新一代天气雷达检修的技术与方法

对新一代天气雷达发生故障的基本原因进行了总结和分类,阐述了检查、分析与排除故障的步骤、方式和方法,并介绍了分析故障的一些技巧。通过对CINRAD/SC型天气雷达一次故障检修个例的分析,进一步对以上技术方法在实际工作中的应用加以说明。目的是希望技术人员在检修新一代天气雷达过程中能严格遵守雷达故障分析的原则,灵活运用故障的诊断方法和技巧,达到事半功倍的效果。     

中朝地块与扬子地块碰撞的时限与方式—长江中下游地区震旦纪一侏罗纪沉积环

古陆碰撞继之为海洋盆地关闭、山脉隆起和前陆盆地巨厚碎屑岩系的堆积。造山带的前陆地区，前身是被动陆,构造上位于较低的部位，其地质记录可以保存得相对完整。长江中下游地区，是大别造山带的前陆构造带。通过对那里沉积物形成环境，特别是物源区的分析研究，识别出震旦系至下三叠统被动陆缘沉积岩系和中三叠统至中侏罗统前陆盆地沉积岩系，据此推测大别造山带碰撞造山作用发生在中三叠世。早三叠世被动陆缘岩系和前陆盆地堆积物的空间分布，揭示出中朝与扬子两个地板之间的碰撞方式，在长江中下游地区从东到西基本是同时的。     

新疆东部哈尔里克山闪长岩锆石SHRIMP U-Pb定年及其地质意义

新疆东部哈尔里克山出露大量闪长岩和花岗岩岩体。一般认为,该区晚古生代岩浆活动中,闪长岩形成比较早,花岗岩形成比较晚。对其中一个闪长岩中的锆石进行SHRIMP U-Pb定年,获得了316±3 Ma的206Pb/238U表面年龄。结合岩体及锆石的矿物学特征,该年龄被解释为代表了哈尔里克山晚古生代岩浆初始侵入活动的时间。通过与前人从博格达山和哈尔里克山获得的岩浆活动年代学资料的比较研究,得出的结论是博格达山与哈尔里克山晚古生代岩浆初始侵入活动的时间大体相同,都发生在该区地壳形成演化的后碰撞阶段;由此进一步推论哈尔里克山晚石炭世期间的构造背景与博格达山基本相同,为与康古尔塔格一带洋岩石圈板块向北俯冲有关的板缘伸展环境下的滞后弧后盆地或者是后碰撞伸展环境下的火山沉积盆地。     

2008年度地球化学领域项目评审与成果分析

1 2008年度项目受理申请和同行评议情况 2008年度面上项目、青年基金和地区基金申请项目共458项,较2007年度增长23.78%.面上项目申请314项(占地球科学部申请项目的9.2%),较2007年增长23.6%;青年基金申请项目134项(占地球科学部申请项目的7.1%),较2007年增加28.85%;地区基金申请项目10项(占地球科学部申请项目的6.0%),较2007年减少2项.     

新疆阿尔泰蒙库铁矿床的辉钼矿Re-Os年龄及意义

蒙库大型铁矿位于阿尔泰南缘麦兹盆地,赋存于晚志留世-早泥盆世变质火山-沉积岩系中,容矿岩石为石榴石矽卡岩、变粒岩、浅粒岩和大理岩.矿体总体顺层分布,空间上与矽卡岩密切相关.对1号矿体含黄铁矿辉钼矿石英大脉中辉钼矿Re-Os同位素年代学进行了研究,7件样品的Re-Os同位素模式年龄为(261.6±3.7)～(264.0±...     

关于雅鲁藏布江缝合带(东段)的新认识

国内外不少地质学家大都将雅鲁藏布江蛇绿岩带视为印度板块与亚洲板块之间的缝合带。但是,笔者等在喜玛拉雅造山带的东段即仁布-康马一线以东地区的研究却发现,在雅鲁藏布江蛇绿岩带的南侧发育着一个宽大的增生杂岩体,它与雅江蛇绿岩是同一大洋即特提斯喜玛拉雅洋俯冲消减的产物,前者代表着特提斯喜玛拉雅洋消亡遗迹的主体,是印度板块与拉萨地块之间缝合带的主要组成部分;而后者代表的是俯冲带与拉萨地块之间的残余洋壳,它由北向南仰冲,构成日喀则-桑日弧前盆地前缘脊和南部基底,因而其不代表主缝合带。北喜玛拉雅增生杂岩体的发现改变了以Gansser(1964)为代表提出的喜玛拉雅造山带的构造模式,为重新审视印度板块与拉萨地块缝合作用过程提供了一个重要的地质制约和新的研究途径。     

First record of the Eurasian jaguar in southern Asia and a review of dental differences between pantherine cats

Felid material from the middle Early Pleistocene Haro River quarry, northern Pakistan, is described. Most of the material is referred to the Eurasian jaguar, Panthera gombaszogensis georgica, representing the first record of the jaguar in southern Asia. A systematic review of dental morphology of all living species of Pantherinae is made to provide a better background for studying the evolution of pantherine cats. A renewed dispersal scenario of the jaguar in Eurasia is provided. Panthera gombaszogensis georgica is suggested to be a distinct subspecies distributed in central, western and southern Asia during the Early Pleistocene, characterized by relatively small body size and slender dentition. The Eurasian jaguar does not possess the derived dental characters of the living jaguar Panthera onca (e.g. weak or no canine vertical groove, robust premolars), and presumably did not specialize on hard-shelled prey, and therefore should be viewed as a distinct species from the living P. onca. Two additional felids from the Haro River Quarry, the large sabre-toothed felid? Megantereon sp. and a small undetermined feline, are also reported. The Felidae faunal composition of southern Asia during the Early Pleistocene is generally similar to that of northern Eurasia, and the paleoenvironment is probably slightly more closed.     

CINRAD/SA雷达数字中频改造技术难题及解决方法

2008年以来,济南CINRAD/SA雷达由于模拟中频接收机系统性能参数退化导致雷达运行的可靠性和稳定性较差,且故障率较高。为了更好的保障雷达服务于气象,2009年7月济南完成数字化中频升级改造工程,改造后的数字中频雷达相位噪声非常稳定,速度信息量更加可信和精确。扼要介绍了数字中频接收机的工作原理,主要是对数字中频安装调试及改造过程中遇到的软、硬件问题的解决措施和改造后的技术参数测试进行技术性的总结,旨在对同行今后的工作具有参考借鉴价值。     

一种土颗粒体微结构特征的描述方法

在前期工作基础上,采用相关分析和主成分分析方法,对三种土的SEM照片特征块原始微结构参数进行了相关分析和主成分分析。研究表明,与域微结构参数一样,特征块微结构参数间也存在“严重”的“信息重复”现象,可以用较少主成分反映全部原始特征块微结构参数的主要信息,从而达到降维目的。     

How did the Alxa Block respond to the Indo-Eurasian collision?

The Cenozoic deformation of the Alxa Block resulted directly from the evolution of the northern Qinghai-Tibetan Plateau. However, many data show that the deformation occurred only in the Middle-Late Miocene. Our studies show that the Altyn Tagh fault did not pass through the Alxa Block; on the contrary it went along the southern boundary of the Jintai-Huahai Basin, linking with the Helishan—southern Longshoushan fault. Due to important tectonic events in the northern Qinghai-Tibetan plateau during the Middle-Late Miocene time, the northern plateau underwent rapid uplift and the plateau compressed the Hexi Corridor Region, resulting in a change from NS-trending to EW-trending structures in the Jinta-Huahai basin, and in the development of compressive structures in the Beishan. The southern Alxa fault underwent right lateral movement, and in the northern and central parts of the block, NS-trending Tertiary extensional structures formed. These basins controlled by Tertiary faults are similar to basins developed by lateral extrusion with a strong foreland and weak limited boundaries. The authors suggest that a regional “conjugate” fault system resulted from nearly NS-trending compression from the Qinghai-Tibetan Plateau during the Miocene and Pliocene in the Alxa Block and southern Mongolia. And due to the control of early structures in these regions, most brittle faults reactivated earlier ductile faults; NW–SE faults along the Altai Mountain and NE–SW faults to the southeast in Mongolia consist of a “conjugate” fault system to the north. The Altyn Tagh fault and southern Helishan-Longshoushan fault comprise a “conjugate” fault system to the south. The Beishan and Jinta-Huahai Basin occupied the convergent area between these two sets of faults; the compression controlled the Tertiary deposition and led to the development of the Cenozoic Jinta-Huahai Basin. The Alxa Block bounded by these two sets of faults moved eastwards, which resulted in the development of Cenozoic compressive structures to the west of Helan Shan, and superimposed early ductile shear zones along the northeastern and southwestern boundaries of the Alxa Block respectively. This model could explain the Cenozoic deformation occurring in and around the Alxa region.