黔南坳陷及邻区盆地演化和海相沉积的后期改造

黔南坳陷是扬子克拉通内由3组不同方向的断裂围限的一个相对稳定的区块。分4个阶段（新元古代,早古生代,晚古生代—三叠纪,侏罗纪—古近纪）重塑了贵州南部及邻区与周边造山作用耦合的盆地演化。广西运动形成北东向构造,是海相沉积建造阶段中的一次重要改造。印支运动使贵阳—镇远断裂和紫云—罗甸断裂反转,奠定了其成为黔南坳陷的北界和西南界断裂的基础。中侏罗世后的逆掩—冲断可分为两期：早期称燕山运动,以北东走向的断裂向北西逆冲和扩展为特征;晚期称燕山末期—喜马拉雅运动,区域上表现为北北东走向的断裂向南东东逆冲,铜仁—三都断裂成为黔南坳陷的东界,印支运动形成的近南北向—北北东向断层向西（偏北）逆冲,构成铜仁—三都断裂的背冲构造。近南北向断层上盘发育的开阔背斜是黔南坳陷内海相油气勘探的最有利靶区。     

Stability analysis of MDOF real‐time dynamic hybrid testing systems using the discrete‐time root locus technique

The time delay resulting from the servo hydraulic systems can potentially destabilize the real‐time dynamic hybrid testing (RTDHT) systems. In this paper, the discrete‐time root locus technique is adopted to investigate the delay‐dependent stability performance of MDOF RTDHT systems. Stability analysis of an idealized two‐story shear frame with two DOFs is first performed to illustrate the proposed method. The delay‐dependent stability condition is presented for various structural properties, time delay, and integration time steps. Effects of delay compensation methods on stability are also investigated. Then, the proposed method is applied to analyze the delay‐dependent stability of a single shaking table RTDHT system with an 18‐DOF finite element numerical substructure, and corresponding RTDHTs are carried out to verify the theoretical results. Furthermore, the stability behavior of a finite element RTDHT system with two physical substructures, loaded by twin shaking tables, is theoretically and experimentally investigated. All experimental results convincingly demonstrate that the delay‐dependent stability analysis on the basis of the discrete‐time root locus technique is feasible. Copyright © 2014 John Wiley & Sons, Ltd.     

嘉山地震台大地电场观测异常干扰研究

地电场观测是地震电磁前兆观测方法之一,由于其观测物理量所受到的干扰因素较多,因此通过对嘉山地震台大地电场观测中常出现的地电阻率同场观测干扰、雷电干扰、降雨影响、电极极化、磁暴干扰等5种干扰和典型变化形态进行识别分析,可有效剔除干扰,从而为提取地震前兆信息,分析和运用地电场资料进行地震预报提供可靠依据,也为观测场地大致相同的其他台站提供参考。     

各向异性介质中的浅海海洋可控源电磁响应特征

由于受到空气波的影响,浅海海洋可控源电磁数据对海底储油层的反映较弱,如何对浅海数据进行处理和解释一直是海洋电磁理论研究的热点。随着近年来海洋电磁理论的不断完善,浅海数据已经可以被较好地处理与反演,但是其解释水平仍然受基本理论研究不足的制约。针对这一现状,本文开展了海底电各向异性对浅海数据影响规律的研究。具体方法为:利用欧拉旋转建立不同的海底电性各向异性模型,然后采用交错网格有限差分法计算浅海海洋可控源电磁响应,最后通过分析同线情况下电场E_x分量的振幅和相位曲线特征以及海底电场及电流密度分布规律,分析各向异性对浅海海洋可控源电磁响应影响的物理机制,并讨论浅海各向异性情况下海洋电磁对高阻储油层的识别能力。得出的结论为各向异性介质中的浅海海洋电磁响应特征与深海有较大区别,在进行数据的处理、反演和解释时应区别于深海情况。     

空间跟踪技术的发展对月球重力场模型的改进

本文基于绕月卫星跟踪技术的三种模式,即地面跟踪模式、高低跟踪模式和低低跟踪模式,将月球重力场的发展历程分为四个阶段.分别介绍了各阶段跟踪模式的主要原理、技术特点以及所获取的具有代表性的重力场模型,并对这些模型的精度特征进行了评述.进而,通过分析不同阶段重力场模型所获取的月球重力异常特征和精度、不同阶段重力场模型的定轨精度,阐明了:空间跟踪技术的进步,极大地提高了月球重力场模型的精度,并且,有效地促进了对月球物质结构特征的认识和绕月卫星定轨的可靠性.最后对月球重力场模型中尚存在的问题以及探测技术的发展前景进行了分析和展望.     

A Lunar-based Soft X-ray Imager(LSXI) for the Earth's magnetosphere

We propose to use the Moon as a platform to obtain a global view of Earth's magnetosphere by a Lunar-based Soft X-ray Imager(LSXI). LSXI is a wide field-of-view Soft X-ray telescope, which can obtain X-ray images of Earth's magnetosphere based on the solar wind charge exchange(SWCX) X-ray emission. Global perspective is crucial to understand the overall interaction of the solar wind with magnetosphere. LSXI is capable of continuously monitoring the evolution of geospace conditions under the impact of the solar wind by simultaneous observation of the bow shock, magnetosheath,magnetopause and cusps for the first time. This proposal is answering the call for the Chinese Lunar Exploration Program Phase IV.     

可扩展的并行地理图像处理系统

可扩展的并行地理图像处理系统 (Par GIP)是基于多操作系统平台的机群并行图像处理系统 ,它采取Client- Server结构 ,采用插件技术和算法化的处理操作 ,具有良好的发展前景.     

台风“烟花”对江苏地区台基噪声自相关函数卓越周期的影响

2021年第6号台风“烟花”是2021年度对江苏地区影响最强烈的台风。地震台站台基噪声是影响观测质量的关键因素,为了探究台风“烟花”对江苏地区地震台站台基噪声的影响,利用江苏地震台网2021年7月1日至8月3日记录的连续波形数据,通过计算波形自相关函数卓越周期与台基噪声水平的速度均方根有效振幅(RMS),研究其与台风参数之间的关系。结果表明：①在台风 “烟花”初始发育阶段,卓越周期由平时的2—4 s逐步上升到4—7 s,随着台风影响范围逐渐向陆地转移,卓越周期缓慢降低,随着台风完全登陆并不断减弱,卓越周期又恢复到正常水平;②在台风“烟花”的整个进程中,绝大多数台站的RMS值变化幅度不超过正常值的15%,各台站RMS值变化幅度在正常波动范围内。     

显胎生红树植物木榄(Bruguiera gymnorrhiza)胎生胚轴发育

跟踪测定显胎生红树植物木榄(Bruguiera gymnorrhiza)胎生胚轴发育过程中的长度、密度、鲜重、干重、含水量、渗透势、五种主要无机渗透调节离子(Ca2+,Mg2+,Na+,K+,Cl-)浓度及含量的变化.结果表明:木榄胚轴在发育过程中不断积累有机营养物质以及盐分,并在母树上完成渗透调节、器官形成等生理过程;可以将木榄繁殖体的发育过程划分为果期、生长活跃期和成熟期3个阶段;比较胚轴和生境中土壤、海水的理化指标,可以得出木榄胚轴的密度、渗透势以及盐分水平的变化是以适应母树所处的高盐和周期性海水浸淹生境为目标;探讨了木榄胎生现象的生理生态学意义及适应方式.     

Distribution and Variability of the Meiobenthic Assemblages near the Korean Polymetallic Nodule Claim Area of the Clarion-Clipperton Fracture Zone (Subequatorial NE Pacific)

This study was carried out as part of a baseline long-term environmental project in the proposed mining areas for an environmental impact assessment of future mining in the Clarion-Clipperton Fracture Zone (CCFZ). The community structure and distributional pattern of meiobenthos were investigated in the deep-sea bottom of the Clarion-Clipperton Fracture Zone of the northeastern Pacific in July 1998, 1999, 2001, 2003 and August 2004, 2005. Twenty one meiobenthic groups were found at the stations in the study area. The most abundant meiobenthos comprised nematodes followed by benthic foraminiferans and harpacticoid copepods. The maximum density of meiobenthos was 306 ind/10 cm² at the station located at 11°N (water depth, 4833 m), and the minimum density was 6 ind/10 cm² at the station located at 14°N (water depth, 5037 m). Oligotrophic conditions in the CCFZ seem to directly reflect the lower standing stocks of meiobenthos in the CCFZ compared to other deep-sea plains of similar depth. The latitudinal distribution pattern of meiobenthos in the study area seemed to be related with surface water primary productivity, which was connected to the water circulation pattern of the Pacific Ocean near the Equator, diverging at 8ºN latitude and converging at 5°N. The horizontal distribution of meiobenthic organisms in the study area showed high densities at the stations within 135–136°W. The densities of meiobenthic organismas within the CCFZ were high at stations with few manganese nodules on the sediment surface at low-latitude sites. In 1998, the observed relative high values of meiobenthic abundance were at stations from 5° to 6°N. Other stations from 7° to 10°N showed no significant fluctuations during the interannual sampling periods. It is considered that the inter-annual fluctuation of meiobenthos abundance is intimately related with a regime shift that may have occurred in the north Pacific between 1998 and 1999, the El Niño period. Vertical distribution of meiobenthic organisms showed the highest individual numbers in the surface sediment layers of 0～2 cm depth and a steep decreasing trend as sediment becomes deeper at the stations of high latitude located in 16～17°N. Size distribution analyses showed that organisms that fit into the sieve mesh size of 0.063 mm were abundant.