THE COMPREHENSIVE ANALYSIS AND RESEARCH OF RECENT GRAVITY AND CRUSTAL DEFORMATION IN NORTHEASTERN EDGE OF THE TIBETAN PLATEAU

In this study, we systematically analyzed the relationship between regional gravity changes, 3D crustal deformation, regional tectonic environment and strong earthquakes based on the relative gravity measurements(2011-2014), GPS data and the background vertical deformation from the leveling measurements conducted from 1970 to 2011. Subsequently, we further characterized the temporal-spatial patterns and discussed the mechanism of regional gravity changes and the crustal deformation. The results can be summarized as follows:1)The regional gravity changes, the GPS-derived horizontal deformation and the vertical deformational obtained from leveling data showed a close spatial relationship:The gravity increased along with the direction of horizontal movement, and the gravity decreased with the crustal uplift and vice versa, which reflects the inherited characteristics of neotectonic activities. 2)The crustal deformation was closely related to the active faults. The contour lines of gravity changes and vertical deformation were generally along with the Qilian-Haiyuan Fault(the strike is NWW), and the crustal horizontal deformation showed left-lateral strike slip motion near the Qilian-Haiyuan Fault. 3)The strong earthquakes usually occur in the active faults where intensive gravity change and vertical and/or horizontal deformation occurred. The extrusion deformation, surface compression rate and gravity changes were obvious near the epicenter of 2016 Menyuan earthquake. The 2013 Minxian-Zhangxian M_S6.6 earthquake occurred in the direction-turning area of intense gravity gradient zone and the transitional area of surface compression and vertical deformation. The first author of this paper has made a medium-term forecast before the Minxian and Menyuan earthquakes, especially the location of the earthquake. Based on the above understandings, we emphasized that:there are still possibilities of strong or huge earthquakes within medium-long term in the areas of crustal deformation anomalies in the study region.     

低电离层调制激励VLF/ELF辐射参数优化理论分析

针对低电离层幅度调制加热过程中甚低频/极低频（VLF/ELF）激发效率较低的问题,该文利用低电离层调制加热模型分析方波幅度调制加热过程中占空比和加热频率对VLF/ELF辐射效率的影响,在此基础上获得最大VLF/ELF辐射效率下的优化占空比和加热频率选择范围.研究表明,随着调制波占空比的增大,激发的VLF/ELF等效辐射源强度先增大后减小,占空比的优化范围为40%~70%;随着加热频率的增大,激发的VLF/ELF等效辐射源强度先增大后减小,加热频率的优化范围为（0.8~0.9）倍低电离层临界频率.     

一种卫星钟差精度评估方法

GNSS观测量测量的是测站与卫星间的相对时间延迟,卫星钟差求解的是相对于基准钟的相对钟差,因此卫星钟差的精度评估方法不同于其他GNSS产品。分析了卫星钟差的精度评估方法,采用消除卫星钟系统偏差的方法进行钟差精度的评估,得到的各产品的精度评定结果与各产品公布的钟差精度基本一致,证明了此方法的有效性。     

64排CT冠脉成像与PET-CT心肌灌注显像对照分析的临床价值

目的:比较64排CT冠脉成像(CTCA)与PET-CT心肌灌注显像(MPI)对相关冠状动脉狭窄,及准确定位"罪犯"血管的价值。方法:回顾性分析内蒙古医科大学附属医院2009年3月到2014年12月,在四周内进行CTCA与MPI的临床确诊及可疑的冠心病(CAD)患者59例,由2名有经验影像与核医学医师进行图像及数据分析,按照冠状动脉节段性供血特点,分析冠状动脉供血区域和心肌节段对应关系,采用Spearman等级相关、Pearson相关和Kappa检验方法。结果:59例患者按照LAD、LCX、RCA三支冠状动脉支配心肌部位来统计,合计177支血管,冠脉血管0级58支;Ⅰ级24支;Ⅱ级33支;Ⅲ级40支;Ⅳ级22支。灌注0分63支;1分30支;2分45支;3分27支;4分12支。三支冠状动脉CTCA与MPI分别行相关性分析和吻合度分析,两者为正性相关,吻合率较高。LAD r=0.764,P=0.000;LCX r=0.593,P=0.000;RCA r=0.831,P=0.000。LAD k=0.666,P=0.000;LCX k=0.601,P=0.000;RCA k=0.589,P=0.000。结论:CTCA的解剖学信息和MPI生理学功能性信息相互结合,有效互补,两者结合能够准确定位CAD患者的"罪犯"血管,大大提高CAD诊断准确率,为临床治疗及预后判断提供有力依据。      

地震下双曲线冷却塔的响应分析

借助ANSYS软件建立双曲线冷却塔的有限元分析模型,讨论自重、风荷载和地震作用下冷却塔的力学性能,通过计算、分析探讨塔筒局部开洞对冷却塔整体及洞口局部强度的影响,主要考虑洞口尺寸和开洞高度对冷却塔整体及洞口局部应力分布规律的影响。结果表明:在一定尺寸范围内,开设洞口对冷却塔的整体强度影响较小,但在洞口局部出现明显的应力集中效应;90 m高度处洞口的应力集中效应低于15 m高度处洞口的应力集中效应,但应力集中效应不容忽视。分析结果为冷却塔结构抗震的设计、加固和施工提供了理论依据和实用的参考建议。     

Clay mineralogy of an Eocene fluvial-lacustrine sequence in Xining Basin,Northwest China,and its paleoclimatic implications

The Eocene was marked by significant cooling during which the global climate was transformed from greenhouse to icehouse conditions. Notable coeval events were the India-Asia collision and the retreat of the Paratethys Sea in Asia. The Eocene section of the long and continuous sedimentary succession of the Xining Basin in Northwest China is characterized by red mudstones with intercalated gypsum and muddy-gypsiferous layers. In this study, we conducted a semi-quantitative analysis of the mineralogy of bulk samples and the clay fraction using X-ray diffraction, with the aim of characterizing the Eocene climatic evolution of the northeastern margin of the Tibetan Plateau and inland Asia. We used a new pretreatment method to address the problem of extracting sufficient clay particles from the gypsum and gypsiferous layers. The bulk mineralogy is dominated by quartz, feldspar, calcite, gypsum and dolomite; and the clay mineralogy is dominated by illite, chlorite, and smectite(including irregular mixed-layer illite-smectite(I/S)). The variations of the clay mineral assemblages indicate the occurrence of alternations between warm humid conditions and hot dry conditions, with relatively high humidity during ～52–50,～41.5–39 and ～35–34 Ma. Comparison of the results with the timing of Tibetan Plateau uplift, transgressions and regressions of the Paratethys Sea, and the marine oxygen isotope record suggest that the Eocene climatic evolution of the study region was driven fundamentally by global climate change.     

孤岛工作面动力灾害预防控制方法研究

为研究孤岛工作面安全开采方法,理论分析其动力灾害多发的岩层运动及应力条件,并提出其安全开采的准则。认为只要合理设计开采参数,就可以避免孤岛工作面动力灾害的发生。分析表明:孤岛工作面长度大于相邻工作面支承压力影响范围之和时,孤岛工作面支承压力无法叠加,工作面较安全;相邻工作面长度大于关键层断裂步距时,覆岩关键层可充分塌垮,孤岛工作面无动压冲击危险;在稳定的内应力场开掘回采巷道时,回采巷道无冲击危险。     

湖北秭归4.5级和4.1级地震前的流动重力变化

处理分析2016～2018年三峡流动重力测网资料,获得2016-03～2018-09共11幅差分和累积重力场变化图像,并结合2018-10-11发生在湖北秭归的4.5级和4.1级地震,分析震前重力场变化特征。结果表明：1）2017年以来,震中区重力场变化经历了从先减小后增大到震前趋缓的过程。2）2 a累积重力场变化显示,新华-龙王冲和高桥断裂带两端重力场变化差异增大,可能与本次地震的孕育有关。3）只要测网网格距合理、数据处理得当,区域流动重力测网对4.0级小震前的重力场变化具有潜在的监测能力。     

基于CORS的分米级GNSS差分定位云服务研究

面向GNSS大众应用领域海量高精度位置服务需求,提出了一种基于CORS的分米级差分定位云服务建设方法,采用虚拟格网用户生成改正数的形式,通过设计解算服务器与业务服务器分离的云服务模式,解决了传统CORS服务中基准站数据安全风险大、用户并发访问数量受限的问题,并以API和SDK形式面向用户和开发者提供应用服务,降低了高精度位置服务专业技术门槛。同时,依托本文研究成果,基于湖南省位置服务平台（HNCORS）,设计并实现了基于CORS的分米级GNSS差分定位云服务架构,并以丢包率、外符合精度、高并发访问为指标进行测试。结果表明,本文设计的云服务架构具有较好的精度、稳定性和可靠性,在高精度位置服务应用中具有较好的应用前景,也可为其他省级CORS网的高精度位置服务云平台建设提供技术参考。     

监控视频中动态目标与地理空间信息的融合与可视化方法

监控视频的动态前景目标智能分析是平安城市、智慧园区等安防建设的重要基础,将监控视频与地理空间数据融合可为静态的地理数据赋予动态属性。针对传统监控视频与地理信息数据集成仅仅将视频数据投射至地理空间,造成存储难、视频内容理解难度大等问题,本文提出了前景动态目标与地理空间信息的融合模型,通过推导出的映射模型将图像空间中的动态前景目标及跟踪轨迹映射至地理空间中,达到将监控视频与地理信息有机融合的目的。根据不同的应用需求,本文设计了4种多图层融合显示模式,实现了监控视频中的动态前景目标在地理空间的可视化。