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断层系统
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  fault system
    The dominant strik direction of fault system in the lower sequence is NE 30° ̄40°,and the upper one is NE 70° ̄80°.
    下部断层系统的走向优势方位为北东30°~40°,按倾向分为同向正断层和反向正断层两组; 上部断层系统的走向优势方位为北东70°~80°。
短句来源
    PEEL FAULT SYSTEM OF DONGXIANG COPPER DEPOSIT AND ITS ORE CONTROLLING SIGNIFICANCE
    东乡铜矿剥离断层系统及其控矿意义
短句来源
    The equilibrium equation of surrounding rock mining fault system is established. The fault destablizing process with shear failure pattern belongs to fold catastrophe model.
    建立了矿井围岩 -断层系统的准静态形变平衡方程 ,将呈剪切破裂形式的断层失稳过程归结为折迭突变模型。
短句来源
    The main Lithology and ore controlling fracture system of Dongxiang Copper deposit belongs to peel fault system and the main orebodies occur in fracture zones of peel fault system where sharp dip tend to be gently.
    东乡铜矿床主要控岩控矿断裂系统属于剥离断层系统 ,主要矿体赋存于剥离断层系统各断裂破碎带由陡变缓处 ;
短句来源
    It is found, by using box-counting method, that the fault system conforms to the power-law distribution on the scale from 5 km to 75 km in the central and western Hainan gold metallogenic province , the fractal dimension of the faults is 1.70. The whole area is divided into nine subblocks according to the difference of the metallogenic systems;
    利用数盒子法对海南岛中西部金矿集中区断层分布统计表明 :断层系统在 5~ 75km尺度内符合分形分布 ,其分维值为 1 .70。
短句来源
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  “断层系统”译为未确定词的双语例句
    The crust extension and rifting occurring in the late post-collisional stage (>18 Ma) formed a series of NS-striking normal faults and associated rifting basins (≤13.5 Ma) across the Tibetan plateau.
    晚期阶段主要发生地壳伸展与裂陷(<18Ma):垂直碰撞带的EW向伸展,形成一系列横切青藏高原的NS向正断层系统(≤13·5Ma)及其围陷的裂谷系和裂陷盆地。
短句来源
    ORE - CONTROLLING EFFECTS OF DETACHMENT FAULT IN THE QINGGANGPING GOLD FIELD
    青岗坪金矿区拆离断层系统的控矿作用
短句来源
    ORE-CONTROLLING EFFECT OF DETACHMENT FAULT IN THE ZHANGJIAHE GOLD FIELD
    张家河金矿区拆离断层系统的控矿作用
短句来源
    The ore-controlling factors are summarized as uplift of basin margin, denudational fault at margin of thermal uplift,nappe of interface of different strata and multiphase deep-seated fault.
    该区金矿控矿条件为盆地边缘隆起带控矿、热隆起周边剥离断层系统控矿、不同岩性界面的推覆构造控矿和多期活动的深大断裂控矿
短句来源
    The ore-controlling factors are attributed into rise on the margin of basin, detach faults around the thermal rise, nappe structure on the interface of different lithology, shear structure and multi-phased deep faults.
    该区金矿控矿条件为盆地边缘隆起带控矿、热隆起周边剥离断层系统控矿、不同岩性界面的推覆构造及剪切构造控矿和多期活动的深大断裂控矿
短句来源
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  fault system
The Yanshan orogenic belt fault system deflected from an EW to a NE direction, then to a NNE direction during the Indo-Chinese epoch-Yanshanian epoch.
      
The thrust-nappe strength of the Qinling-Dabie orogenic belt fault system showed the tendency that the strength was greater in the south and east, but weaker in the north and west.
      
This fault system faulted in the east and folded in the west from the Indo-Chinese epoch to the early Yanshanian epoch.
      
The Tanlu fault system caused the basin to migrate from west to east and south to north.
      
The migration regularity of the East China Sea shelf basin-Okinawa trough fault system shows that the formation age became younger in the west.
      
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Wangxia gliding nappe structure was formed with the forcing intrusion of Bawan-glin superunit granite in western Hainan. Its gliding nappe system,which was composed by C-P structure layer,developed gliding tectonics such as synclinorium,bedding rhed fold,penetrative stretching and flow cleavage,etc.,The autochthon was O-S structure layer. Wangxia gliding nappe structure was formed in the middle and late period of Indosinia;All gliding nappe system was in extension state in early period,and in pressure state...

Wangxia gliding nappe structure was formed with the forcing intrusion of Bawan-glin superunit granite in western Hainan. Its gliding nappe system,which was composed by C-P structure layer,developed gliding tectonics such as synclinorium,bedding rhed fold,penetrative stretching and flow cleavage,etc.,The autochthon was O-S structure layer. Wangxia gliding nappe structure was formed in the middle and late period of Indosinia;All gliding nappe system was in extension state in early period,and in pressure state in later period. The gliding nappe di-rection of the gliding tectonics was N-S and had been displaced Southward for about 7 km.Strong gold mineralization had occurred in Wangxia and Yalao faults which were in the system of detachment faults.

琼西王下滑覆构造是由坝王岭超单元花岗岩的强力侵位而形成的。滑覆系统由C-P构造层组成,发育有复式向斜、顺层掩卧褶皱、透入性拉伸线理和流劈理等滑动构造;原地系统为O-S构造层。王下滑覆构造形成于印支中、晚期。在早期滑覆系统处于伸展状态,晚期则处于挤压状态,滑覆构造的滑覆方向为N→S,滑覆距离大于7km。在滑脱断层系统内的王下断层及牙劳断层中,均发生了较强的金矿化。

mploying the fractal and renormalizational group theories,the essay has established fractal percolation inodels of the rift system umder complex geological conditions,The computation of the fractal dimensions of the actual fault systems reveals that faults are closely related to the connection and per-colation between developed rifts,which may solve some difficult problems in exploring and opening up newoil-gas fields.

运用分形与重正化群理论,建立了复杂地质条件下裂缝系统的分形渗流模型.计算了实际断层系统的分维后揭示了断层与裂缝发育带以及储集空间的连通性与渗流性的密切联系.解决了勘探开发中的某些疑难问题.

The Late Yanshanian extensional environment gave rise to detachments,including peel thrusts, at various tectonic levels on both sides of the deep faultbelt or rift belt. F_(15) peel thrust (system) at the southern side of the Xinjiangrift belt is a dominant ore-controlling factor of deposit No. 50. It is beleived tocontroll the source of ore substances and their precipitation and siting of theorebodies. Besides, the paper also discusses the significance of peel thrusts inmineral prospecting.

燕山晚期的拉张构造环境,在深断裂带或裂陷带两侧形成了各种不同层次的拆离滑脱,包括剥离断层。信江裂陷带南侧的F_(15)剥离断层(系统)控制了50矿床的矿质来源、矿质沉淀及矿体定位。该断层是控矿的主导因素。文中还讨论了剥离断层的找矿意义。

 
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