俯沖的 的英文怎麼說

中文拼音 [chōngde]
俯沖的 英文
diving
  • : Ⅰ動詞(低下) bend down; bow Ⅱ副詞[敬] (舊時公文書信中用來稱對方的動作) deign to; condescend to
  • : 4次方是 The fourth power of 2 is direction
  1. This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement, whose tectonic deformation and magma intrusion is fiercely, and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian, it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area, such as a - granite ' s stock, batholiths and diabase ' s dike. there are many fault depressions possible

    按照不同構造層,研究了各構造層構造特徵:基底構造層:受早海西期構造作用影響,與準噶爾洋盆閉合、而後陸-陸碰撞區域擠壓構造作用有關,為一構造變形和巖漿侵入活動強烈古生代褶皺基底。二疊系構造層:受中海西區域性伸展斷陷作用影響,盆地及其周緣地區發育與伸展構造有關構造-巖漿組合,如呈巖株、巖基狀侵位a型花崗巖以及呈巖墻狀侵位輝綠巖等。
  2. 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陸緣或島弧褶皺帶,具有古生代造山帶性質。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、造山帶增厚陸殼開始發生伸展垮塌構造環境;早白堊世火山巖形成於造山期后進一步發生伸展垮塌區域構造環境。
  3. 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弧形構造形成於古生代時期中國板塊與西伯利亞板塊碰撞帶,而在中生代,中國板塊下kula - pacific板塊向西導致了北北東向和北東向構造(如duimadao斷層、 diaoyudao斷層、 okinawa斷層、隆起帶和沉降帶)以及位於中國板塊東部火山巖漿帶。
  4. You can sit in one of the modified high - powered jeeps of the professional operators, and drive through water, over rocks, whirl about on the sand, and then hurtle downwards from the top of a sand mound as high as a five - story building. your heart will really race - there s simply nothing to compare with it ! sand dunes rising and falling just near the beach are one of the masterpieces created by the chinook - type wind that blows down off pingtung s mountains

    九棚與港仔兩大沙漠,面積廣達二百多公頃,冬季時,屏東特有落山風捲起狂沙,在海灘堆積出綿延沙丘,坐在飆沙業者特製改裝強力吉普車上,涉水越石在沙上橫直撞再從五層樓高沙丘頂端垂直,直令人心跳加速,大呼過癮!
  5. Thus, the paper focuses on mineralogy, petrology, petrogeochemistry, isotopic chorology, and sr - nd - pb isotopes of the mafic intrusions and dikes in fujian province, se china. in addition, we also discussed the process of the plate subduction, mantle evolution, crust - mantle interaction, lithospheric thinning and extension, and the reaction for crustal extensi on in fujian province, se china. ( 1 ) daiqianshan mafic intrusion is situated along the changle - nanao fault, which intruded in the metamorphic rocks

    基於此,本文以中國東南部福建省基性脈巖、巖體為研究對象,運用系統礦物學、巖石學、巖石地球化學、同位素地球化學及同位素年代學證據,詳細論述了晚中生代中國東南部板塊、地幔演化、殼幔相互作用及巖石圈伸展減薄地球動力學過程,探討了地殼拉張期次在福建省區域構造上響應。
  6. It was an excellent dive.

    真是一次十全十美
  7. So in addition to ordinary artillery, the german military was aided by a very large number of stuka dive bombers which could quickly and efficiently destroy the enemy obstacles in the tanks path ( artillery units, fortifications, infantry concentrations, bridges, convoys, etc )

    所以除了普通炮兵外,德國軍隊還裝備了大量斯圖卡式轟炸機,它能夠迅速有效消滅坦克推進道路上障礙(如炮兵,防禦工事,步兵集團,橋梁和護衛車隊等) 。
  8. Secondly, based on the microbeam analytical technique, on the one hand, through investigating the characteristic of major elements in the mantle minerals the author acquired the static information from mantle ; on the other hand, through multi - point analysis of a part of the minerals from mantle, the auther got dynamic information from mantle. finally, generalizating the fruits of this study and predecessors, the autor holds that the constituents of lithospheric mantle possibly includes spinel lherzolites, clinopyroxenites, websterite, dunite, harzburgites, garnet lherzite, phlogopite lherzite, eclogites, clinopyroxene megacrysts ; compared with east china and north china platform, the research field mantle shows the characteristics of higher degree of partial melting processes and more depleted mantle ; the. upper mantle beneath north hetian area is heterogeneous, with a tendency of deficit in a12o3 and lree from kaliyang in west hetian to the river basin of kalakshi river and yulongkashi river ; the subduction of the crust beneath north hetian has ever occurred in geological history and caused the mixing of mantle - crust ; the depth of the origination of basaltic magmas beneath north hetian exceeds 73km ; the thickness of the lithosphere beneath the research area amounts to 204. 9km ; the mantle beneath north hetian has geological condtions for forming diamond deposits

    最後,綜合本區幔源礦物和地幔巖石特徵以及地球物理資料,得出如下結論:本區上地幔物質組成有尖晶石二輝橄欖巖、二輝巖、單斜輝石巖、純橄欖巖、方輝橄欖巖、石榴石二輝橄欖巖、金雲母二輝橄欖巖、榴輝巖;與中國東部以及華北地臺上地幔相比,研究區上地幔具有富集主元素中相容元素和虧損其中不相容元素特徵,局部熔融程度較高;上地幔存在橫向和縱向不均一性,從西部克里陽到喀拉喀什河和玉龍喀什河流域, al和lree富集程度呈下降趨勢,不同來源相同礦物中主元素含量差異較大;地質歷史時期這里可能發生過地殼並產生殼幔混合作用;玄武巖漿起源深度73km ;從幔源重砂礦物溫壓估算結果,可以推斷出巖石圈厚度可達204 . 9km ;綜合巖石圈物質組成特徵、巖石圈熱狀態、地幔溫壓狀態、氧逸度以及幔源巖石和幔源礦物化學成分,認為研究區具備了金剛石成礦地幔地質條件。
  9. The authors consider that high - pressure epidote - blueschist, high - pressure eclogite, and ultrahigh - pressure eclogite formed at the same time, but at different depths

    認為高壓綠簾藍片巖相、高壓榴輝巖相、超高壓榴輝巖相是在同一帶內不同深度發生同期變質作用產物。
  10. A large number of studies of geochronology and geochemistry indicate that mesozoic intermediate - felsic rocks from the dabie orogen have originated from recycling of the subducted yangtze continental crust itself

    摘要大量同位素地質年代學和地球化學研究表明,大別山中生代中酸性巖為揚子陸殼再循環產物。
  11. At the course of subduction, collision and collage among the siberia, khazakstan and junggar blocks, the geotectonic environment underwent a few evolutional stages, they provided good congenital, parturient and postnatal conditions for the deposit

    在西伯利亞、哈薩克斯坦準噶爾板塊多階段、碰撞、拼合過程中,礦床所處大地構造環境經歷了多個開合演化階段,為該礦床提供了良好先天、臨產及後天條件。
  12. The temporal and spatial evolution of orogenic granitic belt shows certain kind of regularities : subduction type granites collision type granites extensional type granites

    造山帶花崗巖時空演變規律是:型碰撞型伸展型。
  13. The helicopter is allowed to fall the same distance that it climbed at the beginning of the maneuver before pulling the helicopter back to straight and level flight

    待直升機垂直俯沖的距離與垂直爬升距離相同時,拉起機頭恢復成水平直線飛行。
  14. Ages of generation and subduction of shiquan river ophiolite : restriction from shrimp zircon dating

    測年對獅泉河蛇綠巖形成和俯沖的時間約束
  15. 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

    這與從地質推斷過去2 3百萬年期間內,印度板塊向歐亞大陸平均為18mm / y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
  16. 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。
  17. The giant eagle swooping over the billows ? when drawing an eagle, we have to capture its stately posture of fierceness and valor over rolling billows as its background

    巨鷹擊浪圖:畫鷹一定要將其勇猛有力雄姿畫出來,背景配上澎湃浪潮,藉鷹向下俯沖的姿態,讓整個畫面形成強而有力動態美。
  18. Andall ofthat will need to be nose - down pitched

    那都是在俯沖的時候必須
  19. A little, but the rush was worth it

    一點點,但是俯沖的時候(危險)真是很值得
  20. B : a little, but the rush was worth it

    一點點,但是俯沖的時候(危險)真是很值得
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