The method of design for seismic data database system based on tree structure     

王喜珍  滕云田  高孟潭  陈步云  姜慧 《地震学报(英文版)》2005,18(1):99-105

Introduction In recent years, with the development of earthquake observation technology, increasing ofobservation stations and improvement of observation instruments which are digitalized and con-nected by network, a great deal of data is recorded, to some extend, which brings difficulty for usto manage and store them. It leads to traditional methods, which use the file system to managemass data, could not satisfy our requirement, and it is necessary to find a new method in place oftradit…  相似文献   

Near-surface seismic anisotropy, attenuation and dispersion in the aftershock region of the 1999 Chi-Chi earthquake   总被引：1，自引：0，他引：1  

Yunfeng Liu  Ta-Liang Teng  Yehuda Ben-Zion 《Geophysical Journal International》2005,160(2):695-706

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Deep Mechanical Background for the Cenozoic Volcanism in the Tibetan Plateau   总被引：1，自引：0，他引：1  

Xiong Xiong* Institute of Geodesy  Geophysics  Chinese Academy of Sciences  Wuhan  China  Institute of Geology  Geophysics  Chinese Academy of Sciences  Beijing  China Wang Jiye Institute of Geodesy  Geophysics  Chinese Academy of Sciences  Wuhan  China  Graduate School  Chinese Academy of Sciences  Beijing  China Teng Jiwen Institute of Geology  Geophysics  Chinese Academy of Sciences  Beijing  China 《中国地质大学学报(英文版)》2005,16(4)

INTRODUCTION Volcanoesaremostlyobservedinoceanicridges,hotspotsandcontinentalriftzones(Hongetal.,2003),andarerarelyobservedincontinentalinteri ors.However,sincethevolcanoeswithintheconti nentinteriorscannotbeattributedtotheplate/block marginprocess,theydr…  相似文献   

Estimation of lateral force acting on piles to stabilize landslides     

Yi He  Hemanta Hazarika  Noriyuki Yasufuku  Jidong Teng  Zhenbo Jiang  Zheng Han 《Natural Hazards》2015,79(3):1981-2003

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Geophysical constraints on mesozoic disruption of North China Craton by underplating‐triggered lower‐crust flow of the Archaean lithosphere     

Zhongjie Zhang  Yanghua Wang  Yangfan Deng  Lin Chen  Jing Wu  Jiwen Teng  Yun Chen  Weiming Fan  Giuliano Panza 《地学学报》2013,25(3):245-251

The mechanism of the disruption, both lithospheric thinning and oceanization of the commonly accepted long‐term‐stable Archaean craton, is still an open question. The available models, all imply a bottom to top process. With the construction of a 1660‐km‐long transect across the eastern North China Craton (NCC), we demonstrate that both the P‐wave velocity and density in the lowermost crust beneath the central section are significantly higher than in the corresponding parts of the south and north sections on the transect. These features are interpreted as geophysical signature of lower crustal underplating, which supplies sufficiently high gravitational potential energy to trigger lateral flow of the lower crust. This magma underplating‐triggered bilateral lower crust flow may facilitate the lithospheric thinning by means of asthenosphere upwelling and decompression melting, which infill the gap produced by the lower crust flow. The underplating‐triggered lower crustal flow can provide an alternative mechanism to explain the NCC lithosphere disruption, which highlights the crustal feedback to Archaean lithosphere disruption, from top to bottom.  相似文献   

湖南宝山矿床花岗岩类硫-铅同位素和流体包裹体研究及其成因意义   总被引：2，自引：0，他引：2  

丁腾  马东升  陆建军  章荣清  谢银财 《矿床地质》2016,35(4):663-676

宝山铜铅锌多金属矿床是湖南重要的铅锌生产基地。矿床内矽卡岩型铜(钼)矿化受侏罗纪花岗闪长斑岩的控制,而主要的铅锌矿体则产于远离岩体的碳酸盐地层中,且缺乏可靠的矿化年龄限制。为了查明宝山铅锌矿体与花岗闪长斑岩之间的成因关系,文章对宝山花岗岩类中浸染状黄铁矿的硫同位素和钾长石的铅同位素,以及铅锌矿石萤石脉石的流体包裹体进行了测试和研究,并与前人报道的铅锌硫化物矿石的硫、铅同位素进行了对比,尝试为宝山铅锌矿化的物质来源及成因提供依据。研究表明,花岗闪长斑岩中浸染状黄铁矿的δ34S值为+1.5‰~+3.5‰,与铅锌矿石硫化物(方铅矿、闪锌矿及黄铁矿)相一致;同时,花岗岩类中钾长石的铅同位素组成206Pb/204Pb、207Pb/204Pb和208Pb/204Pb分别为18.4789~18.7668、15.6835~15.7220和38.7903~39.1035,具有壳源的特征,且与铅锌矿石硫化物的铅同位素分布范围相吻合。宝山矿床的硫、铅同位素特征表明,花岗闪长斑岩应是铅锌矿化的主要硫源及金属来源。宝山矿床铅锌矿石萤石中的流体包裹体具有低温(130~150℃)、低盐度(8%)的特征,可能是岩浆热液演化到晚期的产物。结合已有的有关资料加以对比和分析,研究认为,宝山铅锌矿床的成矿物质应来源于花岗闪长岩的岩浆期后热液,在热液演化晚期迁移到远端地层中沉淀,形成了宝山的主要铅锌矿体。  相似文献   

内蒙古敖汉旗七家金矿闪长玢岩锆石U-Pb年代学、地球化学及地质意义          下载免费PDF全文

王一珅  刘建明  刘红涛  褚少雄  高帅  陈永安  许腾  武宗林  高玉友 《地质科学》2016,(2):633-653

内蒙古敖汉旗七家金矿构造位置上处于兴蒙造山带与华北克拉通北缘的结合部位, 靠近兴蒙造山带一侧, 是近年来新发现的石英脉型金矿床.区内岩脉以闪长玢岩为主, 且与石英脉型矿体空间关系密切.根据岩脉与矿体的穿插关系, 将其分为成矿前闪长玢岩和成矿后闪长玢岩.LA-ICP-MS锆石U-Pb年代学表明, 成矿前闪长玢岩加权平均年龄为166.3±3.4 Ma, 成矿后闪长玢岩加权平均年龄为128.6±4.5 Ma, 与区域上两期构造-岩浆活动时间(分别为160 Ma左右和128 Ma左右)近似吻合.主量元素特征显示: 二者均属于准铝质, 高钾钙碱性系列; 微量元素特征显示: 二者均富集轻稀土元素、大离子亲石元素(Rb、K)和活泼的不相容元素(U、Pb), 相对亏损重稀土元素和高场强元素(Nb、Ta、Ti), 反映出岩浆来源具壳源特征.主微量元素特征均显示出二者具有岛弧岩浆岩的地球化学属性.另外, 成矿后闪长玢岩有较高的Nb/Ta(18.66~20.27)和Zr/Hf(37.16~39.23)比值, 暗示其岩浆来源具明显的幔源特征.岩石地球化学特征表明, 成矿前闪长玢岩可能起源于太平洋板块俯冲导致的下地壳部分熔融岩浆; 成矿后闪长玢岩可能起源于俯冲流体交代的地幔楔熔融岩浆, 并在其演化侵位过程中伴有地壳物质的混染.结合闪长玢岩成岩时代、岩石成因及区域构造演化, 反映出七家金矿的形成与太平洋板块的西向俯冲密切相关, 矿床在地壳由挤压增厚向伸展减薄的转换过程中形成.  相似文献   

近年我国十大重要金属矿种找矿重大进展与成果   总被引：1，自引：0，他引：1  

陕亮  张万益  姚晓峰  马腾  刘江涛  贾德龙  王尧  张鑫刚 《地质论评》2016,62(S1):151-153

近年我国重要矿产资源勘查成果不断快速涌现。为服务矿产勘查进展长期动态跟踪与成果集成研究,2010~2014年,笔者依托原中国地质调查局发展研究中心承担的《重点成矿区带矿产勘查跟踪与成果集成》、《全国地质勘查进展分析》等项目,以铁、铜、铝、铅锌、金、钨、锡、钼、镍、锰等十大重要金属矿产勘查进展为主要研究对象,研究分析了勘查成果特征。  相似文献   

Identifying geospatial services across heterogeneous taxonomies     

Hao Li  Ling Bian  Teng Wang 《国际地球制图》2016,31(10):1058-1077

Geospatial services with different functions are assembled together to solve complex problems. Different taxonomies are developed to categorize these services into classes. As differences in granularity and semantics exist among these taxonomies, the identification of services across different taxonomies has become a challenge. In this paper, an approach to identify geospatial services across heterogeneous taxonomies is proposed. Using formal concept analysis, existing heterogeneous taxonomies are decomposed into semantic factors and their various combinations. With these semantic factors, a super taxonomy is established to integrate the original heterogeneous taxonomies. Finally, with the super taxonomy as a cross-referencing system, geospatial services with classes in original taxonomies are identifiable across taxonomies. Experiments in service registries and a social media-based spatial-temporal analysis project are presented to illustrate the effectiveness of this approach.  相似文献   

高阶边界元方法求解规则波在三维局部渗透海床上的传播     

章旭  勾莹  倪云林  滕斌  刘珍 《海洋学报》2016,38(1):133-142

基于线性势流理论,利用高阶边界元法研究了规则波在三维局部渗透海床上的传播。根据Darcy渗透定律推导出渗透海床的控制方程,利用渗透海床顶部和海底处法向速度和压强连续条件得到渗透海床顶部满足的边界条件。根据绕射理论,利用满足自由水面条件的格林函数建立了求解渗透海床绕射势的边界积分方程,采用高阶边界元方法求解边界积分方程进而得到自由水面的绕射势和波浪在局部渗透海床上传播过程中幅值的变化情况。通过与已发表的波浪对圆柱形暗礁的时域全绕射结果对比,证明了本文建立的频域方法计算波幅的正确性和有效性。利用这一模型研究了三维矩形渗透海床区域上波浪的传播特性,并分析了入射波波长、海床渗透特性系数等参数对波浪传播的影响。  相似文献