構造變質作用 的英文怎麼說

中文拼音 [gòuzàobiànzhízuòyòng]
構造變質作用 英文
tectonic metamorphism
  • : Ⅰ動詞1 (構造; 組合) construct; form; compose 2 (結成) fabricate; make up 3 (建造; 架屋) bui...
  • : Ⅰ動詞1 (做; 製作) make; build; create; produce 2 (假編) cook up; fabricate; concoct 3 [書面語...
  • : Ⅰ名詞1 (性質; 本質) nature; character; essence 2 (質量) quality 3 (物質) matter; substance;...
  • : Ⅰ動詞1 (使用) use; employ; apply 2 (多用於否定: 需要) need 3 (敬辭: 吃; 喝) eat; drink Ⅱ名...
  • 構造 : structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constituti...
  1. Based on the studies of petrotexture, structural deformation and the relevant metamorphism, this paper indicates that this peridotite massif is the product of ultramafic magma cumulated at the crust - mantle transtion zone and has undergone the early stage of plastic deformation under the condition of granulite facies ( 800 ) and late ductile shearing at amphibolite and greenschist facies in relevance to uplifting

    本文通過巖體的結形及相應的研究,提出了該橄欖巖體是由超基性巖漿在殼幔過渡帶結晶而成,並經歷了與圍巖一致的麻粒巖相( 800 )條件下的早期塑性形以及角閃巖相和綠片巖相退化條件下與逆沖上升有關的韌性剪切形。
  2. Stability of rock slopes is generally controlled by the structure of rock masses, especially the soft structure surfaces. analysis of rock mass structures is a key to establish geological models and numerical simulation and a foundation to assess the stability of rock slopes. the weak structure surfaces are mainly bedding planes, faults, joints, schistosity plane and contact zones of intrusive bodies. since they are different in genesis and scale, the rock masses are different in features and mechanical intensities. based on the combination of rock structure bodies, 15 basic modes of deformation and failure of rock slope are systematically summarized. the deformation and failure of rock masses actually result from the recombination and rearrangement of these rock bodies. there are 11 types of rock mass structures and various deformation and failure of bank slopes are present in the reservoir area of the three gorge project

    巖體結,特別是軟弱結面對基巖斜坡形與破壞具有顯著的控製,巖體結模式分析是建立斜坡地模型和數學模型的關鍵和評價斜坡穩定性的基礎。巖層層面斷裂節理裂隙片理與劈理以及侵入體和圍巖的接觸帶等是控制基巖斜坡穩定的軟弱結面,這些成因不同大小不一的結面將巖體分割成性各異力學強度不均的各種巖體結體,成了15種基巖斜坡形破壞的巖體結基本模式。不同結體的重新組合與排列是斜坡失穩的內在原因。
  3. And the rock mass as the main object of most engineering practice is developed by all kinds of geotechnical action and force in the long geology history to the complex characteristic of continuous medium, crannied medium and granular medium, to the anisotropic and heterogeneous entity with elasticity, plasticity, viscidity, creepocity and rheology

    為主要工程對象的巖體是在漫長的地歷史發展過程中經受各種地營力而形成的成因和復雜,巖性多樣且包含了連續介,裂隙介和散體介特徵的,兼有彈性、塑性、粘性、流性的各向異性的非均體。
  4. The movement and deformation of the crust are the comprehensive effects of various kinds of the geodynamical processes on the ground, and the systematical response of the crustal medium to the plate tectonic and deeply dynamic evolution. therefore, the research for them becomes one of important contents in the geodynamic studies

    地殼的運動和形是各種地球動力學過程在地表的綜合顯現,是地殼介對板塊和深部動力過程的綜合響應,因此,對地殼運動和形的研究成了地球動力學研究的重要內容之一。
  5. The two wings tectonics and metamorphism in tai ping - shan syncline were studied by the method of comparison, and it has been proved that the intrusion of fang shan magmatic rock was the sources of various geological effects, all different typical geological phenomena are the results of magmatic rock intrusion, and the nearer distance the area to the fang shan magmatic rock, the stronger effect it has

    本文通過比較分析的方法,對太平山向斜南北兩翼形和進行了研究,提出了「房山巖體」的侵入是本區各種地的主要動力來源,區內各種典型的地現象是巖體侵入的結果,離巖體越近影響程度越大,遠離巖體逐漸減弱。
  6. After making detailed research on ore - controlling factors, the author points out that gold deposits in fujian resulted from the various geologic processes such as sedimentation, metamorphism, tectonism and magmatism

    詳細研究了福建省金礦的金礦的控礦因素,提出省內金礦的形成是沉積和巖漿(包括火山)的綜合結果。
  7. Synthetically analyzed the fracture, earthquake, coal ranks and their distribution, coal seam ' s buried depth and so on, the authors have realised that low - rank bituminites, early - middle jurassic in tianshan area, are formed by burial metamorphism, and it is widespread

    摘要通過對天山地區的斷裂、地震、地熱、煤級及其時空分佈、煤層埋深等因素的綜合分析,認為天山北緣及其鄰區早中侏羅世大范圍分佈的低級煙煤主要由深成形成,深成具普遍性。
  8. Main content in simulation is the spatio - temporal evolution of the set of descriptive variables characterizing tectonic mineralization state under coupling of various processes as following : ( 1 ) variables related to forming and property of ore - forming fluid, such as dissolution rate of minerals ( include metal minerals ) in rock, concentration and saturation of aqueous species in fluid, temperature, pressure, and ionic strength etc. ; ( 2 ) variables related to structural deformation and fluid flow, such as stress, deformation rate, fracture network, porosity, fracture permeability ; ( 3 ) variables related to precipitation and mineralization, such as nucleation rate of gangue and metal minerals, accumulation precipitation of various minerals, etc. ; ( 4 ) spatio - temporal coupling relation of various variables above, such as the coupling relationship between spatio - temporal evolution of fracture permeability and flow and focus of fluid and ore - forming

    模擬的主要內容是在各種過程耦合下,以下描述成礦體系的主要量的時空演化:與成礦流體的形成和性有關的量,如地層中礦物(包括成礦物)的溶解速率、流體中各組分的濃度與飽和度、流體溫度、壓力、離子強度等;與形和流體運移有關的各量,如應力與形速率、巖石孔隙度、(斷裂)滲透率等;與沉澱成礦有關的量,如礦物(金屬礦物和脈石礦物)的成核速率、各礦物的沉澱量等;上述各有關量間的時空耦合關系,如斷裂滲透率時空演化與流體流動、匯聚和成礦的耦合關系等。
  9. The control of the deep - seated structural - magmatic process over the metallogenic system around the middle - lower yangtze river reaches is shown as : ( 1 ) the mantle uplift belt is closely related to the general geological background of the metallogenic system ; ( 2 ) the primitive magma originated from different parts of the mantle uplift belt ( mantle ridge or mantle slope ) shows differences in style of formation and composition and results in different magmatic series and metallogenic subzones, respectively ; ( 3 ) the varying depths of structural - magmatic chambers may form a " three - layered structure " ( central type, network - like and ring - like ) and this is the primary factor that controls the different magmatic series and the concerned cluster of ore deposits ; ( 4 ) the alkaline basaltic magma derived from the mantle ridge forms high - potassium and calcium alkaline magma and shoshonitic magma due to its altering intensity of afc process with the lower crustal material, which has something to do with the copper - gold and iron - sulphur metallogenic subsystems, respectively

    深部巖漿對長江中下游成礦帶安徽沿江地區成礦系統的控製表現為: ( 1 )地幔隆起帶與成礦系統的總體地背景的演密切相關; ( 2 )源於地幔隆起帶不同部位(幔脊與幔坡)的原始巖漿,其生成方式和物組成不盡相同,它們分別產生相應的不同巖漿巖系列和成礦亞帶; ( 3 )不同深度的巖漿房組成中心式網格式環帶式「三層結」 ,是控制區內不同巖漿巖系列及有關礦床集中分佈的主要因素; ( 4 )源於地幔隆起帶脊部的堿性玄武巖漿,由於與下地殼物發生的afc強度不同,形成了高鉀鈣堿性巖漿和橄欖安粗巖漿,分別與銅、金成礦亞系統和鐵、硫成礦亞系統有關。
  10. During the process of studying tectonic origin of gold - bearing breccia bodies in the shuangwang gold deposit, shanxi province, the author apply several modern tectonics theories, such as hydrofracturing, fluid dynamic breccia, tectonic pumping, deformation partitioning, embryonic fracture etc. the paper presents an kind of new model for the formation of hydrofracturing breccia - type metallotectonic, which is one of fracture - vein - breccia series metallotectonics concerning fluid, by deformation partitioning, embryonic fracture, hydrofracturing and rupture - healing

    本文所探討的陜西雙王含金角礫巖體的成因研究運了水力壓裂、流體動力角礫巖、流體泵吸形分解和雛形斷裂理論等幾個現代理論,提出了形分解?雛形斷裂?水力壓裂?裂開愈合四位一體的水壓角礫巖型咸礦模型,是與流體動力有關的裂隙?脈?角礫巖系成礦的一種新的模式。
  11. Lithosphere delamination is an important way for compositional and structural evolution of collisional orogens. geotectonic research, geophysical survey and geochemical analysis have revealed that the lithosphere of east qinling - dabie mountains had delaminated intensively in mesozoic. however, the extensive mesozoic metamorphism and magmatism have been weakly related to lithosphere delamination

    研究地球物理探測和地球化學分析等都已揭示東秦嶺-大別山帶曾在中生代發生巖石圈拆沉,但有關中生代和巖漿活動與巖石圈拆沉的內在聯系研究卻較為薄弱。
  12. Using the theories of probability, algebra and number theory comprehensively, we investigate a class of boolean functions with three - valued walsh spectrum in the first part of this dissertation : the properties of the extended semi - bent functions, which are constructed from any two bent functions, are studied, followed by the structure characteristics of the boolean functions satisfying propagation criterion with respect to all but two vectors ; the definition and cryptographic properties of k - order quasi - bent functions are proposed whose walsh spectrum takes on only three values. some sufficient and necessary conditions are offered to decide whether a boolean function is a k - order quasi - bent function ; a special method is presented to construct the k - order quasi - bent functions, whose cryptographic properties are explored by the matrix method, which is different from the method of walsh spectrum and that of autocorrelation of boolean functions ; the application of this kind of boolean functions in the fields of stream cipher, communications and block ciphers is discussed, which shows the great importance of the fc - order quasi - bent functions ; some methodology are proposed to construct the k - order quasi - bent functions, including the complete construction by using the characteristic matrices of boolean functions, and the recursive method by two known k - order quasi - bent functions we further extend our investigation to the ring zp, where p is a prime, and the similar results are presented as far as the p - valued quasi - generalized - bent functions are considered

    本文首先綜合運概率論、代數學、數論等基礎學科的理論知識,並以頻譜理論為主要研究工具,對一類譜值分佈相對均勻的函數? ?廣半bent函數、 k階擬bent函數和p值k階擬廣義bent函數進行了系統、深入的研究,給出了廣半bent函數定義,並探討了廣半bent函數的密碼學性;給出了k階擬bent函數和p值k階擬廣義bent函數的定義及等價判別條件;討論了k階擬bent函數和p值k階擬廣義bent函數與部分bent函數和p值廣義部分bent函數的關系,探討了它們的密碼學性;給出了k階擬bent函數和p值k階擬廣義bent函數的典型方法,並將對k階擬bent函數的密碼性的研究轉化到對一類特殊的矩陣的研究上;利布爾函數的特徵矩陣原則上給出了k階擬bent函數的一種完全方法,還給出了從已有的p值k階擬廣義bent函數出發,遞歸元個數更多的p值k階擬廣義bent函數的方法;初步探討了k階擬bent函數在序列密碼、分組密碼以及通信中的應;給出了一類布爾函數walsh譜的分解式,並利這類布爾函數的walsh譜分解式給出了一類近似穩定的布爾函數的,特殊情形下為k階擬bent函數;利代數數論的知識考察了p值k階擬廣義bent函數的譜特徵,並給出了k階擬廣義bent函數與所有仿射函數的符合率特徵等等。
  13. Studies on the metamorphism and ptt path of the granulites now become to be one of the most important methods to module a structural evolvement pattern of erogenic belts

    研究高壓麻粒巖的和ptt軌跡已成為建立山帶演化模式的最重要途徑之一。
  14. Eng. ) this course systematically introduces the material of the earth, varied geological processes and their causing, and evolution history of the earth

    本科目有系統的介紹地球的組成物、地球上所發生的各種不同地、各類地及其成因,以及地球演的歷史。
  15. Based on the wholly, dynamics and integrated principle, the guide of petroleum geology and computer technology, the research has been done as follows by the factors of geology, gravity, magnetism and electricity : ( 1 ) building chronostratic framework of wangjiang - qianshan and its neighbor, divide and compare carbonic and permain sequence. ( 2 ) studying distribution of sediment series in different period. ( 3 ) studying the basic tectonic transform style, preliminarily dividing main tectonic units. ( 4 ) describing the formation and evolution of basin

    本文以整體、動態、綜合分析為原則,以石油地理論為指導,以計算機技術為手段,利地面地、重力、磁力、電法所獲得的各項參數,進行了以下研究工:建立望江?潛山盆地及鄰區的年代地層格架,並對石炭、二疊系地層進行層序劃分與對比;研究不同時期沉積體系的展布特徵;研究盆地的基本形樣式,初步劃分盆地的主要單元;描述盆地的形成演化過程;在上述研究基礎上劃分推測的含油氣系統。
  16. Then, media parameters of the crust, boundary function forces of the area and the finite elementary analyses model were reversibly simulated. linking up with the plateau crustal deformation back analyses model, the tectonic deformation was also simulated

    該模型屬于動力學的物理模型,包含反演地殼的介參數、反演研究區域的邊界力與正分析三大部分組成,並以此模型為基礎模擬模擬了高原的形。
  17. Based on the regional geologic survey on the scale of 1 / 250 000, coupled with geological, geochemical and geophysical investigations in some key regions, this dissertation summarized the tectonomagmatic evolution and mineralization of the mid - gangdise area. with respect to tectonic evolution, the gangdise belt has experienced a multi - stage evolutional history since mesozoic, including oceanic crust subduction, arc - continent collision, intracontinental subduction and collision, and strike - slip and block uplift

    論文以新一輪1 : 25萬區域地調查為基礎,在對關鍵區段重點解剖的基礎上,結合地球物理、巖石化學、地球化學、沉積演化和成礦的研究成果,對岡底斯中段的巖漿演化與成礦了較系統的科學總結。
  18. The style of deformation in different rock mass and tectonic units is varied. according to the distinction of stratigraphic assemblage, rock type. tectonic block type and the characteristics of deformation, the whole district can be subdivided into three structure belt. namely southern and northern metamorphic fold stratigraphic system and central tectonic mixed system and multi - stage intruded magmatites

    根據區內出露的地層、巖性、塊體、特徵,全區可分為南北兩帶的褶皺地層系統和中帶的混雜系統以及不同期次的巖漿侵入體。
  19. 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參數,並反分析了簡化后的高原地殼的邊界力,從宏觀上分析了青藏高原的運動特徵,分析結論認為:青藏高原的形以南北擠壓為主,東西擴張為輔;成高原現今格局的主要原因是印度洋板塊和歐亞板塊的持續碰撞。
  20. The stratums containing mine, tectonic - hydro thermally process, magma activity, alteration react to district mineralization in degrees. the belt of granite facies, the inside and outside contact belt of rock body, the joining belt of tectonic - hydro thermally superimposed, the stratum belt of unconformity contact are the main enrichment belt

    含礦地層及礦源層、-熱液、巖漿活動、都在不同程度上對區域成礦起,而花崗巖相化帶、巖體內外接觸帶、?熱液疊加交匯帶、地層不整合接觸帶則為金礦化主要富集帶。
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