五极纵轴测深法在溶洞探测中的应用   总被引：2，自引：0，他引：2  

曹平华  黄文清 《物探与化探》2003,27(4):323-325

以九江某地下溶洞探测工程为例,介绍了五极纵轴测深法的原理、方法及其应用效果.实地钻孔验证说明,五极纵轴测深法在城市地球物理勘探方面具有独特的优势,在未来的应用中必将有广阔的发展前景.  相似文献   

北斗在南/北极地区的基本定位性能评估     

徐炜  贾雪  乔方  刘扬  严超  王涛 《大地测量与地球动力学》2018,38(12):1268-1273

基于BDS、GPS系统的星座结构,对当前的BDS二代导航系统（BD2）、全部建成后的BDS系统在极地科考站（黄河站、昆仑站、中山站、长城站）和北极圈的可见卫星数、DOP值、定位精度等进行评估,并将建成后的BDS、GPS及其组合系统在南/北极的基本定位性能进行对比分析。仿真结果表明,当前的BD2只实现了极地的部分覆盖,对极地提供导航定位的能力有限,大范围内的定位精度大于30.0 m; BDS在极地的定位精度将与GPS相当,可见卫星数可达13颗左右,PDOP值优于1.6,定位精度优于8.0 m;GPS/BDS组合后在极地的PDOP值优于1.4,定位精度优于6.0 m。
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The “peeling” method to process apparent resistivity data for earthquake precursory monitoring     

Mao Xian-jin  Qian Jia-dong 《地震学报(英文版)》2001,14(6):685-691

Considering the fact that there is only one pair of fixed potential poles in one direction used to monitor the resistivity changes under the observatory station which may indicate process of earthquake preparation, based on the precondition that the resistivity structure is 1-dimensional under the observatory station, and by way of equivalent model put forward by the authors, this paper suggests a kind of method trying to separate the resistivity changes in deep layers from that of the shallow layer. Analysis shows that, to obtain the same measured data with the same array, any a multi-layered geo-electrical structure can be equivalently taken as a two-layered one, we call it equivalent model. In this paper, the resistivity and thickness of the upper layer of the equivalent model are equal to that of the first layer of the original one, the resistivity of the lower layer of the equivalent model is obtained with calculation according to the requirement of equivalence, its value is relevant with the resistivities and thicknesses of all layer of the original model except for the first one, so the resistivity change of the equivalent layer can indicate the synthetic effect of variation of all layers of the original model except for the first one. The primary research results show that this method can work well. Foundation item: Chinese Joint Seismological Science Foundation (100146).  相似文献   

中国中西部发展中城市的增长极作用   总被引：1，自引：0，他引：1  

柯善咨 《地理研究》2010,29(3):521-534

为了分析增长极在中部崛起和西部开发中可能发挥的作用,对我国中西部地域相连、经济水平接近的山西、河南、安徽、湖北、湖南、江西、广西、四川、重庆、陕西10个省(直辖市、自治区)的942个市县2000~2007年非农业GDP和就业增长的空间溢出效应进行了检验。模型估计表明,中西部地区各市县非农业经济增长的主要决定因素是自身的投入,同时,中心城市也存在明显的扩散和回流效应。地级市的非农业GDP增长对县级市有扩散效应,意味着城市间经济有一体化趋势,但是地级市的就业增长对县级市有抑制作用;地级城市对相对更不发达的县镇的GDP和就业增长同时具有带动作用;相邻的县级市相互间有较强的促进作用,但是对邻近县镇却有抑制倾向。  相似文献   

输电线路杆塔危岩威胁等级评价方法研究   总被引：1，自引：0，他引：1  

贾宁  孟庆辉  贾剑 《岩土力学》2010,31(2):604-608

从影响滚石击中塔体时的能量以及塔体被滚石击中的可能性出发,提出现场评价危岩对塔体威胁等级的方法。该方法考虑了边坡形状、塔位与山体的相对位置、坡上危岩的数量和大小以及坡脚滚石的数量和大小等因素。当边坡总体坡度相同时,上缓下陡的折线边坡,滚石落地速度最大;而内凹的曲线边坡,滚石落地速度最小。位于山体内凹一侧的塔位,塔体受危岩威胁最大,而位于山体凸出一侧的塔位,受危岩威胁最小。  相似文献   

Reassembling the Paleogene–Eocene North Atlantic igneous province: New paleomagnetic constraints from the Isle of Mull, Scotland     

Morgan Ganerd  Mark A. Smethurst  Sonia Rousse  Trond H. Torsvik  Tore Prestvik 《Earth and Planetary Science Letters》2008,272(1-2):464-475

The paleomagnetic data sets from the British Tertiary Igneous Province (BTIP) have recently been criticized as being unreliable and discordant with data from elsewhere in the North Atlantic Igneous Province (NAIP) [Riisager et al. Earth Planet. Sci. Lett. 201 (2002) 261–276; Riisager et al. Earth Planet. Sci. Lett. 214 (2003) 409–425]. We offer new paleomagnetic data for the extensive lava flow sequence on the Isle of Mull, Scotland, and can confirm the paleomagnetic pole positions emanating from important earlier studies. Our new north paleomagnetic pole position for Eurasia at 59 ± 0.2 Ma has latitude 73.3°N, longitude 166.2°E (dp/dm = 5.2/7.0).A re-evaluation and an inter-comparison of the paleomagnetic database emanating from the NAIP were carried out to test for sub-province consistency. We find a general agreement between the Eurasian part of NAIP (BTIP and Faeroes) and East Greenland data. However a compilation of West Greenland data displays a large and unexplained dispersion. We speculate on if this is related to different sense of block rotation of the Tertiary West Greenland constituents. Combining all data from the NAIP constituents, give a pole position at 75.0°N, 169.9°E (N = 25, K = 84.3, A₉₅ = 3.2) in Eurasian reference frame.  相似文献   

前兆地电阻率资料处理的剥皮法   总被引：2，自引：1，他引：2       下载免费PDF全文

毛先进  钱家栋 《地震学报》2001,24(6):645-650

在台址下电阻率分层均匀的前提下，针对我国绝大多数前兆地电台单极距观测的事实与现状，提出一种试图从这种观测所获得的视电阻率时间序列中识别电阻率表层变化和深部变化的等效模型方法．分析表明，在保持布极方式和观测结果不变的前提下，任意多层的地电结构都可以视为一个二层地电结构——等效模型．本文中，等效模型上层的地电参数（电阻率和厚度）与实际模型第一层相同，下层的地电参数（电阻率）则根据等效要求，由实际模型第二层及其以下各层的地电参数经计算得到，因此，等效模型的下层包含了实际模型第二层及其以下各层的综合影响．初步研究表明，这种方法是可行的．   相似文献   

地极的移动和全球构造     

田世丰 《地球科学》1991,16(4):395-401

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High-resolution plate reconstruction of the southern Mid-Atlantic Ridge     

Charles Weiland  Douglas S. Wilson  Ken MacDonald 《Marine Geophysical Researches》1995,17(2):143-166

We use recently acquired magnetic and SeaBeam bathymetric data to examine the spreading rates and plate boundary geometry of the Mid-Atlantic Ridge 30°–36° S. Using a statistically rigorous estimation of rotation poles we develop a precise spreading history of the African—South American plate boundary. The total opening rate for 1–4.23 Myr (Plio-Pleistocene) is nearly constant at 32.3 ± 1 km Myr^–1. The spreading rate apparently is faster in the Late Miocene (7.3-5.3 Myr), though this may reflect inaccuracies in the geomagnetic time scale. The rotation poles enable a plate boundary reconstruction with an accuracy of 2–3 km. The reconstructions also show that the plate boundary geometry underwent several changes since the late Miocene including the growth of one ridge segment from 40 to 105 km in length, and the reorientation of another ridge segment which has spread obliquely from 7 to 1 Myr. Pole calculations using both right- and left-stepping fracture zones show an offset of 1–2 km between the deepest, most linear part of a fracture zone trough and the former plate boundary location. The high-resolution plate kinematics suggests that the plate boundary, as a whole, evolves 2-dimensionally as prescribed by rigid plates. On a local scale, asymmetric accretion, asymmetric extension, small lateral ridge jumps (< 3 km), and intra-segment propagation result in minor plate boundary adjustments and deformation to the rigid plates.  相似文献   

近地质时期岩石圈板块构造运动的力学分析     

程学友 《地质与勘探》1995,31(5):15-22

运用相对运动的地球动力学理论，把软流圈以上的岩石圈和软流圈以下的地球内圈，作为两个独立的运动单元来考察它们随地球自转时所发生的变化和各自的运动状态。完整的岩石圈碎裂成岩石块之后，它们各自作为独立的单元，在纬向西漂力、经向离极力和洋底扩张力联合作用下，产生相对运动。  相似文献