地表破裂带，也称为surface rupture zone，是指地震发生时地表出现的破裂带的区域。它通常是地震断裂带的一部分，从而造成地表的位移和变形。这些地表破裂带对于研究地震的震中位置、震级大小和地震构造有着重要意义。以下是一些关于地表破裂带的英语短句和例句： 1. The surface rupture zone extends for miles along the fault line. （地表破裂带沿着断层线延伸数英里。） 2. Scientists are studying the surface rupture zone to understand the mechanics of the earthquake. （科学家们正在研究地表破裂带，以了解地震的机理。） 3. The buildings were damaged due to the surface rupture caused by the earthquake. （建筑物因地震引起的地表破裂而受损。） 4. The surface rupture zone serves as a visible indicator of the energy release during an earthquake. （地表破裂带作为地震能量释放的可见指标。） 这些例句展示了地表破裂带在地震研究和影响评估中的重要性。
地表破裂带,surface rupture zone
1)surface rupture zone地表破裂带
1.From north to south,most of the widths of intensesurface rupture zones are less than 40m,and above 1/2 are between 10～30m.0级地震地表破裂带的实地调查,龙门山断裂带的中央断裂与前山断裂地表破裂带宽度自北向南一般<40m。
2.Based on the latest displacement of Huoshan piedmont fault,Mianshan west-side fault and Taigu fault obtained from the beginning of 1990′s up to the present,the characteristics of distribution and displacement ofsurface rupture zone of the 1303 Hongtong M =8 earthquake,Shanxi Province are synthesized and discussed in the paper.综合 2 0世纪 90年代初在霍山山前断裂和近年在绵山西侧断裂和太谷断裂获取的最新调查资料 ,讨论了 130 3年山西洪洞 8级地震地表破裂带的展布和位移特征 。
3.To know the shallow geological structures under thesurface rupture zone,a high-resolut.此项探测研究以出现在什邡市师古镇附近的疑似地震地表破裂带为切入点,通过采用可控震源以及高精度的浅层地震反射勘探方法,获得了深度15～800m范围内高分辨率的地下结构和构造图像。
英文短句/例句
1.A New Discoved Co-seismic Surface Rupture Zone on Changlingshan Northern Piedmont Fault长岭山北麓断裂上新发现的地震地表破裂带
2.Geometry and kinematics in the east segment of the surface rupture zone occurring during the Kunlun earthquake昆仑山地震地表破裂带东段几何学与运动学
3.DISCOVERY OF SURFACE RUPTURE ZONE ON THE SOUTH OF HELISHAN IN GAOTAI,GANSU PROVINCE甘肃高台合黎山南缘发现地震地表破裂带
4.DEFORMATION STYLES OF THE NORTHERNMOST SURFACE RUPTURE ZONE OF THE M_S 8.0 WENCHUAN EARTHQUAKE汶川M_S 8.0地震地表破裂带北端位置的修订
5.GEOLOGICAL BACKGROUND OF LONGMEN SHAN SEISMIC BELT AND SURFACE RUPTURES IN WENCHUAN EARTHQUAKE龙门山地震带的地质背景与汶川地震的地表破裂
6.TIP STRUCTURES OF THE WESTERN SEGMENT OF SURFACE RUPTURE ZONE OF THE M_S 8.1 WEST OF KUNLUN MOUNTAIN PASS EARTHQUAKE昆仑山口西8.1级地震西破裂带尾端破裂特征
7.Any place within the fault zone could have breakage.断层带内的任何地方都会有破裂。
8.Characteristics of the Surface Rupture of the M_S8.0 Wenchuan Earthquake on the Epicenter,Yingxiu Area汶川地震震中映秀地区地表破裂特征
9.The Surface Rupture of the M_S8.0 Wenchuan Earthquake on the Northern Segment of Central Fault汶川M_S8.0地震中央断裂北段地表破裂特征
10.Characteristics of Ground Ruptures in Beichuan County Caused by the Wenchuan Earthquake汶川地震北川县城地表断层破裂特征
11.BROADBAND SEISMOLOGY AND STUDIES ON THE RUPTURE PROCESS OF INTERMEDIATE AND LARGE EARTHQUAKES宽频带地震学与中强地震破裂过程的研究
12.THE FRACTURE BELT OF GULANG EARTHQUAKE ON MAY, 23 IN 1927 IN GANSU PROVINCE1927年5月23日甘肃古浪8级地震破裂带的发现
13.GEOLOGICAL CHARACTERISTIC OF URANIUM MINERALIZATION IN FRACTURED ZONED OF THE LOWER CAMBRIAN SYSTEM寒武系下统断裂破碎带中的铀矿化地质特征
14.Surface Ruptures Induced by Associated Wenchuan Earthquake in Yingxiu and Hongkou Area汶川大地震中映秀-虹口地区的地表破裂
15.The Survey of Geological Condition and Surface Rupture Characters of Yingxiu Town in the Wenchuan Earthquake汶川地震映秀镇地质条件与地表破裂特征调查
16.The actual cause of the quake itself is the rupturing or breaking of rocks at or below the earth"s surface.地震本身的真正原因是地球表面的或地底下的岩石断裂或破裂。
17.Setback distance determination in reconstruction along the trace of surface rupture caused by M_s8.0 Wenchuan earthquake汶川地震地表破裂周围建筑物重建的避让距离
18.Deformation Features of Surface Rupture of the Wenchuan Earthquake (M8.0) at the Bailu Town汶川8.0级地震地表破裂白鹿镇段的变形特征
相关短句/例句
surface rupture地表破裂带
1.Itssurface rupture occurs on the Beichuan-Yingxiu and the Jiangyou-Guanxian faults,with the lengths of 200km and 70km,respectively.地表破裂带的最大挤压缩短量为3。
2.Besides the huge casualties and property losses, a most complicated yet longest thrust-type co-seismicsurface rupture zone was developed in the quake-hit area.0),地震不仅造成巨大的人员伤亡和财产损失,并形成了迄今为止空间上分布最为复杂、长度最大的逆冲型同震地表破裂带。
3)seismic surface deformation地震地表破裂带
1.Primary study onseismic surface deformation and faulting behavior of Central Fault (Beichuan-Yingxiu Fault) is done by methods such as topographic analysis, field geological investigation, trench excavation, geological profile analysis and so on.目前对其活动速率、活动性、强震复发周期以及震后其地震地表破裂带特征等重要的科学问题上都还没有统一的认识。
4)Shunyi ground rupture zone顺义地表破裂带
5)width of surface rupture地表破裂带宽度
6)surface rupture地表破裂
1.The basic characteristics of near-fault ground motion,including the concentration of near-fault strong ground motions,thesurface rupture and fling-step,the rupture directivity effect,the near fault large velocity pulse and the hanging wall effect,are discussed in this paper.本文对近断层地震动的基本特征作了详细分析,这些基本特征主要包括近断层强地震动的集中性、地表破裂、地面永久变形、破裂的方向性效应、近断层速度大脉冲和上盘效应。
2.Field investigation on thesurface ruptures of the MS8.0地震地表破裂的野外地质调查表明,在这一段内主要存在一条地震地表破裂带,总体沿北川-青川断裂带分布。
3.By laying emphasis on the geomorphic features of thesurface ruptures of the huge earthquake in Longmen Mountains on the eastern margin of Qinghai-Tibet Plateau,this paper confirms the vertical and horizontal offsets of the Yingxiu-Beichuan fault and the Pengxian-Guanxian fault by detailed field geomorphic surveys.作者以地表破裂为切入点,在映秀-北川断裂和彭灌断裂的关键部位,对断错山脊、洪积扇、河流阶地、边坡脊、断层陡坎、河道错断、冲沟侧缘壁位错、小路位错、公路位错、公路拱曲、构造裂缝、断层偏转、擦痕、挤压脊、坡中槽等汶川地震所导致的地表破裂和断裂带开展了详细的野外地貌测量,标定了映秀-北川断裂带和彭灌断裂的垂向断距和水平断距,结果表明汶川地震的地表破裂带沿北东东向延伸,走向介于NE30°~50°之间,倾向北西,倾角介于30°~40°之间。
延伸阅读
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