneath the mountain belts are under compression while areas beneath basins and the foredeep of the indian plate are under compression

    區內造山帶下方均處于擠壓；盆地和印度板塊前緣處于拉張。
  4. The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep. under the background of indian plate subducting under asia - europe plate, bachu forebulge was greatly affected by the development of southwest depression and awati depression. almost all of its structure reversed, and as a result of it, both of its south and north boundary migrated. according to its evolution history and its feature, the authors tentatively use both - side migration model to interpret the evolution of compound forebulge. since triassic, almost all the spheres above lithosphere synchronously became flexure. because transpressional stress field became increasingly strong, bachu forebulge continued uplifting and big faults formed. then, bachu uplift, as a whole, slipped upward along those big faults and showed migrating toward thrust zone in plane. in tectonic tranquility, the lithosphere bounded back and in consequence of it, bachu uplift slipped down and showed migration toward craton, at that moment negative inversion structures developed. while the forebulge migrated toward its south and north foredeep, it was very possible that locally extensional stress appeared in the forebulge

    在印度板塊向歐亞板塊俯沖的大背景下，巴楚前緣斷隆受西南坳陷和阿瓦提凹陷的影響，新生代時構造體制發生反轉，邊界向南北遷移。根據其發育過程特徵，作者用復合前緣隆起兩端遷移模式對復合前緣隆起獨特的構造發育史進行了解釋：即三疊紀以來巖石圈各圈層同步撓曲變形。隨著擠壓應力場的增大，巴楚隆起在撓曲基礎上不斷抬升，形成幾條大型斷裂帶。
  5. After growing to a certain height, the effect of gravity and collision - generated extrusion will make them grow wider, but not higher, bian said

    邊教授說，喜馬拉雅山達到一定高度后，在重力和由板塊碰撞產生的擠壓力的作用下，山脈會向外擴展，而不會持續增高。
  6. 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。
  7. Subduction can release pressure by pushing flakes of land that separate from lower stratas forward

    板塊擠壓把較低的地層上面的陸地向前推，這可以釋放壓力。
  8. The two island groups are the peaks of an undersea mountain range, raised by the scraping up of soft sediments as the plate ' s leading edge pressed down and forward against the india plate

    這兩個群島是海底山脈的山峰，它們是緬甸板塊擠壓印度板塊時，緬甸板塊前端下沉至印度板塊下方，並持續向前推進，其前沿的軟質沉積物被颳起、逐漸累積而成。
  9. In the late early cretaceous, the ncc turned into contraction stage again by the influence of the subduction of pacific plate and indian plate

    早白堊世晚期該區受太平洋板塊和印度洋板塊俯沖作用影響，華北板塊再次轉入擠壓作用階段，開始了濱太平洋域的演化。
  10. During subduction northward of neo - tethys oceanic plate, ayla - zhongba micro - continental, the marginal ocean basin and india continental drifted northward all together, the marginal ocean basin was gradually contracted and closed by compressed of india continental

    在新特提斯洋板塊向北俯沖消減過程中，阿依拉仲巴微陸塊、陸緣洋盆和印度大陸一起隨著向北漂移，在印度大陸向北擠壓作用下洋盆逐漸收縮以致最終閉合。
  11. The story begins around 250 million year ago when the planet s hypothetical landmass pangea split, unleashing massive climatic powers across the globe. moving back into the 20th century, the film then examines the landscapes, wildlife, ecosystems and indigenous cultures of each of the seven locations

    這些板塊本來連接在一起，后來分裂及在地幔上漂移，更互相碰撞及擠壓，逐漸形成各大陸海洋山脈和島嶼，也帶來了火山爆發和地震等地殼活動。
  12. The story begins around 250 million years ago when the planet s hypotherical landmass pangea split, unleashing massive climatic powers across the globe. moving back into the 20th century, the film then examines the landscapes, wildlife, ecosystems and indigenous cultures of each of the seven locations

    這些板塊本來連接在一起，后來分裂及在地幔上漂移，更互相碰撞及擠壓，逐漸形成各大陸海洋山脈和島嶼，也帶來了火山爆發和地震等地殼活動。
  13. ( 4 ) the collision zones of eurasia are very complicated due to the extrusion of continent lithospheres and the subduction between the oceanand continent lithospheres, and we analyze the mutual effects of different lithospheres and the crustal deformation features of collision zones ( 5 ) firstly we give the present - day spreading velocity of the mid - atlantic ridge

    （ 4 ）系統分析了歐亞碰撞帶大陸與大陸和大洋與大陸兩種截然不同的巖石圈擠壓與俯沖對歐亞板塊的影響及其邊界地殼形變特徵。
  14. The effect of the indio - australian plate taking a dive under the himalayas is to relieve tension along the african rift, such that this tears, promptly, but in shuddering steps with halting adjustments pauses between shudders

    印澳板塊被壓入喜馬拉雅山脈之下這一結果減輕了沿東非大裂谷的水平方向的擠壓力，所以它們就迅速地撕裂了，並且是在一步步地震動、調整暫停、震動之間完成這一過程的。
  15. Pin is designed to serve as both a spacer and a pilot pin. when squeezing action embeds its head into a hold in a metal sheet, displaced material of the sheet is compelled to flow into the groove of the pin head for self - clinching

    導銷集間隔墊塊和引導銷於一體，當它頭部被沖壓進金屬板上孔中時，板上材料會被擠進導銷頭部上的槽內從而使導銷自行固定
  16. By means of gps velocity field data, the synthetically crustal media parameters of the plateau were reversibly analyzed, as well as the simplified boundary function forces. thus, the moving tectonic characteristics of the plateau were analyzed macroscopically. finally, the main conclusions are that the majority of tectonic deformation of the plateau is the n - s compression and the minority is the w - e stretching

    首先通過gps速度場反分析了高原地殼的綜合介質參數，並反分析了簡化后的高原地殼的邊界作用力，從宏觀上分析了青藏高原的構造運動特徵，分析結論認為：青藏高原的構造變形以南北擠壓為主，東西擴張為輔；造成高原現今構造格局的主要原因是印度洋板塊和歐亞板塊的持續碰撞。
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