盆裂 的英文怎麼說

中文拼音 [pénliè]
盆裂 英文
fissured pelvic
  • : 1. (盛東西或洗東西用的器具) basin; tub; pot 2. (姓氏) a surname
  • : 裂動詞[方言] (東西的兩部分向兩旁分開) open
  1. Sometimes, leaning over the cracked, "tattle-tale gray" bathtub, he scrubbed his father's back, and looked, as the accursed son of noah had looked, on his father's hideous nakedness.

    有時,他俯身靠在了縫的「泄露秘密的灰色」澡上,一邊給父親擦背,一邊就象挪亞的那個遭人控告的兒子一樣,看著父親醜陋的裸體。
  2. Focused on archaean fractured reservoir of metamorphic rock in the damintun depression of liaohe basin, by the newly studied methods, the author predicts fractures in buried hills by drilling, coring, well logging and seismic data intergrately

    本文以遼河地大民屯凹陷太古界變質巖縫性儲層為研究對象,從技術研究的角度出發,首次探索了利用鉆井取芯、測井和地震資料綜合預測潛山縫發育的方法。
  3. 2. tazhong ancient uplift originated from normal fault in paleozoic, hydrocarbon formed in ordovician period, structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period, and it provided geologic background for the deposit of silurian - devonian stratum. tazhong uplift formed at the end devonian, ancient reservoir was destroyed and asphaltum sandstone formed, structure deformation more destroyed ancient reservoir in early permian, after then the major of structure deformation is regulation

    塔中隆起源於早古生代拉張背景下的正斷層,寒武-奧陶紀為其烴源巖形成的重要時期;早奧陶世末-晚奧陶世末的構造反轉是塔中隆起的主要形成期,同時也為志留系形成地層及復合圈閉提供了古地理背景;志留?泥紀塔里木地南北緣均轉為活動大陸邊緣,形成了大量的斷和不整合;泥紀末塔中鼻狀隆起基本定型,古油藏遭受破壞,形成了瀝青砂巖;早二疊世晚期的構造變形使古油藏遭受進一步的破壞;二疊紀后構造變動主要以調節為主。
  4. To achieve good results, try to locate breeding and hiding places of insects ( such as in dark spots, in corners of rooms, in cupboards, cracks in walls, pipes, ducts, behind and beneath sinks and refrigerators, storerooms, cabinets and rubbish bins, baseboards around window frames, door sills and etc. ) before spraying

    為令效果更理想,噴灑目標應為發現害蟲或相信有害蟲的地方,如:房間的黑暗墻角、墻壁縫、杯櫃和碗櫃、渠管、雪櫃背後、鋅底、貯物室、抽屜、垃圾桶、地腳線、窗框和門框周圍等。
  5. The hydrofracturing breccia is formed by deep rich - sodic and gold - hosted fluid hydrofracturing in a set of devonian system hot - water sedimentary rich - sodic rocks

    認為該水壓角礫巖體是深源富?含金流體在泥系一套熱水沉積的富鈉質巖系中發生水力壓作用形成的。
  6. Yitong basin is a big inland basin which was formed in cainozoic. chaluhe depression, which lies in the yitong, is a promising area for long - term oil and gas reservoir exploration

    伊通地是一個較大的新生代內陸陷型地,其中的岔路河斷陷為中長期油氣儲量接替勘探區。
  7. The results indicate that both caledonian basins in north and east guangxi evolved from fracturing to closure

    結果表明,桂北、桂東加里東期地演化均經歷了從拉張解到擠壓閉合的完整過程。
  8. 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、金沙江-哀牢山斷地中軸斷這三條巖石圈斷是主要的控-控巖(巖漿巖)構造及礦集區尺度的控礦構造;地中以三疊系為軸的背斜構造及相關的斷系統、地西南緣公郎弧形構造等是礦田尺度的控礦構造;多組斷的交叉、層間破碎帶及地層柱中的氧化還原界面是形成礦體的有利部位。
  9. Hefei basin that is located on the southern fringe of the north china plate and by the side of tan - lu fault zone is a mesozoic cenozoic continental basin

    合肥地為一中、新生代陸相地,位於華北板塊南緣、郯廬斷帶西側近旁側。
  10. ( 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、山關系以及更大尺度的斷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。
  11. Over ages, hot convection currents in this sea, as well as gravitational forces, move the plates and their superimposed continents and ocean basins, tearing them apart and rearranging them like pieces of a giant jigsaw puzzle

    隨著歲月流逝,海中熱對流及重力移動板塊及覆蓋在上面的大陸塊和海洋地,將它們撕再重新組合,如大拼圖游戲的碎片。
  12. 4 ) analyses boundary faults of the cenozoic longmenshan foreland basin, and thinks the basin boundary faults, being active fault, are thrust and dextral strike - slip. so the longmenshan foreland basin is dextral strike - slip foreland basin

    4 )通過對新生代龍門山前陸地邊界斷的考察分析,認為地邊界斷具逆沖推覆及右旋走滑作用特點,為活動斷
  13. Sxotf is recognized in the northern qaidam based on the analysis of structures of area. this oblique trusting fault zone with northwestern - southeastern trending consists of fault gouge, fault breccia and fault cleavage. fault hanging wall consists of sertengshan - xitieshan napple, which is distribution in dextral en echelon. fault footwall consists of youcangshan formation in neogene

    本文在對賽什騰? ?錫鐵山斜沖斷詳細地段構造解析的基礎上,結合地的沉積特徵、地球物理資料等對該斜沖斷的幾何學、運動學及形成時代進行了研究,論文著重探討了賽什騰? ?錫鐵山斜沖斷的地質意義。
  14. Molten lead and iron boiled in the marble basin of the fountain ; the water ran dry ; the extinguisher tops of the towers vanished like ice before the heat, and trickled down into four rugged wells of flame. great rents and splits branched out in the solid walls, like crystallisation ; stupefied birds wheeled about and dropped into the furnace ; four fierce figures trudged away, east, west, north, and south, along the night - enshrouded

    熔化的鉛和鐵在噴泉的大理石里沸騰,燒幹了泉水滅燭器似的塔樓尖頂在高溫前像冰一樣熔化,滴落下來變作了四個奇形怪狀的火池堅實的墻壁以結晶的紋樣作樹枝形迸,迸出了巨大的豁口和縫。
  15. High resolution borehole micro resistivity image logs ( fmi ) were used to investigate the origin of fracture structures, with tarim basin in northwest china as an example

    摘要以塔里木地為例,探討高解析度電成像測井資料在縫成因分析中的應用。
  16. Pore evolution model for xujiahe formation reservoir in west sichuan foreland basin

    海拉爾地蘇德爾特古潛山縫發育特徵
  17. Broken - foreland basin

    前陸
  18. The geochemical characteristics of gabbros from the jinshajiang ophiolitic melange indicate that they were derived from a mantle source different from that of volcanic rocks, which may be a product in the ocean rift in the earlier stage

    東竹林蛇綠混雜巖中輝長巖地球化學特徵表明,它與火山巖不同源,可能是洋盆裂谷初期的產物。
  19. The author also suggested that the fuxin block developed on the base of the geosyncline in the huabei craton, and had experienced three period process of orogeny, including hercynian folding orogeny in continental margin, mainly indo - sinian to early yanshanian intracontinental fold - faulting orogeny, and late yanshanian to early himalayaian intracontinental range - basin post orogeny

    認為阜新地塊是在克拉通陷槽基礎上發育起來的,經歷了海西期陸緣褶皺始造山、印支?早燕山陸內褶斷主造山、晚燕山?早喜馬拉雅陸內山後(重)造山等過程。
  20. Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin

    通過對平莊地基礎地質資料、國內外大量地熱地質資料的分析和野外地質調查、礦井實測地溫以及上升泉、斷層涌水的地球化學分析等工作基礎上,指出地處低地溫梯度背景區的平莊地地溫梯度異常是由於地基底隆起和坳陷引起傳導型大地熱流再分配所致;運用州sys數值模擬了大地熱流向地表傳導背景下的地地溫場,從而揭示了地基底(義縣組)頂界面地溫分佈特徵;闡明了地具有形成中低溫對流型地熱系統所必需的導水斷、補給水源等的良好條件,中低溫對流型地熱系統是地熱勘查的主要對象;圈定了平莊地北部朝陽溝?駱駝營子地熱勘查遠景區。
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