Tectonic relation between northeastern China and the Korean peninsula revealed by interpretation of GRACE satellite gravity data   总被引：2，自引：0，他引：2  

Sungchan Choi  Chang-Whan Oh  Herrmann Luehr 《Gondwana Research》2006,9(1-2):62

The major continental blocks in northeastern Asia are the North China block and the South China block, which have collided starting from the Korean peninsula. Geologic and geophysical interpretations reveal a well defined suture zone in northeastern China from Qinling through Dabie to Jiaodong. The discovery of high-pressure metamorphic rocks in the Hongseong area of the Korean peninsula, prominent evidence for the collision zone, indicates extension of the collision zone in northeastern China into the Korean peninsula. Interpretation of the GRACE satellite gravity dataset shows two prominent structural boundaries in the Yellow Sea. One extends from the Jiaodong Belt in eastern China to the Imjingang Belt in the Korean peninsula. The other extends from near Nanjing, eastern China, to Hongseong. Tectonic movement in or near the suture zone may be responsible for seismic activity in the western Korean peninsula and the development of the Yellow Sea sedimentary basin.  相似文献   

用ArcIMS建立震源机制解数据发布系统方法浅析     

王津  邵兆刚  雷伟志 《地球学报》2006,27(4):379-384

随着WebGIS(网络地理信息系统)应用的不断深入,我们将WebGIS技术引入到震源机制解数据分析,通过将数据库信息与地理空间属性信息相结合,实现了数据库信息图形化,统计分析自动化,数据访问和查询网络化。本文通过介绍用ArcI MS3.1建立震源机制解数据发布系统,论述了ArcI MS体系结构,详述了中国及邻区地震震源机制解数据发布系统的总体结构和用ArcI MS建立震源机制解数据发布系统的方法,并就系统开发中的技术要点进行了论述。  相似文献   

位场自动反演技术的研究现状及意义   总被引：4，自引：0，他引：4  

张季生 《地球学报》2006,27(6):609-612

本文首先叙述了重、磁异常自动反演技术的特点。与传统的定性分析重、磁场分布特征的方法不同,重、磁异常自动反演方法通过反演得到地下场源分布,即地下密度或磁性的分布特征。由于密度体或磁性体与地质体的关系更为直接,因此这种新一代重、磁解释成果及图件将成为人们从新的角度来认识地质构造的基础材料。文中不但阐述了该方法的研究现状,同时也说明了存在的问题。  相似文献   

Seismic activity associated with the subducting motion of the Philippine Sea plate beneath the Kanto district, Japan   总被引：1，自引：1，他引：1  

Sadaki Hori 《Tectonophysics》2006,417(1-2):85

The Pacific plate and the Philippine Sea plate overlap and subduct underneath the Kanto region, central Japan, causing complex seismic activities in the upper mantle. In this research, we used a map selection tool with a graphic display to create a data set for earthquakes caused by the subducting motion of the Philippine Sea plate that are easily determined. As a result, we determined that there are at least four earthquake groups present in the upper mantle above the Pacific plate. Major seismic activity (Group 1) has been observed throughout the Kanto region and is considered to originate in the uppermost part of mantle in the subducted Philippine Sea plate, judging from the formation of the focal region and comparison with the 3D structure of seismic velocity. The focal mechanism of these earthquakes is characterized by the down-dip compression. A second earthquake layer characterized by down-dip extension (Group 2), below the earthquakes in this group, is also noted. The focal region for those earthquakes is considered to be located at the lower part of the slab mantle, and the Pacific plate located directly below is considered to influence the activity. Earthquakes located at the shallowest part (Group 3) form a few clusters distributed directly above the Group 1 focal region. Judging from the characteristics of later phases in these earthquakes and comparing against the 3D structure of seismic velocity, the focal regions for the earthquakes are considered to be located near the upper surface of the slab. Another earthquake group (Group 4) originates further below Group 2; it is difficult to consider these earthquakes within a single slab. The seismic activities representing the upper area of the Philippine Sea plate are Group 3. This paper proposes a slab geometry model that is substantially different from conventional models by strictly differentiating the groups.  相似文献   

Earthquake generation in Cyprus revealed by the evolving stress field     

Eleftheria E. Papadimitriou  Vassilios G. Karakostas   《Tectonophysics》2006,423(1-4):61

Strong earthquake occurrence (M ≥ 6.0) onshore and offshore the Cyprus Island constitutes significant seismic hazard because they occur close to populated areas. Seismicity is weak south of the Island along the Cyprean Arc and strong events are aligned along the Paphos transform fault and Larnaka thrust fault zone that were already known and the Lemessos thrust fault zone that defined in the present study. By combining the past history of strong (M ≥ 6.0) events and the long-term tectonic loading on these major fault zones, the evolution of the stress field from 1896 until the present is derived. Although uncertainties exist in the location, magnitude and fault geometries of the early earthquakes included in our stress evolutionary model, the resulting stress field provides an explanation of later earthquake triggering. It was evidenced that the locations of all the strong events were preceded by a static stress change that encouraged failure. The current state of the evolved stress field may provide evidence for the future seismic hazard. Areas of positive static stress changes were identified in the southwestern offshore area that can be considered as possible sites of future seismic activity.  相似文献   

农用地分等成果在土地利用总体规划中的应用   总被引：9，自引：1，他引：9  

杨建波  王国强  王莉  胡纪鹏 《地域研究与开发》2006,25(6):118-121

不同层次的农用地分等成果有着不同的应用方向。文章以土地利用总体规划为导向，以农用地利用等别与自然等别的高低延伸顺序与耕地最低需求量相结合，确定出基本农田保护的数量；以基本农田数量的105％～110％为基准，将县级利用等别图与自然等别图重叠的区域划定为基本农田保护区；交叉运用分等的土壤肥力图、气候生产潜力指数曲线图来选择作物适宜生长区和改良土地用养结构；以分等因素图作为限制因子的选择标准来划分土地限制类别区。  相似文献   

Mineralogy, geochemistry, and Nd isotope composition of the Rainbow hydrothermal field, Mid-Atlantic Ridge   总被引：3，自引：0，他引：3  

A. F. A. Marques  F. Barriga  V. Chavagnac  Y. Fouquet 《Mineralium Deposita》2006,41(1):52-67

Petrological, geochemical, and Nd isotopic analyses have been carried out on rock samples from the Rainbow vent field to assess the evolution of the hydrothermal system. The Rainbow vent field is an ultramafic-hosted hydrothermal system located on the Mid-Atlantic Ridge characterized by vigorous high-temperature venting (∼365°C) and unique chemical composition of fluids: high chlorinity, low pH and very high Fe, and rare earth element (REE) contents (Douville et al., Chemical Geology 184:37–48, 2002). Serpentinization has occurred under a low-temperature (<270°C) retrograde regime, later overprinted by a higher temperature sulfide mineralization event. Retrograde serpentinization reactions alone cannot reproduce the reported heat and specific chemical features of Rainbow hydrothermal fluids. The following units were identified within the deposit: (1) nonmineralized serpentinite, (2) mineralized serpentinite—stockwork, (3) steatite, (4) semimassive sulfides, and (5) massive sulfides, which include Cu-rich massive sulfides (up to 28wt% Cu) and Zn-rich massive sulfide chimneys (up to 5wt% Zn). Sulfide mineralization has produced significant changes in the sulfide-bearing rocks including enrichment in transition metals (Cu, Zn, Fe, and Co) and light REE, increase in the Co/Ni ratios comparable to those of mafic Cu-rich volcanic-hosted massive sulfide deposits and different ¹⁴³Nd/¹⁴⁴Nd isotope ratios. Vent fluid chemistry data are indicative of acidic, reducing, and high temperature conditions at the subseafloor reaction zone where fluids undergo phase separation most likely under subcritical conditions (boiling). An explanation for the high chlorinity is not straightforward unless mixing with high salinity brine or direct contribution from a magmatic Cl-rich aqueous fluid is considered. This study adds new data, which, combined with the current knowledge of the Rainbow vent field, brings compelling evidence for the presence, at depth, of a magmatic body, most likely gabbroic, which provides heat and metals to the system. Co/Ni ratios proved to be good tools used to discriminate between rock units, degree of sulfide mineralization, and positioning within the hydrothermal system. Deeper units have Co/Ni <1 and subsurface and surface units have Co/Ni >1.  相似文献   

黄河源地区草地退化空间特征   总被引：54，自引：4，他引：54  

张镱锂  刘林山  摆万奇  沈振西  阎建忠  丁明军  李双成  郑度 《地理学报》2006,61(1):3-14

利用黄河源地区1985年和2000年1：100000土地利用／覆被数据，结合1：250000DEM、道路和居民点数据与野外调查资料，分析草地退化与坡向、海拔及距道路和居民点距离之间的关系．探讨黄河源区15年间土地覆被变化特征与规律。结果表明，退化草地占源区总面积的8．24％，冬春季牧场退化率显著高于夏季牧场：草地退化是黄河源区研究时段内土地利用／覆被变化最主要的特征。草地退化表现为：①阳坡退化率高于阴坡；②受人口密度影响，草地退化率与海拔高度成反比，相关系数为．0．925；③距离居民点越近。退化率越高。尤其当与居民点距离≤12km时，草地退化率与其相关系数高达-0．996；④在距道路4km以内．草地退化率与道路距离成反比．相关系数高达-0．978。1985年以来，源区的草地退化有自然因素的影响．但人类活动的影响仍起主导作用。科学地减少当地居民对草地的过分依赖是解决脆弱的江河源区环境退化的根本。  相似文献   

GIS应用项目可行性研究初探   总被引：1，自引：0，他引：1  

孔云峰 《地理与地理信息科学》2006,22(1):35-39

总结GIS应用项目可行性研究的基本理念、主要内容和工作步骤,认为全面的GIS项目可行性研究是在战略层次上分析组织环境,在战术层次上全面评估技术、财务、组织与实施方面的可行性,并撰写研究报告、论证报告建议。技术可行性分析包括产品的成熟程度评估、系统集成方案复杂程度评估和招聘技术人员的难易程度评估;财务可行性分析是识别项目成本和收益的类别和细目、估算成本并预期收益、计算财务指标;组织与实施可行性分析是组织对组织变革的适应性、接受程度做出判断。建议采用案例研究的方法,总结国内可行性研究的经验与教训,编制更实用的研究指南。  相似文献   

旅游影响调适系统研究   总被引：2，自引：0，他引：2  

肖佑兴 《地理与地理信息科学》2006,22(5):81-85

旅游发展对目的地产生各种影响,如何调适旅游影响对目的地非常重要。该文从系统论的角度探讨旅游影响调适问题,分析旅游影响的形成机制,认为旅游影响是旅游影响动力因子模块、旅游影响应力因子模块及旅游影响规范因子模块在旅游影响场的作用下形成的。在此基础上探讨旅游影响调适机理及调适流程,指出旅游影响调适是旅游调适主体通过旅游制度创新系统对旅游利益相关者发生作用而进行的。根据调适机理和调适流程,建立旅游影响调适库,认为旅游影响调适的4个分目标(减量、扩容、治理和适应)通过旅游制度创新系统及其派生措施来实现。  相似文献