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low-angle fault
相关语句
  缓倾角断层
     Study on the stability against sliding for dam block on low-angle fault in Yunfeng dam
     云峰大坝缓倾角断层坝段抗滑稳定分析
短句来源
     There is a long low-angle fault extending in the dam foundation from BL 51 to BL53 in Yunfeng dam, and it is unfavorable for stability against sliding.
     云峰大坝50号~53号坝段基础存在缓倾角断层,对抗滑稳定不利。
短句来源
  低角度断层
     The low-angle fault not only serves as one of the most important ore-bearing structures but also plays an important role in controlling the geochemical interface of mineralization.
     NE向低角度断层不仅是重要的含矿构造,而且在成矿过程中起着控制成矿物理化学界面的作用。
短句来源
  “low-angle fault”译为未确定词的双语例句
     The main sliding plane is of a low-angle fault with a west trend and 10°~15° dip angle. The strata around the main sliding plane were overlaid unconformably by Lishan Formationand Ezhai Formation (Mesozoic).
     主滑面为向西倾斜、倾角10°~15°的低角度缓断层,四周被中生代梨山组及鹅宅组不整合覆盖。
短句来源
  相似匹配句对
     Low and N.
     Low和N .
短句来源
     and for T-N and T-P are quite low.
     对T-N和T-P的去除效果较差。
短句来源
     low cost;
     生产成本低;
短句来源
     Low-votagize of ZNR
     ZnO压敏陶瓷的低压化
短句来源
     angle.
     角。
短句来源
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  low-angle fault
The low-angle fault with additional source, possibly a submarine slump, is the most likely source of the 1998 tsunami, although other possibilities cannot be excluded.
      
Relocated aftershock distribution and observed coastal subsidence were preferable for the low-angle fault, but the low-angle fault alone could not reproduce the large near-field tsunamis.
      
In our Barbados example we were able to establish the presence of a widespread 80-160 m thick low-velocity zone at and above the main low-angle fault.
      
This evolution in the Westernmost Tethys seems to be related to areas out of the limit of significant crustal extension in the hanging wall block of the main cortical low-angle fault of the rifting.
      
Along a low-angle fault marked by thin slices of red-green phyllites, tectonic slices of the Lycian nappes overlay garnet-micaschists of the massif.
      
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On the basis of spatial and temporal characteristics of vertical deformation in the study area as shown by data obtained from repeated levelling,dynamic state of recent tectonic movement is described in this paper.It is suggested that a N-S slip of the block was accommodated along the low angle fault before and after the Tangshan earthquake.Moreover,in view of changes in deformation following the shock in point the stress accumalation might be on the front of the slipping block,suggesting an increase in...

On the basis of spatial and temporal characteristics of vertical deformation in the study area as shown by data obtained from repeated levelling,dynamic state of recent tectonic movement is described in this paper.It is suggested that a N-S slip of the block was accommodated along the low angle fault before and after the Tangshan earthquake.Moreover,in view of changes in deformation following the shock in point the stress accumalation might be on the front of the slipping block,suggesting an increase in tectonic stresses in the southern part of the North China plain.It is concluded that historically seismic zones and those in the process of being deformed,which have NW-treniding structures acting as a barrier to shocks can regarded as seismically potential regions.

本文根据文安、霸县地区(简称文霸区)历年水准复测资料所反映的垂直形变时、空分布特征,对该区现今构造的动态进行了初步分析。认为该区在唐山地震前后,地块沿缓倾断裂生了由北向南的滑动。同时,根据震后形变大势的改变,滑块前端可能存在着应力积累。这预示着华北平原南部构造应力的加强。在这一过程中,老震区和起阻隔作用的北西向构造区可视为地震发生的潜在地区。

During the 1∶50000 regional geological survey, the decollement structures werediscovered in the west limb of the Qiguanchang anticline from Yankeng, Youxi County. Itsmain structure feature is that the strata of Qixia Formation, Tongziyan Formation andCuipingshan Formation (Permian period ) were slipped upon the metamorphic rocks ofDongyan Formation and Longbeixi Formation (Middle-Upper Proterozoic).The main sliding plane is of a low-angle fault with a west trend and 10°~15° dip angle.The strata around...

During the 1∶50000 regional geological survey, the decollement structures werediscovered in the west limb of the Qiguanchang anticline from Yankeng, Youxi County. Itsmain structure feature is that the strata of Qixia Formation, Tongziyan Formation andCuipingshan Formation (Permian period ) were slipped upon the metamorphic rocks ofDongyan Formation and Longbeixi Formation (Middle-Upper Proterozoic).The main sliding plane is of a low-angle fault with a west trend and 10°~15° dip angle.The strata around the main sliding plane were overlaid unconformably by Lishan Formationand Ezhai Formation (Mesozoic). The decollement structures show an east-west slidedirection and an unidentified displacement. It is inferred that they were formed in IndosinianMovement. The discovery of the Yankeng decollement structures is of importance to theevaluation of the coal deposits and prospecting other mineral deposits in the area.

福建尤溪砚坑滑脱构造是在1∶5万区域地质调查中发现的。它位于七官场背斜西翼,其主要构造特征是二叠纪栖霞组、童子岩组、翠屏山组地层滑移到中—晚元古代东岩组及龙北溪组变质岩之上。主滑面为向西倾斜、倾角10°~15°的低角度缓断层,四周被中生代梨山组及鹅宅组不整合覆盖。滑动方向由东向西,滑距不明,属印支期构造运动形成的滑脱构造。砚坑滑脱构造的发现,对该区煤矿的评价及指导普查其它矿床具有重要意义。

The ore-controlling structure in Xiaoban gold deposit is a low-angle fault-detachment faultof north-western of Puyang metamorphic core complex, developing on the metamorphic structure. It is characterized by the flat occurrence, stable extension and frequent dissection to theschistosity of metamorphic rocks. It is a ductile-brittle compreso-shear deformation belt with itsupper side moving towards the western. The fault rocks in the lower-angle fault are mainlyphyllonite and tectoncaschist....

The ore-controlling structure in Xiaoban gold deposit is a low-angle fault-detachment faultof north-western of Puyang metamorphic core complex, developing on the metamorphic structure. It is characterized by the flat occurrence, stable extension and frequent dissection to theschistosity of metamorphic rocks. It is a ductile-brittle compreso-shear deformation belt with itsupper side moving towards the western. The fault rocks in the lower-angle fault are mainlyphyllonite and tectoncaschist. The low-angle fault is the important impounding structure, whichcontrols over shape, occurrence, scale and distribution of the gold ore-body, and the dynamicpropelty of the compresso-shear constrains the mineralization alteration type. The ore-controlling structure also plays an important rule of geochemical interface in the gold mineralization.

肖板金矿床控矿构造是在变质岩构造基础上发育起来的蒲洋变质核杂岩构造之北西侧的剥离构造-低角度正断层系,具有产状平缓、延伸稳定、明显穿切变质岩片理等特征,为以压扭性为主的韧脆性变形,上盘向北西运动,构造岩以千枚岩或构造片岩为主。低角度断层是重要的储矿构造,其控制了矿体的形态、产状、规模和分布,其压扭性力学性质决定了交代为主的矿化蚀变类型,而且在成矿过程中也起到地球化学界面作用。

 
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