歐亞板塊 的英文怎麼說

中文拼音 [ōuyǎbǎnkuāi]
歐亞板塊 英文
eurasia late
  • 歐 : 名詞1. （姓氏） a surname 2. （歐洲的簡稱） short for europe
  • 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）
  • 歐亞 : eurasian歐亞大陸 eurasia
  • 板塊 : [地] plate板塊邊緣 plate margin; 板塊構造 plate tectonics; raft tectonics; 板塊假說 plate hypothe...
  1. ( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper. the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting, which is of great theory significance for studying regional structural framwork, relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin. moreover, the result is of guidance significance for the forecast of combination gas, distributing and formation of nappe metal deposit in northern qaidam basin

    （ 6 ）論文探討了賽什騰? ?錫鐵山斜向逆沖推覆構造的地質意義，認為賽什騰-錫鐵山斷裂斜沖作用是印度板塊與歐亞板塊碰撞、會聚的遠程效應的結果，該認識對于研究柴北緣區域構造格局、盆山關系以及更大尺度的斷裂帶或造山帶的斜向逆沖作用具有理論意義，對柴達木北緣的油氣預測、推覆體金屬礦床的分佈、形成具有指導意義。
  2. The result of geodetic inversion shows that india block moves at rates of 20. 4 millimeters per year with respect to the stable eurasia, consistent with the result comes from geology. this indicates that the rate india block moves towards eurasia is stable

    這與從地質推斷的過去2 3百萬年期間內，印度板塊向歐亞大陸俯沖平均為18mm / y的速率大致相同，表明在較長時間范圍內，印度板塊向歐亞大陸俯沖的速率是穩定的。
  3. Due to the west north direction subduction, fast collapse ( delamination ) may take place and the mantle plume emerged in ludong, in addition, owing to the subduction of pacific plate under eurasian, there appeared left - lateral advection and extension for tan - lu faults ( named as yishu fault in shandong ), and together with the collapse of yanshanian orogenic belts, all induced the crustal extension in shandong

    由於太平洋板塊對歐亞板塊的俯沖（ nw向） ，魯東地區巖石圈發生了快速拆沉減薄作用，同時魯東地區也可能會出現地幔柱的活動；另外，在太平洋板塊俯沖作用影響下，郯廬斷裂（山東稱沂沭斷裂）帶發生了大型左行走滑剪切和拉張活動。
  4. The collision between continental plates is a key to understanding the evolution of continental dynamics. perhaps the most spectacular large - scale result of plate tectonics is the broad complicated zone of intracontinental convergence between eurasia and peninsular india following their collision at about 45 ma

    大陸內部的陸-陸碰撞過程是大陸動力學的核心問題，青藏高原被視為印度板塊與歐亞板塊于新生代碰撞的結果，是典型的陸-陸碰撞帶。
  5. 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。
  6. To benzilan ( where visitors can view the geological legacy of the collision of the european - asian plate with the indian sea plate ), then on to the dongzhu temple group, and then proceeding to baimang snow - capped mountain, and the feilai temple in deqin, and on to meili snow - capped mountain, mingyongqia glacier, and xidang hot springs from which one can continue on to the yuben fairy waterfall

    由中甸為起點，松贊林寺、納帕海、奔子欄（游覽歐亞板塊與印度洋板塊碰撞地質遺址） 、東竹林寺、白茫雪山、德欽飛來寺、梅里雪山、明永恰冰川、西當溫泉、雨崩神瀑。
  7. 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。
  8. We deduce that it is a relic old crust that was brought upwards during the formation of neo - tethyan ophiolite. the step heating 40ar - ' 9ar spectra show that during 100ma, luobusha ophiolite suffered intensely alternation, which affected distinctly the k - ar system ; during 771ma some basalt formed in the country rock of xiubugabu ophiolite ; during 55ma, the pillow basalt of rikangba ophiolite affected by a strong thermal event ; all the variety of ages illustrates possible impacts of the subduction - collision between india and eurasia. through dissecting mainly the gabbro of luobusa ophiolite and studying the 40ar / 39ar

    ~ （ 40 ） ar ~ （ 39 ） ar階段升溫年齡圖譜顯示， 100ma左右羅布莎巖體經歷了較強的後期蝕變作用，對其k ? ar體系造成明顯影響； 77 1ma休古嘎布巖體圍巖中形成玄武質火山集塊巖； 55ma日康巴巖體巖石枕狀玄武巖受到較強熱事件影響；這些~ （ 40 ） ar - ~ （ 39 ） ar年齡上的變化顯示了印度板塊與歐亞板塊俯沖?碰撞對該區的強烈影響。
  9. The southeastern china locates at the joint of the pacific plate and eurasian plate. the special geological location and structural movements have received considerable attention by geologists

    中國東南部地處太平洋板塊與歐亞板塊的接合部位，其獨特的地理位置和構造運動長期以來引起了地質學家的廣泛關注。
  10. When the tectonic system completely changed from paleo - asian tectonic circle to shore pacific tectonic circle, and established the elementary tectonic framework of shandong province. from then on, the tectonic movements of shandong were ascribed to the subduction ( north - west - trending ) of pacific plate under eurasian

    燕山期（ 205 65ma ）山東地區地殼活動強烈，構造體系已由古亞洲構造域完全轉化為濱太平洋構造域，構造活動導源於太平洋板塊對歐亞板塊的俯沖。
  11. Because mount jade was built by euro - asia plate and philippine plate, it has an elevation of 3952 meters, and a cross shape

    玉山山塊因歐亞板塊和菲律賓板塊相擠撞而隆起，主脈略呈十字型，海拔3952公尺。
  12. But at sicily the african and eurasian plates are colliding, so one would expect the stresses to be compressive rather than extensional

    但是在西西里島，非洲板塊和歐亞板塊相撞，因此有些人會認為這里的應力是壓縮而非伸張。
  13. This system plays an important role in the relative movement between the west pacific plate and eurasian continental plate. thus, the paleozoic structures had been modified

    此斷層系列對于西太平洋板塊與歐亞板塊之間的相對運動起重要作用，於是古生代構造帶被改造。
  14. As the plate collides into and slips under the massive eurasian plate to the north, it lifts the world ' s highest mountain ranges, the himalayas, even higher

    這個板塊以每年40公釐的速度往北移動，當它跟北邊巨大的歐亞板塊發生碰撞，或者是滑入歐亞板塊時，世界最高的喜馬拉雅山脈也被墊得更高了。
  15. We find the movement velocity field and distribution of strain field in the middle tianshan mountain relative to eurasia plate by analyzing the continuous observation datum of gps in the region

    摘要通過對天山中部地區連續多年的gps觀測分析，得到了該監測區相對歐亞板塊的運動速度場及應變場分佈情況。
  16. Big tsunamis are caused by great submarine earthquakes that mainly occur along the circum - pacific seismic belt, and along the active seismic belt between the eurasian tectonic plate and the indian - australian tectonic plate

    引發嚴重海嘯的海底大地震大多發生在環太平洋地震帶或歐亞板塊及印澳板塊之間的活躍地震帶。
  17. Geologists and geophysicists have carried out substantial work on petrology, geochemistry, chronology and geophysics, et al., which yields important reference material and constrains for explanations of questions, such as the delamination and exhumation mechanism for the lower crust, models of the rapid uplift of himalayan orogen and deep subduction of india - eurasia plate. while only a little has been done to study the eastern syntaxis at present

    地質學家和地球物理學家已經對西構造結進行了大量的巖石學、地球化學、年代學和地球物理學等方面的研究，為解釋下地殼的拆沉、折返機制，喜馬拉雅造山帶的快速隆升和印度-歐亞板塊的大陸深俯沖模式等提供了重要的參考信息和約束條件。
  18. ( 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。
  19. Indus - tsangpo suture zone is the joint of indian plate and eurasia plate. the study on its evolution history can provide us dynamic evidence for continent - continent collision between indian plate and eurasia plate. then what is the formation mechanism and deformation history for the indus - tsangpo suture zone

    雅魯藏布江結合帶是印度板塊和歐亞板塊碰撞的結合部位，研究其演化歷史能夠為解釋印度-歐亞板塊的陸-陸碰撞提供動力學方面依據，那麼本區雅魯藏布江結合帶的形成機制和變形歷史又是怎樣的呢
  20. 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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