Structural pattern of eastern Himalayan syntaxis in Namjagbarwa and its formation process   总被引：20，自引：4，他引：16  

ZHANG Jinjiang  Jl Jianqing  ZHONG Dalai  DING Lin & HE Shundong. Department of Geology  Peking University  Beijing  China  . Institute of Geology  Geophysics  Chinese Academy of Sciences  Beijing  China Correspondence should be addressed to Zhang Jinjiang 《中国科学D辑(英文版)》2004,47(2):138-150

The structural pattern of the eastern Himalayan syntaxis in Namjagbarwa consists of two series of structures with different styles. One series compiles the earlier ductile contrac-tional and lateral-slip deformation system, formed by nearly north-south shortening within the syntaxis, left-lateral and right-lateral slipping along its western and eastern boundaries respectively. They were possibly produced by the indentation of the Indian continent into Asian continent after India-Asia collision. The peak deformation-metamorphic ages in these structures are 62-60 Ma, -23 Ma and -13 Ma. The other series is composed of ductile-brittle normal faults distributing concentrically and dipping toward the outsides of Namjagbarwa Peak. They were probably the collapse structures caused by rapid uplift in a later time and the beginning ages for the normal faulting are about 7.3-6.3 Ma.  相似文献   

    

Shen Bing 《中国地理科学(英文版)》2004,14(2):97-103

While China’s economic growth has been impressive since 1978, regional disparity in terms of provincial per capita GDP has been increasing. On the other hand, this rapid but uneven growth was accompanied by China’s deepening openness and structural reforms including the development of non-state-owned enterprises (non-SOEs) and fiscal decentralization. Based on quantitative analyses, this paper tries to explore the features of regional disparity in China and the relationships between regional growth and China’s openness and economic structure reforms in the period from 1981 to 2000. The paper finds that the catching-up of the coastal region to the initially rich provinces, which are mainly located in inland areas, brought about a convergence of the growth pattern across provinces in the 1980s. The subsequent divergence in the provincial growth rates between the coast and the interior generated an enlarging regional disparity in China in the 1990s. The ever-faster growth in the coastal region was benefited by China’s openness and the development of non-state-owned enterprises. The development of non-state-owned enterprises underlies the higher operational efficiency in the coastal region. Additionally, with the insignificant regression results, fiscal decentralization was observed to facilitate faster growth in the coast region. The findings justify the initiative of the "West Region Development Strategy" and offer some policy implications for China. Biography: SHEN Bing (1966–), female, a native of Hebei Province, associate professor, specialized in regional economy and urban development. E-mail: shenbing@mx.cei.gov.cn  相似文献   

Ductility demands on buckling-restrained braced frames under earthquake loading     

Larry?A.?FahnestockEmail author  Richard?Sause  James?M.?Ricles  Le-Wu?Lu 《地震工程与工程振动(英文版)》2003,2(2):255-268

Accurate estimates of ductility demands on buckling-restrained braced frames (BRBFs) are crucial to performance-based design of BRBFs. An analytical study on the seismic behavior of BRBFs has been conducted at the ATLSS Center, Lehigh University to prepare for an upcoming experimental program. The analysis program DRAIN-2DX was used to model a one-bay, four-story prototype BRBF including material and geometric nonlinearities. The bucklingrestrained brace (BRB) model incorporates both isotropic and kinematic hardening. Nonlinear static pushover and timehistory analyses were performed on the prototype BRBF. Performance objectives for the BRBs were defined and uscd to evaluate thc time-history analysis results. Particular emphasis was placed on global ductility demands and ductility demands oa the BRBs. These demands were compared with anticipated ductility capacities. The analysis results, along with results from similar previous studics, are used to evaluate the BRBF design provisions that have been recommended for codification in the United States. Thc results show that BRB maximum ductility demands can be as high as 20 to 25. These demands significantly exceed those anticipated by the BRBF recommended provisions. Results from the static pushover and timehistory analyses are used to demonstrate why the ductility demands exceed those anticipated by the recommended provisions.The BRB qualification testing protocol contained in the BRBF recommended provisions is shown to be inadequate because it requires only a maximum ductility demand of at most 7.5. Modifications to the testing protocol are recommended.  相似文献   

初论造山带古地理学   总被引：21，自引：2，他引：19  

吴根耀 《地层学杂志》2003,27(2):81-98,115

造山带古地理学属构造古地理学 ,是造山带地层学的姐妹学科 ,其核心是活动论构造观。简述了造山带古地理学的形成和内涵 ,重点讨论了地质记录已发生移位、歪曲和混杂的造山带地区 (或经造山作用改造的克拉通地区 )正确地进行构造—古地理重建的三个问题 :一是不能用“将今论古”的方法恢复地史期间的隆起区和堆积区 ,地史期间的物源区并非一成不变 ,要充分认识物源供应的多样性和多重性 ;二是沉积相带的展布受区域构造应力场及基底构造格局控制 ,要特别重视边缘相及其物源区的研究 ;三是辨析原生沉积盆地与构造盆地 ,对盆地进行正确的构造复位是古地理重建的基础。  相似文献   

Subsurface structure under a basaltic monogenetic volcano near the active Atera fault     

T. Tanaka  H. Aoki  A. J. Martin  K. Oshita  K. Nozaki  M. Onishi 《Tectonophysics》2004,378(3-4):197

In this study, we examined the subsurface structure in the vicinity of the active Atera fault beneath at least one monogenetic volcano that forms the Sakashita body of the Ueno basalts, central Japan. Microgravity and seismic reflection surveys over an area of about 3×3 km (horizontal)×1 km (vertical from surface) revealed that (1) a low-density body interpreted as the damaged zone of the Atera fault reaches a depth more than 200 m below sea level; and (2) a weak zone of crust that may exist about 1.5 km southwest of the Atera fault in a direction parallel to it. By combining the shape of the Sakashita body and (2), we propose that a dyke extending in a NW–SE direction with several vent alignments in the same direction may exist along this weak zone. This suggests that the studied area was governed in the NW–SE compressional and NE–SW extensional stress field when the Sakashita body formed.  相似文献   

福建安砂水电站大坝左岸边坡稳定性分析     

郑师春  黄莉菁 《中国地质灾害与防治学报》2004,15(4):40-43

安砂水电站建成以来，大坝左岸边坡仍有掉块现象。文章通过分析原有资料和实地调查，对存在问题的左岸和厂房后边坡，进行地质构造、岩石结构情况研究，综合考虑其构造地貌、坡度、地下水、岩石中缓倾角断层、节理或地层层面相互作用，引入同时考虑地震力E和重力W共同作用下，岩石结构面组合稳定性图解分析等方法，对大坝左岸近坝岸坡进行地震边坡稳定性评价。分析结果认为：大坝左岸岸坡高陡岸坡的上段、中段剖面中的一些结构面及组合面存在下滑及接近下滑的危险。  相似文献   

Where and why do large shallow intraslab earthquakes occur?     

Tetsuzo Seno  Masaki Yoshida 《Physics of the Earth and Planetary Interiors》2004,141(3):183-206

We try to find how often, and in what regions large earthquakes (M≥7.0) occur within the shallow portion (20-60 km depth) of a subducting slab. Searching for events in published individual studies and the Harvard University centroid moment tensor catalogue, we find twenty such events in E. Hokkaido, Kyushu-SW, Japan, S. Mariana, Manila, Sumatra, Vanuatu, N. Chile, C. Peru, El Salvador, Mexico, N. Cascadia and Alaska. Slab stresses revealed from the mechanism solutions of these large intraslab events and nearby smaller events are almost always down-dip tensional. Except for E. Hokkaido, Manila, and Sumatra, the upper plate shows horizontal stress gradient in the arc-perpendicular direction. We infer that shear tractions are operating at the base of the upper plate in this direction to produce the observed gradient and compression in the outer fore-arc, balancing the down-dip tensional stress of the slab. This tectonic situation in the subduction zone might be realized as part of the convection system with some conditions, as shown by previous numerical simulations.  相似文献   

龙川江盆地上第三系芒棒组沉积体系与层序地层分析   总被引：2，自引：1，他引：2  

孙泽轩  姚毅锋  陈勇  李国新 《铀矿地质》2004,20(5):286-293,298

龙川江盆地是造山带内部发育的新生代小型山间断陷盆地。本文结合该盆地晚新世构造、火山活动与沉积作用，对盆地盖层芒棒组沉积体系与层序地层进行了分析。通过分析，建立了龙川江盆地晚新世沉积模式，认为晚新世早期断陷带内快速堆积，主要以发育冲积扇沉积体系为特征，中、晚期冲积扇快速人湖，由此而形成冲积扇一扇三角洲一湖泊沉积体系组合；提出了龙川江盆地芒棒组层序的形成受多期构造活动控制的观点，并建立了3个构造层序，划分了体系域。  相似文献   

甘肃金塔煤田构造分析   总被引：2，自引：0，他引：2  

曹大文 《中国煤田地质》2004,16(5):5-6,11

甘肃金塔及其所在的河西地区均是煤炭资源严重缺乏的地区。区内尽管煤点出露较多，但在深部煤层常常缺失或尖灭，针对这一现象，本文从构造单元划分人手，运用板块构造学的分析方法对本区的构造活动史进行了简明的阐述，断陷盆地成为本区赋煤的主要构造。  相似文献   

福建永定龙川矿区构造特征及其演化过程     

练光春 《中国煤田地质》2004,16(Z1):26-27

介 绍了 龙川 矿 区区 域 构造 地 质 背 景,总 结了 矿 区 构 造特 征 ,探讨 了 研 究 区构 造 的 演 化过 程 ,对龙 川 矿 区 勘探和开发 具有 指导意 义。  相似文献