基于液化SPT基准值的液化势估计     

符圣聪  江静贝 《世界地震工程》2010,26(4)

基于神经网络BP模型和可靠度理论,并沿用抗震规范中液化标准贯入锤击数基准值概念,建立了简化的液化判别概率方法。文中以液化标准贯入锤击数作为估计液化势的基本依据。该基准值是给定地面加速度、土层埋深、地下水位的液化临界锤数,也与震级大小和液化概率有关。为了对不同震级和土层中任一点进行液化判别,引入土层埋深水位以及震级大小对基准值的修正系数。为了方便工程应用,也给出了按地震分组的液化判别方法。  相似文献   

长输油气管道地震监测预警的应用与技术     

刘建平  付立武  郝建斌  詹美萍 《世界地震工程》2010,26(2)

在最近40年的管道工业中,地震灾害导致了大量管道破坏事故.长输管道地震监测预警的目的不是震前预报,而是震后紧急速报,为管道震后决策和紧急救援提供依据.介绍了地震监测预警系统在阿拉斯加管道、冀宁管道、东京煤气公司等管道上的典型应用,对地震监测预警的硬件和软件技术手段进行了分析.硬件手段有地震动参数监测、断层位移监测、管道泄漏监测以及数据传输;软件手段包括地震动参数处理、自动报警,以及灾情评估与管道维修咨询.  相似文献   

内蒙古金厂沟梁地区晚三叠世脉岩地球化学特征及成岩动力学背景   总被引：2，自引：1，他引：1  

付乐兵  魏俊浩  魏启荣  谭俊  李艳军  李闫华  王明志  蒋永建 《地球科学》2010,35(6):933-946

金厂沟梁位于张家口-赤峰-朝阳金矿集区东端, 区内发育大量规模不等的脉岩, 岩性以闪长岩、闪长玢岩为主.对其进行了锆石U-Pb年龄、主微量元素及Sr-Nd同位素分析.脉岩锆石LA-ICP-MS U-Pb年龄值可分为三组: 2 458~2 524 Ma、253±6 Ma(MSWD=3.0)及228±1 Ma(MSWD=0.26).2.5 Ga锆石反映成岩过程中有古老地壳物质参与, 253 Ma锆石可能与古亚洲洋闭合时的岩浆事件有关, 228 Ma则为脉岩的形成年龄.脉岩SiO₂(51.22%~68.48%)、MgO(1.35%~8.13%)含量变化较大, 且具有高Na₂O+K₂O、Al₂O₃及低的TiO₂、P₂O₅含量等特征.岩石LREE及LILE富集, HFSE亏损.脉岩(87Sr/86Sr)_i比值较为一致(0.704 95~0.705 92), 而ε_Nd(t)(-0.2~-9.5)及T_2DM(1.02~1.77 Ga)值变化范围较大.主微量元素及同位素研究结果表明: 部分熔融的岩石圈地幔熔体底侵到壳幔边界, 诱发古老地壳物质的部分熔融, 随后发生的幔源熔体与壳源熔体的混合是脉岩最可能的源区过程.主微量元素构造判别图解指示岩石形成于陆弧向板内演化的构造环境; 结合区域上同时代脉岩群、碱性岩带及A2型花岗岩的侵位, 认为晚三叠世华北板块北缘已完成与蒙古弧地体的碰撞并进入造山后伸展阶段.   相似文献   

TRANSVERSE STRUCTURES FEATURES OF DIFFERENT DEPTHS DERIVED FROM BOUGUER GRAVITY ANOMALIES IN THE SOUTHERN SEGMENT OF TAN-LU FAULT ZONE          下载免费PDF全文

WANG Xin  ZHANG Jing-fa  JIANG Wen-liang  JIANG Hong-bo  TIAN Tian  GAO Min  FU Ping-jie 《地震地质》2016,38(2):370-385

To research the faults distribution and deep structures in the southern segment of Tan-Lu fault zone(TLFZ) and its adjacent area, this paper collects the Bouguer gravity data and makes separation by the multi-scale wavelet analysis method to analyze the crustal transverse structure of different depths. Meanwhile Moho interface is inversed by Parker variable density model. Research indicates that the southern segment of TLFZ behaves as a NNE-directed large-scale regional field gravity gradient zone, which separates the west North China-Dabie orogen block and the east Yangtze block, cutting the whole crust and lithosphere mantle. There are quite differences of density structures and tectonic features between both sides of this gradient belt. The sedimentary and upper crustal density structure is complex. The two east branches of TLFZ behave as linear gravity anomalous belt throughout the region, whereas the two west branches of TLFZ continue to extend after truncating the EW-trending gravity anomaly body. The lower crustal density structure is relatively simple. TLFZ behaves as a broad and gentle low abnormal belt, which reflects the Cretaceous-Paleogene extension environment caused graben structure. The two west branches of TLFZ, running through Hefei city, extend southward along the west margin of Feidong depression and pinch out in Shucheng area due to the high density trap occlusions in the south of Shucheng. The Feizhong Fault, Liu'an-Hefei Fault, and Feixi-Hanbaidu Fault intersect the two west branch faults of TLFZ without extending to the east. Recent epicenters are mainly located in conversion zones between the high-density and the low-density anomaly, especially in TLFZ and the junction of the faults, where earthquakes frequently occurred in the upper and middle crust. As strong earthquakes rarely occur in the southern segment of TLFZ, considering its deep feature of abrupt change of the Moho and intersections with many EW-trending faults, the hazard of strong earthquake cannot be ignored.  相似文献   

先天性支气管闭锁的MSCT表现          下载免费PDF全文

吴德红  陈少波  龚晓虹  刘超  付传明 《CT理论与应用研究》2016,25(1):85-93

目的:分析先天性支气管闭锁的多层螺旋CT(MSCT)表现,以提高该病的诊断水平。方法:回顾性分析15例先天性支气管闭锁患者MSCT表现;全部病例采用GE公司螺旋CT(Lightspeed 64)行胸部扫描,原始图像传送至AW 4.4工作站进行图像后处理重组,观察病变的特点并结合文献复习。结果:全部病例显示支气管黏液栓的改变,发生在左肺6例,右肺9例;13例显示黏液栓周围有肺气肿;2例无肺气肿,11例粘液栓伴行肺动脉分支变细,所在的肺叶血管细小,分支减少,分布稀疏。结论:MSCT对先天性支气管气闭锁具有较高的诊断价值,能显示先天性支气管闭锁的黏液栓和周围肺气肿的典型征象,后处理多平面重组(MPR)图像及最大密度投影(MIP)可任意角度观察黏液栓的形态、位置及其与邻近支气管、肺血管的关系。结合薄层重建图像观察可提示支气管闭锁部位。   相似文献   

湖南保靖X区页岩气储层“甜点”区地震资料非线性反演预测方法          下载免费PDF全文

梁国华  黄捍东  刘福义  符超  林中月  王向浩  杨亚迪  苗雨新  沈金松  张晓晨 《CT理论与应用研究》2016,25(3):299-310

针对湖南保靖地区地表覆盖层复杂、地下高陡构造多变、地震勘探资料信噪比低,以及页岩气储层与周围泥岩层波阻抗对比度小等特点,研究敏感测井曲线重构与优化处理、地震资料相控非线性反演和叠后地震属性流体检测的综合储层评价方法。通过对多条测线的地震资料反演和流体检测并与实钻井结果对比,获得了良好的地质效果,初步验证了所研究方法的有效性和实用性。   相似文献   

COSEISMIC SURFACE RUPTURES AND SEISMOGENIC MUJI FAULT OF THE 25 NOVEMBER 2016 ARKETAO M_W6.6 EARTHQUAKE IN NORTHERN PAMIR          下载免费PDF全文

CHEN Jie  LI Tao  SUN Jian-bao  FANG Li-hua  YAO Yuan  Li Yue-hua  WANG Hao-ran  FU Bo 《地震地质》2016,38(4):1160-1174

The M_W6.6 Arketao earthquake,which occurred at 14:24:30 UTC 25 November 2016 was the largest earthquake to strike the sparsely inhabited Muji Basin of the Kongur extension system in the eastern Pamir since the M 7 1895 Tashkurgan earthquake.The preliminary field work,sentinel-1A radar interferometry,and relocated hypocenters of earthquake sequences show that the earthquake consists of at least two sub-events and ruptured at least 77km long of the active Muji dextral-slip fault,and the rupture from this right-lateral earthquake propagated mostly unilaterally to the east and up-dip.Tectonic surface rupture with dextral slip of up to 20cm was observed on two tens-meter long segments near the CENC epicenter and 32.6km to the east along the Muji Fault,the later was along a previously existing strand of the Holocene Muji fault scarps.Focal mechanisms are consistent with right-lateral motion along a plane striking 107°,dipping 76° to the south,with a rake of 174°.This plane is compatible with the observed tectonic surface rupture.More than 388 aftershocks were detected and located using a double-difference technique.The mainshock is relocated at the Muji Fault with a depth of 9.3km.The relocated hypocenters of the 2016 Arketao earthquake sequence showed a more than 85km long,less than 8km wide,and 5~13km deep,NWW trending streak of seismicity to the south of the Muji Fault.The focal mechanism and mapping of the surface rupture helped to document the south-dipping fault plane of the mainshock.The listric Muji Fault is outlined by the well-resolved south-dipping streak of seismicity.The 2016 Arketao M_W6.6 and 2015 Murghob M_W7.2 earthquakes highlight the importance role of strike-slip faulting in accommodating both east-west extensional and north-south compressional forces in the Pamir interior,and demonstrate that the present-day stress and deformation patterns in the northern Pamir plateau are dominant by east-west extension in the shallow upper crust.  相似文献   

青海日月山断裂德州段断错地貌的高分辨率遥感影像解译     

黄帅堂  田勤俭  李智敏李文巧  付国超  殷翔 《地震》2016,36(3):87-98

青海日月山断裂带是青藏高原东北缘柴达木—祁连活动地块内部的一条NNW走向的右旋走滑兼逆冲断裂。 本文基于ENVI 5.1遥感图像处理平台对研究区高分一号多光谱(分辨率8 m)和全色(分辨率2 m)影像进行融合, 获取了高保真、 高分辨率的卫星遥感影像。 通过多尺度、 多角度、 多层次的构造解译以及对比, 将日月山西支断裂的海晏段划分为德州段(F_1-3)和海晏段(F_1-4)两个次级段, 同时利用高分辨率Google Earth影像对德州段断错微地貌进行了解译、 分析, 结合对德州段野外地质考察, 进一步验证了影像解译结果。 研究表明: 日月山断裂的德州段由5条次级段落组成(f₁, f₂, f₃, f₄, f₅), 并且该段断裂晚更新世以来活动性明显, 以右旋走滑为主兼有逆倾滑分量; 断裂在晚更新世以来发生过多期断层活动, 其中全新世断层活动可划分为两期, 最新一期水平位错量为6.5~8.7 m, 第二期水平位错量为12.3~14 m; 晚更新世也可划分出两期活动, 第一期水平位错量为16~20 m, 第二期水平位错量为28.5~47 m。  相似文献   

大庆长垣西缘断裂浅部构造特征     

邓小娟  赵斌  石金虎  酆少英  秦晶晶 《震灾防御技术》2016,11(2):218-229

大庆石油物探资料结果表明,大庆长垣西缘断裂的上盘,即东侧的北西向断裂可能存在第四纪活动断裂。为了确定大庆长垣西缘断裂的空间展布以及该区的地壳浅部地质构造特征,本项研究布设了2条跨大庆长垣西缘断裂的浅层地震探测剖面。结果表明,大庆长垣西缘断裂表现为走向北东、倾向南东的逆断层,为一条中生代晚期活动断裂。断裂的上盘,即东侧发育有一系列次级断裂,断裂的断层性质以及断层倾向多样化,两条测线东部均发育错断第四纪地层的断层,使得该区浅部地层形成地堑与地垒构造。本项研究不仅可进一步提高对大庆长垣地区浅部构造特征的认识,而且为大庆市地震危险性评价提供依据。  相似文献   

隧道开挖对下伏水平薄煤层采空区地层的扰动及衬砌受荷特征     

符亚鹏  姚志刚  方勇  陈先国 《岩土力学》2016,37(Z1):117-125

为探明下伏薄煤层采空区地层中隧道施工对地层的扰动以及衬砌结构受荷特性,采用离散元颗粒流软件,从细观角度对隧道开挖引起的地层应力变化特性进行了模拟分析,同时在室内开展模型试验量测了下伏煤层采空区地层隧道衬砌背后土压力以及二次衬砌结构内力（轴力、弯矩）,分析了特定围压下间距对土压力和二次衬砌受力的影响。结果表明,下伏煤层采空区地层因隧道开挖引起的围岩松动区呈“O”形分布,隧道下伏围岩颗粒接触力反而小于隧道上覆围岩;洞周允许位移越大,颗粒接触力链间断区域越大;间距越小,颗粒接触力链间断区域越大,当间距大于2.0D（D为隧道跨度）时,下伏采空区对隧道围岩颗粒接触力影响逐渐消失,降低了地基反力,间距越小,降低程度越高;二次衬砌内力分布有一定的离散性,二次衬砌裂缝最先出现在拱底,是隧道主体结构的薄弱环节。  相似文献