deep fault 中文意思是什麼
deep fault
解釋
深斷裂-
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。 -
The sankeng geothermal field is located on the northeastern side of the wuchuan - sihui deep fault and in the sankeng synclinal karstic basin
摘要廣東三坑地熱田位於吳川四會深大斷裂帶的東北側，三坑向斜巖溶盆地內。 -
Placer abnormal of volcanic lithoclast at longjingjie in kaili of guizhou locates in regional shidongkou deep and major fault nearby, abnormal materials that are obsidian lithoclast and volcanic glass
貴州凱里龍井街火山巖屑重砂異常位於區域性施洞口深大斷裂近旁，異常物質為黑曜巖屑及火山玻璃。 -
But the deep, multiple fault lines that the row is laying bare ? both within the atlantic alliance, and between the alliance and russia ? seem all too reminiscent of cold - war politics at their dismal worst
但是深處的多重裂紋凸露出來? ?不僅在北約內部，而且在北約和俄羅斯之間? ?似乎極度憂郁地（表現出）對冷戰政策的懷念。 -
Near shore sub - aqueous fans, fan delta and delta occurred on the footwall of the hainan marginal fault, whereas turbidity fans developed in the deep water area and the footwall of the hainan no. 2 fault
海南邊界斷層下降盤分別發育近岸水下扇、扇三角洲和三角洲沉積。海南2號斷層下降盤及深水區域濁積扇沉積發育。 -
The basin - formed mechanism, evolution model and petroliferous geological features of compresso - shear basins in the world are analyzed, by which six aspects of the features are summarized as follows : 1 ) in the compresso - shear process, the sedimentary speed of basin is high, forming thicker coarse - grained clastic rocks which normally shape good petroleum reservoir ; 2 ) the source rocks of basin tend to coming from the organic matter - enriched rocks formed in pre - compresso - shear stages, except that in intense compresso - shear process, deep water - semi deep water source rocks are possibly developed in pre - compresso - shear stages, e4xcept that in intense compresso - shear process, deep water - semi deep water source rocks are possibly developed in frontal of deep depression ( fore deep ) of thrust belt ; 3 ) the en echelon folds ( including anticline and fault - nose structure ) are generally as good oil traps ; 4 ) the compresso - shear process is helpful to hydrocarbon accumulation ; 5 ) it may promote the maturity and hydrocarbon - generating process of organic matte, and 6 ) the thrust belts in the surrounding areas of compresso - shear basin are favorable are favorable domains for petroleum concentration
摘要通過對世界上壓扭性盆地的成盆機制、演化模式和油氣地質特點分析，總結壓扭性盆地具有6個方面的石油地質特徵：壓扭作用期間盆地的沉積速率較高，一般形成較厚的粗碎屑沉積，它們常構成很好的油氣儲集層：盆地的烴源巖往住來自於前壓扭期砂成的富含有機質的巖石，但在強烈的壓扭作用期間，在沖斷帶的前緣深坳陷（前淵）中有可能發育深水半深水相的烴源巖；壓扭（張扭）作用期間形成的雁行式褶皺（包括背斜和斷鼻等）往住是很好的油氣圈閉；壓扭作用易於成藏；壓扭作用可以促進有機質的成熟生烴作用；壓扭性盆地的周邊沖斷帶是油氣賦存的有利部位。 -
Within the basin of shangdu, there may occured deep - large fault of long activiation which had affected the basin in its structure, lithofaces of the overlays, dynamic field of undergroud water and the environment of geochemistry
摘要商都盆地發育盆內深大斷裂，其形成時間早、活動時間長，對盆地結構、蓋層巖性巖相、地下水動力場和水文地球化學環境產生影響。 -
The comparison study of the three belts indicates although they are distinct from each other all the three belts show many common features in the aspect of the metallogeny of large - rich vein uranium deposits, i. e : the important metallogenic areas are located above the old crystalline basement ; the paleo - rifting ( taphrogeny ) controls the development of the volcanic belt and at the same time it is favourable metallogenic tectonic environment ; the occurrence of uranium deposit does not depend on the lithology of volcanic rocks ; uranium metallogeny is obviously constrained by deep geologic processes and the connected fault - structural net is the necessary condition for the formation of large - rich uranium deposits
對比研究表明，雖然它們各具特色，就脈型富大鈾礦床成礦作用而言，它們又具有較多的共性：重要成礦區的火山噴發皆奠基在古老的結晶基底上；古裂谷（或裂陷）既控制了火山巖帶的發育，又是有利的成礦構造背景；鈾礦賦存對火山巖的巖性沒有明顯的選擇性；鈾成礦的深部控製作用明顯；聯通的構造網路系統是形成富大鈾礦的必要條件。 -
They good-naturedly cherish a deep conviction that anything which impairs the timing accuracy of seismic results from the fault of the instruments.
他們總是好心地把任何損害地震結果計時準確度的現象怪罪于儀器缺欠。 -
The authors hold that the joint actions of numerous factors such as the upper mantle uplifted zone ( the mantle thinned zone of lithosphere ), the upper mantle anomalous area ( relatively low - velocity area ), the uplifted zone of intracrustal high - conductivity layer, the deep fault ( shear zone of lithosphere ), the margin of the crust - upper mantle uneven masses, the basement uplifted area reflected by gravity high, the magmatic belt and tectonic intersection reflected by skipped magnetic field, control the distribution of auriferous skarn deposits and copper ( associated with gold ) skarn deposits
作者認為，上地幔隆起帶（巖石圈地幔減薄帶） 、上地幔異常區（相對低速區） 、殼內高導層隆起帶、深斷裂（巖石圈剪切帶） 、地殼上地幔不均勻性塊體的邊緣、重力高反映的基底隆起區、跳躍磁場反映的巖漿巖帶和構造交匯處等諸多因素的共同作用控制著含金夕卡巖礦床和銅伴生金夕卡巖礦床的分佈。 -
With the development of electric power, the problem of vibration on turbogenerator shafts stands out. a deep research on vibration mechanism is carried out. and valid method for preventing and diagnosing fault is explored
隨著電力工業的發展，汽輪發電機組振動問題越來越突出，人們對相應的振動機理開展了深入的研究，並積極探尋有效的故障預防和診斷方法。 -
It is therefore proposed in this paper to strengthen the exploration of such wide and deep subsags as chagannuoer and hongqi subsags, to lay emphasis on the exploration of superposed and residual fault depression, and to pay attention to the discovery of various oil and gas reservoirs including metamorphic buried hills, fracture slope breaks, and volcanic rocks, etc
因此，指出下一步應加強類似查干諾爾，紅旗等寬深窪槽的勘探，重視具疊合型和殘留型斷陷的勘探，注重尋找包括變質巖潛山，斷裂坡折帶、火山巖等在內的各類油氣藏。 -
The depositional character of zhuxiang formation in the basin reads as follows : a series of nne alluvial fan were formed along the fault. the half - deep lake to deep lake faces appeared by west side of the fault, towards the west the saucer lake faces, shore deposit and flood plain face appeared in proper order. the depositional center of lower cretaceous was formed in eastern part of the basin, and the depositional depth was pinch - out and thinning out from the east to the west
盆地內下白堊統朱巷組沉積特徵表現為：沿郯廬斷裂帶呈北北東向廣泛發育了沖積扇體系，從近斷裂帶西側出現的半深湖-深湖相，向西依次為濱淺湖相到泛濫平原相的規律性分佈，沉積厚度由東向西尖滅、超覆，構成了明顯的東斷西超的盆地構造格局，表明下白堊統的沉積中心依然位於盆地東部。 -
Through field investigation and analysis indoor, with studying all hydrochemistry data in detail, including macro components and micro components, the author finds out the hydrochemistry feature of ground water. for further specifying the ground water system, with cluster analysis of macro components of surface water and ground water in total 147 samples and the analysis of micro components, including ree, the main ground water systems are distinguished by and large, especially the ground water system main of fault no. 7 and fault no. 15 water bearing belts which have differences at macro and micro components between the two ground water systems, moreover, the main hydrogeochemistry effects are established such as lixiviation, oxidization, precipitation and mixing effect, especially the mixing effect which result in the complexit y of the hydrochemistry of deep bearing tectonic fracture water. based on them, the hydro geological model of upper dam base is established, meanwhile the author summarizes the hydrochemistry feature of weathering crevice water, surface tectonic crevice water and deep tectonic crevice water
為此，本文以大崗山壩區水文地球化學問題為研究對象，通過野外調查和室內分析，詳細的研究了壩區水化學資料，包括宏量組分、微量組分，查明了壩區地下水水化學特徵，對採集的147個地表及地下水樣的宏量組分進行聚類分析，結合微量元素，稀土元素的研究，並應用二氧化硅地熱溫標確定了深部構造裂隙水的熱源深度，基本區分了壩區各個主要地下水水系，特別是以f7 、 f15斷裂含水帶為主的地下水系，它們的宏量組分、微量組分以及稀土等方面均存在差異，以此為基礎，結合壩區水文地質條件，建立了壩區的上壩址的水文地質模型，同時通過分析了壩區花崗巖區的水化學資料，確立了壩區主要的水文地球化學作用，分別為：溶濾作用、氧化作用、沉澱作用、以及混合作用，混合作用是導致深部承壓裂隙水水化學復雜的主要原因，並總結了壩區風化裂隙水、淺部構造裂隙水、深部構造裂隙水的水化學特徵。 -
The paper discusses the deep tectonic setting of yinshan lead - zinc deposit and emphaticly studies geological features of two fault belt and relationships between deep structures and mineralization
本文論述了銀山鉛鋅礦床形成的深部構造背景，著重研究了桐柏?桐城斷裂帶、商城?麻城斷裂帶的地質特徵及其與成礦作用的關系。 -
The nancha suspending - gay bridge of the changjiang road - bridge in jiangshu runyang, with a main span of 1490m, ranks first in china, third in the world. the north rivets, only 250m from the main stream of changjiang, have a tight liaison with the waterpower of it. especially, in this area, the face of rocks undulates a lot and exist fault - fabric. the soil there has apparent difference with the trend of water. the base - hole of north rivets can be named a super - deep one, with a 60m length, 50m widths, and 48m depths. the fence of the base takes advantages of the rectangular underground continuous wall structure and succeeds
江蘇潤揚長江公路大橋南汊懸索橋，主跨1490m ，居中國第一，世界第三。該橋的北錨碇距長江幹流僅250m ，與長江水力聯系密切，錨碇區水文、地質情況復雜，表層淤泥質土及松軟粘土層較厚，基巖頂面起伏較大，且存在斷裂構造，土層具明顯的流變特性。北錨碇基坑為長60m 、寬50m 、深48m的矩形超深基坑，其基礎圍護在國內首次採用矩形地下連續墻結構，並獲得成功。 -
Based on 1 : 100000 high - precision aeromagnetic data, the author holds that huangzhuguan - yushuba fault is not only a second - order synsedimentary fault associated with lixian - mayanhe regional fault in the north, but also a deep fault that cuts the basement
摘要通過對1 : 10萬高精度航磁資料研究，認為黃渚關榆樹壩斷裂不僅僅是其北部禮縣麻沿河區域性斷裂伴生的1條次級同沉積斷層，而是1條切割基底的深大斷裂。 -
Twelve deep and great faults are developed in daqing city and its adjacent areas, they include nenjiang fault, keshan - da ' an fault, fuyu - zhaodong fault and the second songhuajiang fault etc, and they have been active in different degree since early pleistocene
大慶市及鄰區斷裂發育包括嫩江斷裂、克山-大安斷裂、扶余?肇東斷裂、第二松花江斷裂等12條深大斷裂，在早更新世以來均有不同程度的活動。 -
While there is no distict evidence to prove the tanlu fault ' s noted deep and dynamic behavior within the lower crust or even on the upper mantle. thus there still exists a necessary to research and check the understanding about the boundary ' s location and the dynamic background
作為一級構造單元分界線的紅河斷裂、怒江斷裂是超殼斷裂，而昌寧雙江斷裂顯示為低角度鏟式斷層，中下地殼無與之對應的速度異常，可能意味著該斷裂切割不深。 -
In the chapter 2, on the basis of combining the development practice of loan security, the article analyzes the main problems existing along the development of loan security in china : vain security, unsatisfied security, fault security. it also gives deep exposition to the concrete manifestation of these problems and identifies there are much contradiction between the law theory and financial practice. in the chapter 3, through analyzing the problems existing in loan security, the writer thinks what is necessary for china to develop loan security is to change and improve legal protection system for loan security and suggests some solutions to the existing problems : a ) to change and improve the law system
在結合商業銀行貸款擔保的發展實踐的基礎上，分析了目前中國商業銀行貸款擔保發展存在的瑕疵：無效擔保、擔保落空、虛假擔保；深入的論述了這些問題的具體表現；剖析了產生這些問題的法律原因和社會原因，認為就商業銀行貸款擔保法律制度本身來看，無論從法律法規制定的技術水平，還是從法律法規本身反映的金融法律實踐的要求，都不能滿足我們今天的發展要求；而且長期的計劃經濟的金融體制下所形成的制度和觀念與滲透著法治精神的現代金融體制也存在著很多不相包容的地方。
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