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中国地震学会地震电磁学专业委员会2013年会暨学术研讨会于2013年8月11日～14日在宁夏回族自治区银川市召开.本次会议由中国地震学会地震电磁学专业委员会主办,宁夏回族自治区地震局协办,中国地震局监测预报司、监测二处以及挂靠单位地震预测研究所对会议的召开提供了大力支持.中国科技大学、云南大学、哈尔滨工业大学、上海大学、防灾科技学院等高等院校,中国地震局直属研究所与中心,部分省(市、自治区)地震局、市县地震局、企业台站、公司等地震相关部门30多个单位60多位专家代表出席了会议. 相似文献
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中国地震学会地震电磁专业委员会 《国际地震动态》2007,(12):37-38
中国地震学会地震电磁学专业委员会于2007年10月15—22日在四川省成都市召开第四届委员会换届暨学术讨论会。本次会议由中国地震学会地震电磁学专业委员会主办,北京鸿基国际旅行社协办,主管部门中国地震局监测预报司和挂靠单位地震预测研究所对会议的筹备和组织工作给予了很大关注,对会议的召开提供了大力支持。四川省地震局王力副局长到会祝贺,监测处杜斌副处长、监测中心杨贤和副主任出席了会议;地震预测研究所科技发展处杨林章处长参加会议,和与会代表一起进行研讨。中国地震局地震预测研究所、地球物理研究所、地壳应力研究所、防灾科技… 相似文献
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由中国地震局分析预报中心主办、广西壮族自治区地震局协办的中国地震学会第二届地震电磁学专业委员会成立大会暨学术交流会 2 0 0 0年 4月 1 7～ 2 1日在广西族自治区北海市召开 .本次会议与会代表 68位 ,列席代表 1 2位 ,有 30多位代表作了专题报告和学术交流报告 .地震学报编辑部刘新美主任应邀参加了本次会议 .地震电磁学专业委员会成立大会由钱家栋主任委员主持 .中国地震局监测预防司代表余书明、专业委员会挂靠单位代表分析预报中心副主任张金祥、东道主广西族自治区地震局局长袁家治以及广西壮族自治区北海市科协主席等同志应邀出席… 相似文献
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福建沿海、台湾海峡GPS观测分析及地球动力学特征研究 总被引：1，自引：1，他引：1
利用 3期GPS联测结果所获得的福建沿海地壳水平运动信息 ,采用ITRF94全球框架为基础的GPS测站地壳运动模型及其处理软件 ,对所获得的观测数据进行处理和精度分析。得到福建省高精度的GPS测站大地坐标、边长及其位移矢量 ,其精度达到 1 7×10 - 8。计算了福建地壳运动速率、主应变率 ,东西与南北向线应变率、面应变率、剪应变率、大地转动率和最大剪应变率等值线并给出了它们的分布图象。根据多年形变和现今GPS观测资料 ,分析福建地壳垂直运动与水平运动 ,显示区域应力场优势分布特征。最后 ,对福建沿海及台湾海峡地壳动力学特征作了初步的探讨 相似文献
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Zhivanovich I. Solov’ev A. A. Efremov V. I. Miller N. O. 《Geomagnetism and Aeronomy》2020,60(7):865-871
Geomagnetism and Aeronomy - Two main features define a sunspot as an object: a strong magnetic field and a low umbra temperature. The same can be said about a facular knot, in the center of which... 相似文献
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Michele Caputo 《Pure and Applied Geophysics》1964,57(1):66-82
Summary Adopting thePizzetti-Somigliana method and using elliptic integrals we have obtained closed formulas for the space gravity field in which one of the equipotential surfaces is a triaxial ellipsoid. The same formulas are also obtained in first approximation of the equatorial flattening avoiding the use of the elliptic integrals. Using data from satellites and Earth gravity data the gravitational and geometric bulge of the Earth's equator are computed. On the basis of these results and on the basis of recent gravity data taken around the equator between the longitudes 50° to 100° E, 155° to 180° E, and 145° to 180° W, we question the advantage of using a triaxial gravity formula and a triaxial ellipsoid in geodesy. Closed formulas for the space field in which a biaxial ellipsoid is an equipotential surface are also derived in polar coordinates and its parameters are specialized to give the international gravity formula values on the international ellipsoid. The possibility to compute the Earth's dimensions from the present Earth gravity data is the discussed and the value ofMG=(3.98603×1020 cm3 sec–2) (M mass of the Earth,G gravitational constant) is computed. The agreement of this value with others computed from the mean distance Earth-Moon is discussed. The Legendre polinomials series expansion of the gravitational potential is also added. In this series the coefficients of the polinomials are closed formulas in terms of the flattening andMG.Publication Number 327, and Istituto di Geodesia e Geofisica of Università di Trieste. 相似文献
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D. Zidarov 《Pure and Applied Geophysics》1973,105(1):655-668
Summary The paleomagnetic field (declination and inclination) in different geological epochs is represented through the field of the so-called magnetic dipole. The optimal dipole coordinates so obtained show that during older geological times the optimal dipole lay outside the earth's centre and moved towards and around the earth centre. It is supposed that the optimal dipole trajectory in the earth coincides with earth core trajectory. This core motion brought about a motion of the masses of the mantle in a direction opposite to the motion of the core. This in turn brought about the break-down of Pangea and the separation of the continents. The drift of the continents, the relative changing of the earth's rotational axis and many other geological and geophysical phenomena may be explained through such a motion, that is through the motion of an eccentrical core towards the earth centre. 相似文献
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Prof. Dr. W. A. Heiskanen 《Pure and Applied Geophysics》1958,41(1):1-18
Summary The author mentions the aims of the World-wide gravity project he established in the Ohio State University in Columbus, in 1950. He outlines the practical procedure of the gravimetric computations of the undulationsN and the vertical deflection components and and emphasizes that only by the global international cooperation and additional gravity observations at sea carried out during the last decade it has been possible to gather to Columbus the needed gravity material. Since there exist still large gravimetrically unsurveyed areas it is of vital significance to study what gravity anomalies are best to be used for these regions. The given figures concerning the accuracy of theN, and , estimated theoretically and obtained in practice, indicate that in the gravimetrically well surveyed parts of the world like in Europe and the United States we can get gravimetrically on basis of existing gravity material theN-values with accuracy of about 5–10 meters, and and with the accuracy of about 1. The geoid undulationsN are already computed in Columbus for more than 6000 points of the northern hemisphere. The sample maps show the interesting geoid of Europe and vicinity between the latitudes 60° and 30° and longitude 5° W and 30° E, drafted on basis of more than 1000N-values computed at the corners of 1°×1° squares. It is interesting to realize that the geoid undulations in all this area are positive, the extreme values being between 40 and 50 meters. The geophysical significance of the geoid maps of this kind is pointed out. 相似文献
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针对我国当前较具典型的几种地震社会心理，指出职能部门疏导、防治的工作重点，并从顺应国情、民情及国家经济体制改革的方向出发，提出相应的对策建议。 相似文献
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本文搜集了2001—2013年间在太行山与燕山构造带交汇部位先后布设的4个宽频带流动地震台阵和首都圈固定地震台网共192个台站记录到的全球5.5级以上远震事件波形资料,综合采用接收函数H-κ和CCP叠加分析获得了134个基岩台站下方的地壳厚度和泊松比结果.综合分析与前人研究相吻合但更加精细的地壳约束分布信息,发现研究区域的地壳厚度和泊松比在整体上呈现出从西北到东南方向渐变的特征,在南北重力梯度带两侧及其附近呈现出明显的小尺度地壳结构和物质组分的差异,且可明显区分出太行山地区和燕山构造带及盆山交界处的地壳厚度与泊松比的相对差异,这可能反映了这些地区在华北克拉通的构造演化过程中所经历的不同地壳改造过程. 相似文献
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Kenneth A. Goettel 《Surveys in Geophysics》1976,2(4):369-397
Progress in understanding the condensation of planetary constituents from a solar nebula necessitates a re-examination of models for the origin and composition of the Earth. All models which appear to be viable require the Earth to have an Fe–FeS core and the full, or nearly full, solar (i.e. chondritic) K/Si ratio. The crust and upper mantle do not contain the requisite potassium for the entire Earth to have the solar K/Si ratio. Therefore, these models require that much of the Earth's potassium, about 80–90%, must be in the deep interior—in the lower mantle or in the core.The hypothesis that a substantial fraction of the Earth's potassium is in the Fe–FeS core is based on the chalcophilic behavior of potassium. Data including the stability of K2S, the occurrence of potassium in sulfide phases in meteorites and in metallurgical systems, and most importantly, experiments on potassium partitioning between solid silicates and Fe–FeS melts support this hypothesis. The present data appear to require at least several percent of the Earth's total potassium to be in the core. Incorporation of much larger amounts of potassium into the core, possibly most of the 80–90% of the Earth's potassium which is postulated to be in the deep interior, is not contradicted by the present data. Additional experimental data, at high pressures, are required before quantitative estimates of the core's potassium content can be made.It is likely that40K is a significant heat source in the core. Decay of40K is a plausible energy source to drive core convection to maintain the geomagnetic field, and to drive mantle convection and seafloor spreading. 相似文献
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Geomagnetism and Aeronomy - The behavior of the correlation between the radial BR and normal BN components of the interplanetary magnetic field (IMF) in the dependence on the time, the flow type of... 相似文献
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1 工作特点美国的地质学、地球物理学和海洋学家们利用他们所掌握的科学知识 (地球物理、地质和历史等方面的知识 )来确定水资源、矿产资源和能源等的状况 ,围绕如何保护环境 ,预测未来地质灾害 ,利用土地资源等问题开展工作。他们利用先进的仪器对地球和水资源进行分析研究。地质学家 ,同时也包括地球物理学家们研究地球的过去、现在和未来。例如他们研究地球运动 ,试图预报地震与火山会在何时何地发生 ,以及它们对周围地区的影响。虽然地质学、地球物理学、海洋学领域密切相关 ,但也有很大的不同。地质学家研究地球的构成、过程和历史。… 相似文献