活動斷層 的英文怎麼說
中文拼音 [huódòngduàncéng]
活動斷層
英文
active fault- 活 : Ⅰ動詞1 (生存; 有生命) live 2 [書面語](救活) save (the life of a person):活人無算 (of a goo...
- 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...
- 層 : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
- 活動 : 1 (運動) move about; exercise 2 (動搖) shaky; unsteady 3 (不固定) movable; mobile; flexible...
- 斷層 : fault; slip; slicle; fracture; dislocation
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Along some active faults we can see clear alignments of microearthquakes.
微震清晰地沿著某些活動斷層排列著。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。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,研究了各構造層的構造特徵:基底構造層:受早海西期構造作用的影響,與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的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的古生代褶皺基底。二疊系構造層:受中海西區域性伸展斷陷作用的影響,盆地及其周緣地區發育與伸展構造有關的構造-巖漿組合,如呈巖株、巖基狀侵位的a型花崗巖以及呈巖墻狀侵位的輝綠巖等。With the carryout of it, we have prompted the democracy of the country, and we have got great achievements. however, with a big population and complex situations, we still have some problems in applying it in practice. i have been participating in groundwork in villages and towns for more than ten years and put it in practice in person. as a missionary,
我在鄉鎮從事基層工作十幾年,直接參與了村民自治的實踐活動,做為推動村民自治的鄉鎮工作人員,對村民自治有著直接的感受,也嘗到了村民自治過程中的酸甜苦辣,並在實踐中進行不斷的思考總結和探索。The fault controlled the magmatism and metallization relevant to the contact zone, and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene. the fault zone deformed right - laterally under ne - sw striking transtention, and new joints zone was produced at the end of the two main faults because of local stress concentration. the fault produced inchoative cataclastic rocks, and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks, which was during the himalayan movement
其後的繼承性活動在斷裂帶內形成碎裂程度最強達到碎裂巖的碎裂巖系列構造巖,變形帶兩側發育兩組典型的共軛剪節理;第二次在晚白堊世?始新世,斷裂在北東?南西向近水平擠壓作用下右行張扭性活動,斷裂帶兩主斷裂在斜列重疊的端部由於局部應力集中進一步擴展形成節理帶,而斷裂在巖體區也發育兩組典型的共軛剪節理,斷裂內形成初碎裂巖為主的構造巖;第三次是喜山期以西側抬升、東側下降的強烈升降為主的活動,在基巖中,主斷層兩側圍巖出現微破裂。Following the idea of coseismic stress - triggering, coseismic strain steps recorded by borehole strainmeters are used to study coseismic stress - triggered fault slips
摘要沿著同震應力觸發的思路,提出了利用鉆孔應變觀測記錄的同震應變階反演同震應力觸發斷層活動的方法。In the process of social transition, the memory of community becomes vague, thus lineage activities are no very common. in addition, due to the slight economic difference, several community elites exist, but among them there are no dominative elites
由於社區變遷的影響,社區記憶變得模糊甚至斷裂,因而社區中宗族活動不強烈;又因為村莊經濟分層不明顯,故村莊存在多種類型的社區精英,但又缺乏佔主導優勢的社區精英。Active faults ; earthquake ; seismogenic faults ; epicenter
活動斷層地震發震構造震中For a long time researchers believed that etna ' s position at the crossroads of these faults was the explanation for its volcanism
長久以來,研究人員相信埃特納火山活動的原因,正是因為它位處這些斷層的交會處。On the east terrace - fault slope of the depression, the sedimentary mode of fan - shaped delta - slump turbid fan - deep lake facies are developed. on the long axial direction of fula depression, the southeastern groove was filled with a large scale delta which was the main sources, the other little delta limited by the 3 syndepositional fault was distributed down the slope edge of the northern sub - depression. this stage developed a favorable oil sources, reservoir and regional seal which formed the good matching relations of generation, reservoir and seal in the time - space zone
Abugarbra組的sc和sd層序發育在邊界斷層和同沉積斷層活動劇烈、湖盆擴張期,凹陷中心發育半深湖-深湖相沉積,在凹陷陡坡發育近岸水下扇,斷階緩坡帶發育扇三角洲?滑塌濁積扇?深湖相組合,長軸凹槽和北部次凹的北部緩坡帶發育三角洲體系,此層位是有利生油層和巖性圈閉發育層段。Active faults or tectonic lines are clear boundaries between a very active region and a quiet region.
活動斷層或構造線是強烈活動已和平靜區之間的清晰邊界。Yanqi basin is an intermont basin of tian shan, there is a nww trending right lateral strike slip active fault in southwestern basin, its maximum slip distance is 210m, and slip rate is about 10mm / yr, moreover, there is a west - east trending active anticline along northern basin
焉耆盆地是一個天山山間盆地,盆地西南緣發育一條走向北西西的右行走滑活動斷層,最大走滑距離為210m ,走滑速率約10mm / yr ,盆地西北緣發育走向近東西的活動褶皺。Base on the definition of active fault and its meaning to engineers, this paper reviews some geological aspects and problems, such as the application of dating results in determination of active faulting ages, seismo - tectonics background studying on moderate - strong earthquakes, estimating earthquake recurrence from geological investigation, and probabilistic evaluation of the ground offset of active fault
摘要本文在對活動斷層的工程涵義進行了簡要分析后,討論了斷層物質測年的工程應用進展及其斷層活動時代鑒定問題,並就如何加強中強地震發震構造判別、應用地震地質資料評估大地震年平均發生率、以及活動斷層地表斷錯位移的概率評價等問題作了初步探討。The cover faults in daqing region are mainly developed in formation of huoshiling member late jurassic and its cover formations. according to their formation period, activity characteristics and penetrating relationship, four types of faults were divided, that is fault - depression faults, depression faults, inverted - strike - slip faults and inverted - extension faults ; according to the activity history of the faults, five types of faults were divided, that is long - term active faults, early active faults, early - medium - term active faults, medium - term active faults and terminal active faults
大慶地區內發育在晚侏羅世火石嶺組及其以上的沉積蓋層中的蓋層斷裂,依斷層形成時期、活動特徵及切割層位可將蓋層斷層細分為四種類型,即斷陷期斷裂、坳陷期斷裂、反轉走滑斷裂和反轉張性斷層;按其活動歷史可以分為五種類型:即長期活動斷層、早期活動斷層、早-中期活動斷層、中期活動斷層和晚期活動斷層。6. 5 earthquake in the west of beijing in 1730 together with the data of drills, electromagnetism and gravity, the qinglongqiao - qiliqu and shahe active faults are identified for the first time. although at present all aspects of the earthquake are not fully known, the authors consider that the two active faults are responsible for the earthquake and the first one plays the leading role
在前人研究1730年北京西郊6 . 5級地震的基礎上,綜合井孔電磁和重力資料,經分析初步確定了青橋七里渠活動斷層和沙河斷陷南緣活動斷層的存在及其位置規模和基本特徵,認為這兩條活動斷層是此次地震的發震構造,其中青橋七里渠斷層在此次地震中起主導作用。The establishment of seismogenic faults and epicenter of the earthquake will benefit for the disaster mitigation and city construction of beijing
這些活動斷層和震中位置的確定,有利於首都地質災害防治和城市建設。This paper discusses the features of active fault through data analysis by using short water level across the fault to measure and set up the monitor net of south branch of the yamalike fault deformation
摘要利用跨斷層短水準測量,建立了跨雅瑪里克斷裂南支斷層形變監測網,通過資料分析得出該斷裂帶斷層活動特徵,確定了雅瑪里克斷裂為全新世早期活動斷裂。Temporal variation of the seismic activity along the active fault is closely related with similar variations in others.
沿活動斷層的地震活動性隨時間的變化與其他活動斷層的類似變化密切相關。These phenomena indicate that heavy rainfall is a kind of trigger for the occurrence of earthquakes which occur along the fractured zones of the active faults.
這些現象表明,大雨是發生於活動斷層斷裂區的那些地震的一種觸發因素。Main works : fractal and mechanism of forming fractal of fault surface in rock masses is analyzed and examined with it ' s affect on failure process of mining rock masses ; fractal curves are constructed with matlab to simulate the fault surface. similar material modeling is carried out and the fractal weak - face effect of mining rock masses is studied. mechanics character of rock masses with fractal fault in mining condition is simulated with large finite element software an sys ; catastrophe model of fault activated by mining is constructed with catastrophe theory
主要工作有:檢測和分析了巖體斷層面的分形性和斷層面分形的形成機制及其對采動巖體破壞的影響機理;運用matlab構造了分形曲線來模擬分形斷層面,進行了相似材料模擬實驗,研究了采動巖體的分形弱面效應;採用大型有限元軟體ansys模擬了含有分形斷層面的巖體在采動條件下的力學性態;運用突變理論建立了采動斷層活化的突變模型。分享友人