Earthquake epicentroids in the Beijing-Tianjin-Tangshan-Zhangjiakou region inversed by gravity variation data   总被引：1，自引：0，他引：1  

郑金涵  宋胜合  刘克人  卢红艳  郭宗汾 《地震学报(英文版)》2003,16(4):449-458

Introduction Since the 1960s, gravity changes associated with seismogenesis and earthquake occurrences have been found by many researchers and various physical mechanisms have been proposed to explain these relationship (MEI, 1993; Chen, et al, 1979; Li, Fu, 1983). The US/China joint project beginning in 1981 presented a thorough study of the relationship between gravity variations and earthquake occurrences in the Beijing-Tianjin-Tangshan-Zhangjiakou (BTTZ) region, leading to a combined…  相似文献   

深源成矿物质与深部找矿分析   总被引：1，自引：0，他引：1  

张阔  赵闯  牛树银  孙爱群  王宝德  闫军印 《吉林地质》2008,27(4)

本文认为金银铅锌等成矿物质主要来自核—幔源区,通过地幔热柱多级演化迁移到地壳上部,在较好的构造扩容带中集聚成矿,而围岩萃取的成矿物质较为有限,不应花费很大精力去寻找所谓矿源层,而要侧重研究构造成矿控矿作用,对新一轮地质找矿和资源评价,特别是一些老矿山的深部、外围找矿有重要的参考价值。  相似文献   

UKF的改进算法及其在伪卫星定位中的应用     

LI Xue-peng  ZHANG You-qun  BAO Kuo 《测绘学院学报》2008,(2)

首先介绍了伪卫星导航系统的观测方程和动力学模型方程。然后,分析了基于UT变换的UKF算法,针对该算法存在的问题,结合迭代滤波思想和抗差估计原理提出了一种新的抗差UKF算法。并与EKF和UKF算法进行了比较。计算结果表明,该算法不仅可以提高滤波器的精度,而且能够更有效地控制观测异常对导航解的影响,使导航解更能反映导航系统的真实情况。  相似文献   

Temporal and spatial variations of post-seismic deformation following the 1999 Chi-Chi, Taiwan earthquake     

Ya-Ju Hsu  Paul Segall  Shui-Beih Yu  Long-Chen Kuo  Charles A. Williams 《Geophysical Journal International》2007,169(2):367-379

We use GPS displacements collected in the 15 months after the 1999 Chi-Chi, Taiwan earthquake  ( M _w 7.6)  to evaluate whether post-seismic deformation is better explained by afterslip or viscoelastic relaxation of the lower crust and upper mantle. We find that all viscoelastic models tested fail to fit the general features in the post-seismic GPS displacements, in contrast to the satisfactory fit obtained with afterslip models. We conclude that afterslip is the dominant mechanism in the 15-month period, and invert for the space–time distribution of afterslip, using the Extended Network Inversion Filter. Our results show high slip rates surrounding the region of greatest coseismic slip. The slip-rate distribution remains roughly stationary over the 15-month period. In contrast to the limited coseismic slip on the décollement, afterslip is prominent there. Maximum afterslip of 0.57 m occurs downdip and to the east of the hypocentral region. Afterslip at hypocentral depths is limited to the southern part of the main shock rupture, with little or no slip on the northern section where coseismic slip was greatest. Whether this results from along strike variations in frictional properties or dynamic conditions that locally favour stable sliding is not clear. In general, afterslip surrounds the area of greatest coseismic slip, consistent with post-seismic slip driven by the main shock stress change. The total accumulated geodetic afterslip moment is  3.8 × 10¹⁹ N m  , significantly more than the seismic moment released by aftershocks,  6.6 × 10¹⁸ N m  . Afterslip and aftershocks appear to have different temporal evolutions and some spatial correlations, suggesting that aftershock rates may not be completely controlled by the rate of afterslip.  相似文献   

地质灾害危险性评价研究——以四川省青川县为例   总被引：3，自引：0，他引：3  

李阔  杨景  唐川 《中国地质灾害与防治学报》2007,18(2):54-57,121

我国是一个地质灾害多发的国家。20世纪90年中期,每年造成1000多人死亡,经济损失高达200多亿元。地质灾害危险性评价是地质灾害调查的重要内容,也是风险管理及减灾管理的基础,它为管理部门制定出相应的减灾对策并为部署实施有效的减灾工程提供了科学依据。文章首先介绍了国内外地质灾害危险性评价方法的研究现状,通过对比,指出现阶段我国地质灾害危险性评价中的不足;结合实际工作经验,运用危险性评价指标对比法建立了简单有效的地质灾害危险性评价体系。以四川省青川县地质灾害调查为例,对该县地质灾害进行了危险性评价,为地质灾害易发区划分及防治分区提供了依据。  相似文献   

The Assimilation of GPS Radio Occultation Data and its Impact on Rainfall Prediction along the West Coast of India during Monsoon 2002     

Ching-Yuang Huang  Ying-Hwa Kuo  Shu-Ya Chen  Anisetty S. K. A. V. Prasad Rao  Chien-Ju Wang 《Pure and Applied Geophysics》2007,164(8-9):1577-1591

In this study, the Weather Research and Forecasting (WRF-2.0.3.1) model with three-dimensional variational data assimilation (3DVAR) was utilized to study a heavy rainfall event along the west coast of India with and without the assimilation of GPS occultation refractivity soundings in the monsoon period of 2002. The WRF model is a next-generation mesoscale numerical weather prediction system designed to serve both operational forecasting and atmospheric research communities. The Global Positioning System (GPS) radio occultation (RO) refractivity data, processed by UCAR, were obtained from the CHAMP and SAC-C missions. This study investigates the impact of thirteen GPS occultation refractivity soundings only, as assimilated into the WRF model with 3DVAR, on the rainfall prediction over the western coastal mountain of India. The model simulation, with the finest resolution of 10 km, was in good agreement with rainfall observations, up to 72-h forecast. There are some subtle but important differences in predicted rainfalls between the control run CN (without the assimilation of refractivity soundings) and G13 (with the assimilation of thirteen GPS RO soundings). In general, the assimilation run G13 gives a better prediction in terms of both rainfall locations and amounts at later times. The moisture increments were analyzed at the initial and forecast times to assess the impact of GPS RO data assimilation. The results indicate that remote soundings in the forcing region could have significant impacts on distant downstream regions. It is anticipated, based on this study, that considerably occultation soundings available from the six-satellite constellation of FORMOSAT-3/COSMIC would have even more significant impacts on weather prediction in this region.  相似文献   

昆明市东川城区后山泥石流危险性评价   总被引：4，自引：1，他引：4  

李阔  唐川 《云南地理环境研究》2005,17(6):23-28

云南省是中国遭受泥石流灾害最严重的省区之一,而对危险范围和危险程度进行划分和评估是泥石流减灾的重要内容。以昆明市东川城区后山泥石流为例,应用泥石流沟危险度综合评价法对泥石流危险度进行了评价;接着应用流域背景预测模型对泥石流危险范围进行预测,在这些数据和已构建的东川城区数字高程模型数据的基础上,应用GIS生成了以上泥石流危险范围预测图,研究成果为东川城区减灾防灾提供了科学依据。  相似文献   

A general solution for groundwater flow in an estuarine's leaky aquifer system after considering aquifer anisotropy          下载免费PDF全文

Po‐Chia Chen  Mo‐Hsiung Chuang  Yih‐Chi Tan  Kuo‐Chen Ma 《水文研究》2016,30(12):1862-1871

This paper presents an analytical model for describing the tidal effects in a two‐dimensional leaky confined aquifer system in an estuarine delta where ocean and river meet. This system has an unconfined aquifer on top and a confined aquifer on the bottom with an aquitard in between the two. The unconfined and confined aquifers interact with each other through leakage. It was assumed that the aquitard storage was negligible and that the leakage was linearly proportional to the head difference between the unconfined and confined aquifers. This model's solution was based on the separation of variables method. Two existing solutions that deal with the head fluctuation in one‐dimensional or two‐dimensional leaky confined aquifers are shown as special cases in the present solution. Based on this new solution, the dynamic effect of the water table's fluctuations can be clearly explored, as well as the influence of leakage on the behaviour of fluctuations in groundwater levels in the leaky aquifer system. Copyright © 2015 John Wiley & Sons, Ltd.  相似文献   

Ancient mantle lithosphere beneath the Khanka massif in the Russian Far East: in situ Re–Os evidence          下载免费PDF全文

Kuo‐Lung Wang  Vladimir Prikhodko  Suzanne Y. O'Reilly  William L. Griffin  Norman J. Pearson  Victor Kovach  Yoshiyuki Iizuka  Yu‐Hsian Chien 《地学学报》2015,27(4):277-284

The Os‐isotope compositions of sulphides in mantle xenoliths hosted by Late Miocene alkali basalts from the Sviyaginsky volcano, Russian Far East, reveal the presence of Archaean–Proterozoic subcontinental lithospheric mantle beneath the Khanka massif. Their T_MA and T_RD model ages reveal similar peaks at 1.1 and 0.8 Ga suggesting later thermotectonic events in the subcontinental lithospheric mantle, whereas T_RD model ages range back to 2.8 ± 0.5 (2σ) Ga. The events recognized in the subcontinental lithospheric mantle are consistent with those recorded in the crust of the Khanka massif. The sulphide Os‐isotope data show that the subcontinental lithospheric mantle beneath the Khanka massif had formed at least by the Mesoproterozoic, and was subsequently metasomatized by juvenile crustal‐growth events related to the evolution of the Altaids. The Khanka massif is further proposed to have tectonic affinity to the Siberia Craton and should originate from it accordingly.  相似文献   

低温无固相钻井液配方优选及经济性评价          下载免费PDF全文

周忠鸣  张扩  朱宝 《探矿工程》2015,42(4):21-25

为解决高原冻土和天然气水合物勘探过程中钻进和取心问题,选择了NaCl作为抗冻剂,抗盐共聚物GTQ和水解聚丙烯酰胺PHP作为主要聚合物试剂,采用正交试验法,在常温下优选出了9组配方,经过低温测试,确定了在 -15 ℃可用的钻井液配方Z1（20%NaCl+0.1%PHP+1.2%GTQ+1%KHm）和Z2（25%NaCl+0.15%PHP+1.0%GTQ+1%KHm）,其主要性能指标分别为：AV值46.5、47.5 mPa·s,PV值34、35 mPa·s,YP值12.8、12.8 Pa,FLAPI值6.8、7.6 mL/30 min。经成本核算,2种配方具有比较好的经济性,可以满足高原冻土层钻进要求。  相似文献