乌鲁木齐地区现今构造应力场综合分析

乌鲁木齐地处天山中段.震源机制解研究表明,北天山中段区域主压应力方向为N10°E左右,且具有自西向东逐渐东偏的特点.在乌鲁木齐地区,由中强地震震源机制解反演的主压应力方向为N15°-20°E;由断层滑动资料反演的乌鲁木齐周边构造应力场的主压应力方向为N17°W-N2°E.上述两种资料反演的乌鲁木齐构造应力场主压应力方向...     

三维轴对称驻点流系统的一些研究(英文)

为了研究Navier-Stokes方程相关的三维轴对称驻点流系统的解,给出了一个积分方程系统,扩展了它的用途.并通过研究该积分方程系统的性质,在更广的范围内,利用这个系统的解,得出了与Navier-Stokes方程相关的三维轴对称驻点流系统的相似解.同时还改进了一个相似解的不存在性结果.     

我国海洋科技成果产业化发展研究

我国的海洋科技成果转化和产业化工作在相关政策的支持下,取得了瞩目的成就.文章回顾了海洋科技成果发展的历程,指出了海洋科技成果产业化对于我国海洋发展战略的重要意义,总结了近几年来我国海洋技术各个领域的产业化成果,揭示了产业化过程中面临的困难,提出了加速科技成果产业化的几点对策.     

Eigen solutions of internal waves over subcritical topography

Diapycnal mixing plays an important role in the ocean circulation.Internal waves are a kind of bridge relating the diapycnal mixing to external sources of mechanical energy.Difficulty in obtaining eigen solutions of internal waves over curved topography is a limitation for further theoretical study on the generation problem and scattering process.In this study,a kind of transform method is put forward to derive the eigen solutions of internal waves over subcritical topography in twodimensional and linear framework.The transform converts the curved topography in physical space to flat bottom in transform space while the governing equation of internal waves is still hyperbolic if proper transform function is selected.Thus,one can obtain eigen solutions of internal waves in the transform space.Several examples of transform functions,which convert the linear slope,the convex slope,and the concave slope to flat bottom,and the corresponding eigen solutions are illustrated.A method,using a polynomial to approximate the transform function and least squares method to estimate the undetermined coefficients in the polynomial,is introduced to calculate the approximate expression of the transform function for the given subcritical topography.     

论苗族传统知识在贵州麻山石漠化灾变救治中的价值

20世纪中期以来,麻山喀斯特山区随着周边社会环境的巨变,这些巨变冲击了麻山地区生态系统的脆弱环节,使麻山地区石漠化灾变日趋扩大。国家从20世纪60年代开始虽经多方救治,成效甚微。我们在对苗族生计方式的田野调查后发现,生息在这里的苗族积累有高效利用与精心维护喀斯特生态系统的经验和技能,发掘和利用苗族传统的地方性知识和技能,在石漠化灾变救治中具有不可替代的特殊价值。     

煤田三维地震勘探解决复杂地质问题的应用

煤田复杂地质问题是制约煤矿安全生产的主要难题,也是当前三维地震勘探需要解决的难题。本文根据三维地震勘探及这些地质问题的特点,将煤田复杂地质问题归纳为复杂地质构造问题、煤层赋存及岩性变化问题以及地质异常体问题,介绍了解决这些问题采用的方法及其特点和效果,并指出了其中某些方法的不足和改进方向。     

欧拉反褶积在重磁位场中应用与发展

介绍了欧拉反褶积方法原理,概述了国内外近几十年地球物理学者对欧拉反褶积方法进行的一系列改进及相关问题研究取得的主要进展和成就,并着重分析了构造指数的选取和欧拉解的稳定性等问题。通过分析指出了构造指数的正确选取、多场源混合叠加干扰和高阶次背景场研究及欧拉解的稳定性仍是今后欧拉反褶积方法研究重点和发展的主要方向,这对解决欧拉反褶积在重磁位场资料解释实用化中具有重要意义。     

珊溪水库地震小震震源机制解特征研究

利用P波初动和直达P、S波最大速度振幅比联合求解小震震源机制的方法求出珊溪水库ML2.0以上地震的震源机制,得到了珊溪水库震源机制各参数时空特征如下:主压应力为SN向,主张应力为EW向,应力主要为水平应力,发震断层倾角较大且多为走滑断层。在个别4级左右地震前P轴方位都有偏离再恢复的现象。在北纬27.65°～27.69°间,P轴方位集中在0°±30°或者180°±30°,节面走向集中在45°±15°或者135°±15°。震源深度大于4km的地震倾角多集中在70°～90°度之间。     

Focal Mechanism Solutions of the 2008 Wenchuan earthquake sequence from P-wave polarities and SH/P amplitude ratios:new results and implications

Abstract The 2008 Wenchuan earthquake, a major intraplate earthquake with Mw 7.9, occurred on the slowly deforming Longmenshan fault. To better understand the causes of this devastating earthquake, we need knowledge of the regional stress field and the underlying geodynamic processes. Here, we determine focal mechanism solutions （FMSs） of the 2008 Wenchuan earthquake sequence （WES） using both P-wave first-motion polarity data and SH/P amplitude ratio （AR） data. As P-wave polarities are more reliable information, they are given priority over SH/ PAR, the latter of which are used only when the former has loose constraint on the FMSs. We collect data from three categories： （1） permanent stations deployed by the China Earthquake Administration （CEA）; （2） the Western Sichuan Passive Seismic Array （WSPSA） deployed by Institute of Geology, CEA; （3） global stations from Incorporated Research Institutions for Seismology. Finally, 129 events with magnitude over Ms 4.0 in the 2008 WES are identified to have well-constrained FMSs. Among them, 83 are well constrained by P-wave polarities only as shown by Cai et al. （Earthq Sci 24（1）：115-125,2011）, and the rest of which are newly constrained by incorporating SH/P AR. Based on the spatial distribution and FMSs of the WES, we draw following conclusions： （1） the principle compressional directions of most FMSs of the WES are subhorizontal, generally in agreement with the conclusion given by Cai et al. （2011） but with a few modifications that the compressional directions are WNW-ESE around Wenchuan and ENE-WSW around Qingchuan, respectively. The subhorizontal compressional direction along the Longmenshan fault from SW to NE seems to have a leftlateral rotation, which agrees well with regional stress field inverted by former researchers （e.g., Xu et al., Acta Seismol Sin 30（5）, 1987; Acta Geophys Sin 32（6）, 1989; Cui et al., Seismol Geol 27（2）：234-242, 2005）; （2） the FMSs of the events not only reflected the regional stress state of the Longmenshan region, but also were obviously controlled by the faults to some extent, which was pointed out by Cai et al. （2011） and Yi et al. （Chin J Geophys 55（4）：1213-1227, 2012）; （3） while the 2008 Wenchuan earthquake and some of its strong aftershocks released most of the elastic energy accumulated on the Longmen- shan fault, some other aftershocks seem to occur just for releasing the elastic energy promptly created by the 2008 Wenchuan earthquake and some of its strong aftershocks. （4） Our results further suggest that the Longmenshan fault from Wenchuan to Beichuan was nearly fully destroyed by the 2008 Wenchuan earthquake and accordingly propose that there is less probability for great earthquakes in the middle part of the Longmenshan fault in the near future, although there might be a barrier to the southwest of Wenchuan and it is needed to pay some attention on it in the near future.     

New Periodic Solution for Planar 8-body Problems

For planar Newtonian 8-body problems with equal masses, we prove the existence of the new non-collision periodic solution such that two pair bodies move clockwise and the other two pairs counter-clockwise. This revised version was published online in July 2006 with corrections to the Cover Date.