基于Android智能终端的地震现场应急指挥技术系统运维信息管理平台

地震现场应急指挥技术系统在震后救援行动中发挥着重要的通信和指挥枢纽作用,为了提升现场技术系统的运维质量,并解决目前运维时上报信息分散且不易查询的问题,本文基于C/S架构设计了1套运维信息管理平台,客户端采用手机、平板电脑等智能终端,基于Android SDK进行应用程序开发,采用轻量级文本格式JSON与服务器端进行数据交互。客户端用户登录平台后,可上报文字和图片信息,也可根据上报时间、内容、位置等关键字查询历史信息,实现了信息的汇总和共享;平台还设计了故障排查辅助、设备操作说明、演练信息发布等实用功能,数据汇集在服务器端,便于管理和考核。本系统已在山东省地震局部署应用,有效提升了地震现场工作的效率和水平。     

移动智能终端在贵州省耕地质量地球化学调查的实践应用

基于移动互联网、大数据发展的时代背景,本文提出了移动智能终端辅助耕地质量地球化学调查工作新模式,并应用到贵州省耕地质量地球化学调查实际采样工作中,改变了传统的工作方式,极大地提高了采样工作效率,改善了野外工作设备的便携性和室内外沟通性,加快了贵州省耕地质量地球化学调查评价项目的工作进度,为其他省开展相关工作起到示范作用。     

Anatomy and facies distribution of terminal lobes in ephemeral fluvial successions: Jurassic Tordillo Formation,Neuquén Basin,Argentina

In terminal fluvial-fan systems, characteristic proximal to distal variations in sedimentary architectures are recognized to arise from progressive downstream loss of water discharge related to both infiltration and evaporation. This work aims to elucidate downstream trends in facies and architecture across the medial and distal zones of terminal-fan systems, which record transitions from deposits of channel elements to lobe-like and sheet-like elements. This is achieved via a detailed characterization of ancient ephemeral fluvial deposits of the well-exposed Kimmeridgian Tordillo Formation (Neuquén Basin, Argentina). The fine sand-prone and silt-prone succession associated with the medial to distal sectors of the system has been studied to understand relationships between depositional processes and resulting architectures. Facies and architectural-element analyses, and quantification of resulting sedimentological data at multiple scales, have been undertaken to characterize sedimentary facies, facies transitions, bed types, architectural elements and larger-scale architectural styles. Eight bed types with distinct internal facies transitions are defined and interpreted in terms of different types of flood events. Channelized and non-channelized architectural elements are defined based on their constituent bed types and their external geometry. The most common elements are terminal lobes, which are composite bodies within which largely unconfined sandy deposits are stacked in a compensational manner; a hierarchical arrangement of internal components is recognized. Proximal feeder-channel avulsion events likely controlled the evolution of terminal-lobe elements and their spatiotemporal shifts. Stratigraphic relations between architectural elements record system-wide trends, whereby a proximal sector dominated by channel elements passes downstream via a gradational transition to a medial sector dominated by sandy terminal-lobe elements, which in turn passes further downstream to a distal sector dominated by silty terminal lobe-margin and fringing deposits. This work enhances current understanding of the stratigraphic record of terminal fluvial systems at multiple scales, and provides insight that can be applied to predict the facies and architectural complexity of terminal fluvial successions.     

lbb-用于射电天文VLBI基带数据读写的库

Library for Baseband (lbb)是一个自研的用于读取解析甚长基线干涉测量(Very Long Baseline Interferometry, VLBI)基带数据的工具库,主要用于VLBI观测中对终端基带数据的读取、解析及输出结果分析.该软件库通过对基带数据的自动判断,自动实现读取不同数据格式的功能,并提供了各种各样的API (Application Programming Interface)功能供用户调用.目前lbb软件库已经成功应用在了探月工程VLBI测轨任务中的硬件相关处理机配置项和测地VLBI观测数据的预处理.文章详细介绍了lbb软件库的设计、功能及用法.     

基于功率变化的移动终端欺骗干扰检测方法

对欺骗信号的功率检测是目前最常用的欺骗检测方法之一,但欺骗源可以通过调整发射的信号功率,仍然可实现对环形范围内所有终端的欺骗攻击．针对该问题,本文提出了一种基于信号功率变化的移动终端欺骗干扰检测方法,该方法利用了真实卫星和欺骗源与终端在距离上差异的本质属性,通过终端运动情况下真实信号与欺骗信号在相同距离上信号功率变化的不同,实现对近距离欺骗干扰源的有效检测．本文建立了移动终端导航信号功率变化模型,并在此基础上给出了针对欺骗信号的二元假设检验方法．通过理论分析和仿真实验,验证了本文提出的基于信号功率变化的移动终端欺骗干扰检测技术的有效性,当干扰源距离终端小于2 000 m,终端运动距离大于200 m即可实现在1％的虚警概率下实现对97％以上欺骗攻击的有效检测．      

Precambrian crustal evolution in Rangrim Massif,Korean Peninsula

Petrological, chronological and geotectonic geological analysis of Precambrian metamorphic rock in Korean Peninsula shows that the remnants （ 〉3.4 Ga） of continental nuclei crust were formed in the Paleoarchean in the Rangrim Massif. In the massif, the main formation ages of continental crust range from 3.2 Ga to 2.5 Ga, its important growing period was 2.8 - 2. 5 Ga. The subsequent expansion period of the Rangrim Massif was 2. 4 - 2. 2 Ga. The division events occurred in 1.85 Ga and in the Late Paleoproterozoic-Early Mesoproterozoic, respectively. Since then the massif was relatively stable. However, the last division of the Rangrim Massif occurred at 793 Ma.     

一种基于E-Key及Web页面监控的网站防篡改机制研究

通过监控Web页面文件变化和利用E-Key数字证书提高操作安全的网站防篡改机制,可以有效减少甚至消除由于网页遭遇篡改而给企业造成负面影响的目的.特殊设计的Web页面访问过滤监控程序通过计算,比对摘要,可以及时发现被篡改页面并执行删除操作和通知Web页面文件监控程序.Web页面文件监控程序立即停止Web服务,并删除变化文件.Web页面文件监控程序定期向Web页面安全管理服务程序发送心跳包,Web页面安全管理服务程序通过对心跳包的实时监测监控文件变化情况,并及时进行修复还原和报警,同时进行文件更新管理以及文件及其摘要备份.客户端安全控件实现操作者E-Key数字证书和服务器证书间的双向认证,确保web管理者远程操作过程的安全性.     

鲁西蒙山山脉中段早前寒武纪花岗质岩石岩石学和单锆石年龄

用Ｋｏｂｅｒ方法测定了平邑县、蒙阴县普照寺闪长岩、松山－邱子峪二长花岗岩、周公地－花果庄－宁子洞花岗闪长岩、余粮店辉长岩和东近台英云闪长岩的锆石年龄。多数样品中的锆石反映了多于一期的地质记录，其中东近台英云闪长岩中的锆石（２８６８±１３Ｍａ、２７１２±５Ｍａ、２７１１±７Ｍａ和２５９８±６Ｍａ误差均为２σ），反映了本区最老的地质记录；部分样品中的２４００Ｍａ可能反映了太古宙最后一期的地质作用；而大部分样品中的锆石显示了２５００Ｍａ和２６００Ｍａ的地质记录，即岩浆活动多集中于２６００Ｍａ、２５００Ｍａ和２４     

Precambrian crustal contribution to the Variscan accretionary prism of the Kaczawa Mountains (Sudetes,SW Poland): evidence from SHRIMP dating of detrital zircons

SHRIMP dating of detrital zircons from sandstones of the Gackowa Formation (Kaczawa Complex, Sudetes, SW Poland) indicates input from late (550–750 Ma) and early Proterozoic to Archaean sources (∼2.0–3.4 Ga, the latter being the oldest recorded age from the Sudetic region). These dates preclude within-terrane derivation from seemingly correlatory acid volcanic rocks of early Palaeozoic age. Rather, they indicate provenance from Cadomian and older rocks that currently form part of other, geographically distant terranes; the most likely source identified to date is the Lusatian Block in the Saxothuringian Zone. Hence, the Gackowa Formation may be late Proterozoic rather than early Palaeozoic in depositional age, possibly coeval with the late Proterozoic (pre-Cadomian) greywackes of Lusatia, being subsequently tectonically interleaved with early Palaeozoic volcanic rocks into the Kaczawa accretionary prism during the Variscan orogeny. However, correlation with the lithologically similar early Ordovician Dubrau Quartzite of Saxothuringia, and so assignation to the early Paleozoic (post-Cadomian) rift succession deposited at the northern margin of Gondwana, cannot yet be precluded.     

Isotopic connections between basement rocks exposed in the St. Francois Mountains and the Arbuckle Mountains,southern mid-continent,North America

Two distinct crustal provinces have been identified in the southern mid-continent based on U–Pb crystallization ages. Both contain large volumes of undeformed granite and rhyolite, with minor amounts of metamorphic rock and mafic intrusions. The Eastern Granite-Rhyolite province is characterized by felsic rocks with crystallization ages of 1,470 ± 30 Ma and exposures are restricted to the St. Francois Mountains in southeastern Missouri. Similarly, the Southern Granite-Rhyolite (SGR) province is characterized by felsic units with ages of 1,370 ± 30 Ma with primary exposures in the eastern Arbuckle Mountains of southern Oklahoma. Within the SGR province three magmatic pulses can be identified starting at 1,400, 1,370, and 1,340 Ma. Although the crystallization ages are different, the Sm–Nd isotopic signatures are similar for the units exposed in these areas as well as the buried basement in between. Depleted mantle model ages for rocks within the Arbuckle Mountains range from 1,530 to 1,430 Ma with ɛ_Nd(t) values of +3.2 to +4.1 while units of the St. Francois Mountains range from 1,550 to 1,430 Ma and +4.5 to +4.7. Comparison of Sm–Nd isotopic data also indicate similarities between the ¹⁴⁷Sm/¹⁴⁴Nd and ¹⁴³Nd/¹⁴⁴Nd ratios for the rock units in these areas suggesting a common source.