斷裂系 的英文怎麼說

中文拼音 [duànlièxì]
斷裂系 英文
fracture system
  • 斷 : Ⅰ動詞1 （分成段） break; snap 2 （斷絕;隔斷） break off; cut off; stop 3 （戒除） give up; abstai...
  • 裂 : 裂動詞[方言] （東西的兩部分向兩旁分開） open
  • 系 : 系動詞（打結; 扣） tie; fasten; do up; button up
  • 斷裂 : break; disrupt; flying off; fracture; fragmentation; out break; rift;crack;bursting;rupture;rendi...
  1. In the tide of the afflux of knowledge from west to east, with the transplantation of modern legal system, development of legal education and the introduction of the western legal analysis method, both the legal system and the legal knowledge system of classical china ruptured, then collapsed

    隨著西學東漸，隨著現代西方的法制、法律教育與法學研究範式的全面導入，古典中國的法律制度結構與法律知識體系開始出現斷裂，並且迅速解體。
  2. 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?泥盆紀塔里木盆地南北緣均轉為活動大陸邊緣，形成了大量的斷裂和不整合；泥盆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。
  3. It is barely ten since systematic deep ocean bathymetry revealed the structure of rifts, fractures and trenches associated with sea floor spreading.

    系統的深海深度測量揭示了與海底擴張有關的狹谷帶、斷裂帶和海溝的結構。
  4. Finally, author have discussed the relationship transformation process of the honghe fault shear mode and block movement, proofed that the eta - type tectonic system was formed in miocene epoch

    討論了紅河斷裂剪切方式的轉變過程與巖塊運動的關系，論證了歹字形構造體系形成於約20ma的中新世時期。
  5. 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、盆地西南緣公郎弧形構造等是礦田尺度的控礦構造；多組斷裂的交叉、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。
  6. Fundamental of laser 40ar / 39ar dating method : our laboratory has successfully set up the laser microprobe 40ar / 39ar geological dating method. our works include adjustment of the high - gain electron multiplier in mass spectrometer and correction of mass discrimination, adjustment of the laser, test for absorption ability of minerals to laser, designing and manufacturing high - vacuum sample chamber, sample preparation and irradiation, research on the variability of j values on the surface of rock chips, measuring atmospheric argon, determination and correction of blanks and ages, etc. the laser microprobe technique is particularly effective for some geological samples. it can be used, for example, for research of distribution of the components in extremely small samples that are very difficult to be separated and purified and those which contain excess argon

    本文首先從常規~ （ 40 ） ar ~ （ 39 ） ar階段升溫定年實驗室的改進入手，進而建立了激光~ （ 40 ） ar ~ （ 39 ） ar定年實驗室，利用這兩種先進同位素地質定年方法，結合其他手段，對青藏高原腹地和北緣的阿爾金斷裂系多期地質事件進行了詳細的同位素年代學研究：一、參照國際先進實驗室的流程，對我們的常規~ （ 40 ） ar ~ （ 39 ） ar階段升溫實驗室在樣品的預處理、樣品的照射條件和系統空白測量及校正等方面進行了改進，使之產出的同位素年代數據更可靠並為國際同行所承認。
  7. Based on 3 - d seismic well and logging data, mainly by means of advanced seismic theories of reservoirs prediction and other corelational multidisciplinary, an extensive and indepth studying on the tight sandstone reservoir with fracture of the second part of the xujiahe formation in west sichuan depression has been carried out. a series of theoretical viewpoints and research fruition are concluded as follows :. 1 on the basis of analysis of the regional and local structure characteristics and evolution, a conclusion comes in to being : inchoate and nowadays structure traps and the match model between structure and fracturation system are the main factors in controlling the formation of effective traps

    本文綜合利用三維地震、鉆井、巖心、測井資料，採用地震儲層預測方法為主線的多學科綜合研究思路對川西坳陷上三疊統須家河組二段緻密裂縫性砂巖儲層進行了較為廣泛、深入的研究和探索，取得以下一系列理論認識和研究成果： 1 、通過區域及局部構造特徵及構造演化史分析，認為古今構造圈閉、構造與斷裂系統配置關系是控制有效圈閉形成的主要因素。
  8. 6. it is indicated that the fractures of marlite are next to de nan fault zone on the slice of seismic coherence. de nan fault zone is controlled by de nan fracture system, which is broom - like and is composed by faults no. l, no. 2 and no. 3 from north to south

    6 、利用先進的工作站上的相干技術和可視化技術研究裂縫發育帶、精細解釋了德南斷裂系並取得了好的成果，為目標選取提供可靠依據。
  9. The result is as follows : ( 1 ) cu - ag polymetallic mineralization field lied in the north of lanping basine between jinshajiang fissure and lancangjiang fissure, whose internal mid - axis fissures and different subfissures formed the fissure system of the basin. they were the transport system of the ore - forming fluid, which was important to the formation of copper - silver polymetllic deposits

    研究結果表明： （ 1 ）蘭坪白秧坪地區銅銀多金屬礦田位於金沙江斷裂和瀾滄江斷裂的之間的蘭坪盆地的北端，盆地內部的中軸斷裂和不同方向的次級斷裂，構成了盆地的斷裂系統，是成礦流體的運移系統，對銀、銅多金屬礦床的形成具有重要意義。
  10. One of the most important discoveries in this study is the regional exhalative sedimentary mineralization along the bobai - chenxi faulted zone in early palaeozoic, based on which, the metallogenic model of diplogenesis is developed for the fozichong orefield

    博白-岑溪斷裂帶在早古生代為一同生斷裂系統，在拉張環境下沿斷裂帶形成了一地塹型斷陷盆地。
  11. The investigation in the field was combined with research indoors. by classifying tectonic sequence, confirming corresponding prototype basin, analyzing paleo - tectonic stress fields in different periods, plotting correlative tectonic map based on 297 explore wells, and analyzing the traits of the remaining depressions producing hydrocarbon and their migration rules in the ordovician, the author studied the basement of the basin ; the fault system of the basin ; the tectonic - sedimentary evolution of the basin and its circumference areas ; the prototype basin and corresponding dynamics background ; the paleo - tectonic patte rn and its evolution in the layers of producing gas in different periods of ordovician ; the superposition relationship among the different period basins formed by different stress fields ; the reformation of the basin and the formation, redistribution and final emplacement of the gas pools

    採用野外地質調查與室內綜合研究相結合，通過構造層序的劃分及其相應盆地原型的確定、不同期次古構造應力場的分析、以297口探井數據為基礎的相關構造圖件的編制、奧陶系殘餘生烴坳陷及其遷移規律研究等的綜合分析，開展了盆地基底以及盆地斷裂系統、盆地及鄰區構造與沉積演化、盆地原型及其形成的動力學背景、奧陶系產氣層不同時期的古構造格局及其演化、不同期次構造應力場形成的不同世代盆地之間的疊置關系以及盆地改造與天然氣藏的形成、重新分配和最終就位諸方面的研究。
  12. Liaohe basin is a part of tanlu rifting system, and it belongs to continental rift basin

    遼河盆地是郯廬斷裂系的組成部分，屬大陸裂谷盆地。
  13. 7. the dabie orogenic belt is of transformation and superposition character. its new superimpose

    Ne向郯廬斷裂系的大型平移作用疊加在原來印支期消減帶之上，產生新的俯沖。
  14. Fault systems and their tectonic evolution in the eastern tarim basin

    塔里木盆地東部斷裂系統及其構造演化
  15. The fault system of the ordos basin includes the basin - surroundings fault system, the basement fault system, the platform cover fault system, and the platform cover fracture system

    將鄂爾多斯盆地的斷裂構造造劃分為盆地周緣斷裂系統、盆地基底斷裂系統、盆地蓋層斷裂系統和盆地蓋層裂縫系統。
  16. The mesozoic - cenozoic intracontinental strike - slip fault system and the associated hydrothermal uranium mineralization in the border area of eastern hunan and western jiangxi provinces

    湘贛邊區中新生代走滑斷裂系統及對熱液鈾成礦作用的控制
  17. Mesozoic - cenozoic continental strike - slip fault system and its roles on uranium mineralization in hunan and guangxi, china

    湘桂地區中新生代走滑斷裂系統對鈾成礦的控製作用
  18. In the jinshajiang suture zone, it lasted only a span of 9 ma from the start of subduction ( marked by the eruption of andesitic magmas and intrusion of intermediate rock of iag type at about 227 ma ) to the end of subduction, consumption of oce

    Iv期： 45ma以來，高原快速抬升；斷裂系活化，產生大規模走滑活動；巖體或被斷層切割、遷移，或抬升剝蝕。 ivi ： 45 25mi ，巖體和整個青藏高原一起呈周期性的、脈動式抬升。
  19. The study covers regional stratigraphy, regional geological structures and their evolution ; deep - large fracture system and building - moutain straps in the basin ; distributing of mineralization concentration area and mineralazition characteristics of different metal fields ; volcanic magmatic activity and magmatic distributing ; the petrology, element geochemistry features of the magmatic rock series ; the relationship between magmatic distributing and mineralization ; the relationship between magmatic forming - age and mineralization ; the relationship between magmatic form and mineralization ; source of mineral materials, source of hydrothermal solution and source of mineralizing agent ; transport forms of metal in the solution ; the ore - forming geochemical mechanism, etc. it turns out as follows : ( 1 ) lanping basin formed in the linkup of the plates and it was propitious to form deep - large fracture

    研究內容包括：區域地層及區域構造演化；盆地深大斷裂系統及造山帶；區域地球物理場；礦集區礦床的時空分佈、礦化特徵；巖漿巖活動與巖漿巖分佈；巖漿巖巖石學特徵；巖漿巖元素地球化學特徵；巖漿巖分佈與成礦的關系；巖漿巖成巖時代與成礦的關系；巖漿巖組成與成礦的關系；成礦物質的來源，成礦流體的來源；成礦物質搬運、富集的地球化學機理等。研究結果表明：蘭坪盆地發育于板塊的拼接地帶，有利於發育深大斷裂系統。
  20. In the northern part, the oceanic crust occurring between the bayan har and kunlun terranes started subduction from south to north at about 243 ma, and did not stop until the development of post - orogenic pog - type granite in the bayan har terrane at 220 ma, thus illustrating the orogeny in the form of subduction and collision kept active for over 20 ma

    以pog型花崗巖在巴顏喀拉地體內大量生成、在阿尼瑪卿巖帶中較多出現、在昆侖巖帶利金沙江巖帶少量出現為標志。期： 160 - 140ma ，斷裂系活動；金沙江、東昆侖剪切作用發生；部分巖體動力變質變形。
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