小波分析在T梁结构损伤识别中的应用研究     

韩西  崔璟  钟厉  狄海波  杨科 《地震工程与工程振动》2011,31(1):101-105

为了提高结构损伤识别的精确度和适用性,将小波分析引入到结构损伤识别中.本文介绍了梁结构在完好状态与损伤状态下振动测试加速度差的理论分析,证明了小波分析加速度差应用于桥梁结构损伤检测的可行性.然后以小波分析为工具,在桥梁结构不同损伤状态下,以移动荷载作用下各节点的加速度时程曲线差为研究对象,来识别结构的损伤状态.并通过试...  相似文献   

《重庆历史地图集·第一卷古地图》设计与研制     

熊明 《测绘科学》2015,(9):149-153

文章介绍了该图集编制的背景及国内编纂情况,阐述了图集需遵循的设计原则和工艺流程,构思了图集每个版块的定位及内容组成。重点对图集在编纂过程中开本设计、结构设计、内容设计、排版和整饰设计等方面进行了剖析,并根据重庆本地历史文化展现的需要,进行了对应的设计。其中的结构编排设计、内容排版设计、图名设计、文字内容结构设计,及版式中使用的中华民族文化元素和重庆本地的文化元素的有机融合等方面,在同类作品中实现了多项创新。最后,分析总结了图集编纂中的问题和解决方法,为后续相关产品的设计与编制提供参考。  相似文献   

Structural Evolution and Hydrocarbon Potential of the Upper Paleozoic Northern Ordos Basin, North China     

YANG Minghui  LI Liang  ZHOU Jin  JIA Huichong  SUN Xiao  GONG Ting  DING Chao 《《地质学报》英文版》2015,89(5):1636-1648

The hydrocarbon potential of the Hangjinqi area in the northern Ordos Basin is not well known, compared to the other areas of the basin, despite its substantial petroleum system.Restoration of a depth-converted seismic profile across the Hangjinqi Fault Zone(HFZ) in the eastern Hangjinqi area shows one compression that created anticlinal structures in the Late Triassic, and two extensions in ~Middle Jurassic and Late Early Cretaceous, which were interrupted by inversions in the Late Jurassic–Early Early Cretaceous and Late Cretaceous, respectively.Hydrocarbon generation at the well locations in the Central Ordos Basin(COB) began in the Late Triassic.Basin modeling of Well Zhao-4 suggests that hydrocarbon generation from the Late Carboniferous–Early Permian coal measures of the northern Shanbei Slope peaked in the Early Cretaceous, predating the inversion in the Late Cretaceous.Most source rocks in the Shanbei Slope passed the main gas-migration phase except for the Hangjinqi area source rocks(Well Jin-48).Hydrocarbons generated from the COB are likely to have migrated northward toward the anticlinal structures and traps along the HFZ because the basin-fill strata are dipping south.Faulting that continued during the extensional phase(Late Early Cretaceous) of the Hangjinqi area probably acted as conduits for the migration of hydrocarbons.Thus, the anticlinal structures and associated traps to the north of the HFZ might have trapped hydrocarbons that were charged from the Late Carboniferous–Early Permian coal measures in the COB since the Middle Jurassic.  相似文献   

甘肃肃北贾公台金矿构造叠加晕特征及深部找矿预测     

蒙轸 《地质与勘探》2015,51(4):731-740

通过对贾公台金矿开展系统的原生晕研究工作,初步建立了矿区原生叠加晕轴向分带(自上而下):W-Mo-Bi-Ni-Co-Cu-Zn-Pb-Ag-Au-Sb-As,认为区内成矿热液具有多期次叠加成矿的特点,深部前缘晕元素异常发育,预示深部找矿前景较好,预测深部盲矿靶位在3200 m标高以下。  相似文献   

甘孜地区雅拉河段地热系统特征及控制因素   总被引：1，自引：0，他引：1  

林正良 《地质与勘探》2015,51(4):764-771

综合应用区域地质、地震、地球化学等资料,对甘孜地区雅拉河段地热系统及其主控因素进行研究。分析认为,甘孜地区地热属于典型的对流型地热系统,雅拉河断裂破碎带及板岩中发育的大量裂隙共同构成了研究区的热储体,这些热储体沿雅拉河断裂带不均匀分布。研究区充沛的大气降水以及季节性的冰雪融水为地热系统提供充足的水源。雅拉河断裂与色拉哈断裂之间大范围相对平坦的区域以及大量储水洼地为地热系统中的水源提供存储空间。该地区地表裂隙发育,利于地表水向下渗透,是地下水的主要补给通道。色拉哈断裂的强烈活动为浅层地下水在重力作用下进一步向深层运移提供重要流体通道。雅拉河断裂带的地势相对低,断裂破碎带是深层流体上涌的重要通道。在流体供给区与出露区的重力势能差以及两条走滑断裂带压力差共同作用下,流体经深部热源加热后在流体通道内形成持续的热流体循环系统。  相似文献   

Water in garnet of garnetite (metarodingite) and eclogite from the Erzgebirge and the Lepontine Alps     

Esther Schmädicke  Jürgen Gose 《Journal of Metamorphic Geology》2020,38(9):905-933

Little is known about water in nominally anhydrous minerals of orogenic garnet peridotite and enclosed metabasic rocks. This study is focused on peridotite-hosted eclogite and garnetite (metarodingite) from the Erzgebirge (EG), Germany, and the Lepontine Alps (LA), Switzerland. Newly discovered, peridotite-hosted eclogite in the Erzgebirge occurs in the same ultra-high pressure (UHP) unit as gneiss-hosted coesite eclogite, from which it is petrologically indistinguishable. Garnet is present in all mafic and ultramafic high pressure (HP) rocks providing for an ideal proxy to compare the H₂O content of the different rock types. Garnet composition is very similar in EG and LA samples and depends on the rock type. Garnet from garnetite, compared to eclogite, contains more CaO (garnetite: 10.5–16.5 wt%; eclogite: 5–11 wt%) and is also characterized by an anomalous REE distribution. In contrast, the infrared (IR) spectra of garnet from both rock types reveal the same OH absorption bands that are also identical to those of previously studied peridotitic garnet from the same locations. Two groups of IR bands, SW I (3,650 ± 10 cm⁻¹) and SW II (3,570–3,630 cm⁻¹) are ascribed to structural hydroxyl (colloquially ‘water’). A third, broad band is present in about half of the analysed garnet domains and related to molecular water (MW) in submicroscopic fluid inclusions. The primary content of structural H₂O, preserved in garnet domains without fluid inclusions (and MW bands), varies systematically—depending on both the location and the rock type. Garnet from EG rocks contains more water compared to LA samples, and garnet from garnetite (EG: 121–241 wt.ppm H₂O; LA: 23–46 wt.ppm) hosts more water than eclogitic garnet (EG: 84 wt.ppm; LA: 4–11 wt.ppm). Higher contents of structural water (SW) are observed in domains with molecular water, in which the SW II band (being not restricted to HP conditions) is simultaneously enhanced. This implies that fluid influx during decompression not only led to fluid inclusions but also favoured the uptake of secondary SW. The results signify that garnet from all EG and LA samples was originally H₂O-undersaturated. Combining the data from eclogite, garnetite and previously studied peridotite, H₂O and CaO are positively correlated, pointing to the same degree of H₂O-undersaturation at peak metamorphism in all rock types. This ubiquitous water-deficiency cannot be reconciled with the derivation of any of these rocks from the lowermost part of the mantle wedge that was in contact with the subducting plate. This agrees with the previously inferred abyssal origin for part of the rocks from the LA (Cima di Gagnone). A similar origin has to be invoked for the Erzgebirge UHP unit. We suggest that all mafic and ultramafic rocks of this unit not only shared the same metamorphic evolution but also a common protolith origin, most probably on the ocean floor. This inference is supported by the presence of peridotite-hosted garnetite, representing metamorphosed rodingite.  相似文献   

浙江省台州-昌化深部构造特征探测     

杨福平  余刚群  侯林锋  孙海青 《大地测量与地球动力学》2019,39(2):142-147

采用高分辨折射和宽角反射/折射综合地震探测方法，在浙江省中部沿黄岩、临海、东阳、桐庐、昌化进行深部构造探测，获得一条长约350 km的速度结构剖面。探测结果表明，地壳结构具有明显的多层性，存在3个速度间断面;基底速度结构图像揭示了速度结构的横向非均匀性，这种不均匀性既对应于地质构造单元的分界线或断裂构造带，也反映出东西部构造特征的差异性。  相似文献   

结构性参数在黄土地基沉降计算中的应用研究          下载免费PDF全文

陶虎  邵生俊  王正泓  张少英  石喜 《地震工程学报》2020,42(6):1604-1608,1631

弦线模量法建立了考虑黄土基本物性指标及附加应力综合影响的弦线模量函数，应用分层总和法计算黄土地基的变形量，并在陕西关中黄土地区工程实践中获得良好的预测结果，而在分析兰州等其他黄土地区地基沉降时，结果出现偏差，究其原因，与计算中忽视了天然状态下黄土的结构性特征有关。以弦线模量法为基础，通过西安近郊4处土样试验和大量载荷试验资料，分析黄土的构度指标与压缩模量、孔隙比、含水量的关系，并将构度指标引入弦线模量表，深化结构性参数在地基沉降变形计算中的理论。  相似文献   

考虑支座摩擦滑移及结构碰撞的非规则人字形桥梁地震响应分析          下载免费PDF全文

闫磊  李青宁  刘芳平  申纪伟  程龙飞  杨茂 《世界地震工程》2018,34(2):044-54

针对非规则人字形桥梁在地震作用下灾变严重的问题，以一座非规则人字形桥梁为研究对象，建立其空间分析模型，研究综合考虑支座摩擦滑移、结构碰撞对非规则人字形桥梁地震响应的影响。结果表明:邻梁间的碰撞作用可使得桥梁墩顶位移及内力相比不考虑时有所减小，但同时也使梁体产生了较大的加速度脉冲效应；当考虑支座摩擦滑移和结构碰撞时，固定墩墩顶位移和邻梁相对位移峰值有一定程度增大，然而对梁体加速度脉冲效应结果影响并无统一规律；纵向地震波作用下，非规则人字形桥梁不仅存在顺桥向的碰撞，横桥向的碰撞响应也不容忽视。非规则人字形桥梁进行抗震设计计算时应选取符合实际情况的计算模型，考虑支座摩擦滑移及结构间的碰撞。  相似文献   

多维多点激励下考虑支座摩擦滑移及结构碰撞的非规则桥梁抗震性能研究          下载免费PDF全文

闫磊  李青宁  岳克锋  李鲁平  付亚男  蓝仕成  喻国根 《世界地震工程》2019,35(2):068-77

以一座典型山区非规则梁桥为研究对象，建立了该桥梁多维多点激励下的多自由度动力计算模型，研究了该桥梁在多维多点激励下考虑支座摩擦滑移及结构碰撞等非线性因素时的抗震性能。研究结果表明:相比一维地震输入，多维地震可使结构的动力响应增加，桥墩底部弯矩需求增大；相比一致激励，多点激励可使得支座的位移需求增大，且地震波最后到达的桥墩上方支座位移最大；同时考虑多点激励和碰撞效应可使桥墩的弯矩需求增加；水平地震作用下，矮墩上部的支座容易滑动，且双向地震较单向地震更明显，三向地震输入较双向有所增强。因此，对山区非规则梁桥进行抗震设计时应有针对性地进行多维多点地震输入计算，找出结构的最大地震需求，以期指导设计。  相似文献