西秦岭三叠系一个浊积岩序列金的地球化学特征

本文在详细分析沉积韵律、沉积构造、成分及粒度的基础上,论证了四川省若尔盖县阿西乡牙相一带上三叠统卡车组一套浊积岩沉积。通过对牙相浊积岩序列的２３个采自各浊积旋回各层段的系列样品的金分析,发现这一浊积岩序列具有：以泥质粉砂岩、泥质岩为主的鲍玛序列的Ｄ—Ｅ段与其上旋回的以含砾砂岩、粗砂岩为特征的Ａ段含金量呈线性关系,表明这两段之间元Ａｕ元素发生了循环,进一步揭示了浊积岩具有金的可迁移性这一矿源层的重要特征。另外,砂质单元金含量比细粒的粉砂岩和泥岩要高,从浊积岩序列的底部旋回至上部回金的含量降低并由不稳定到稳定     

海尔—波普彗星的CO（J=1—0）谱线的观测

使用紫金山天文台青海观测站13．7米毫米波射电望远镜,于1996年12月10日至1997年1月2日和1997年3月25日至1997年4月4日对海尔－波普彗星的CO分子J＝1—0转动跃迁谱线（频率为115．27120GHz）进行了观测．观测谱线表明,CO分子相对于地心的速度比彗星整体相对于地心的速度要小些,即有蓝移现象．这反映了CO分子是由该彗星迎着太阳的面以一定的速度产生出来的．从观测谱线中还初步估算了该彗星CO分子的产生速率．     

THE PALEOSEISMIC SURFACE RUPTURE AT SOUTH OF CENTRAL ALTYN TAGH FAULT AND ITS TECTONIC IMPLICATION

In this study, we described a 14km-long paleoearthquakes surface rupture across the salt flats of western Qaidam Basin, 10km south of the Xorkol segment of the central Altyn Tagh Fault, with satellite images interpretation and field investigation methods. The surface rupture strikes on average about N80°E sub-parallel to the main Altyn Tagh Fault, but is composed of several stepping segments with markedly different strike ranging from 68°N~87°E. The surface rupture is marked by pressure ridges, sub-fault strands, tension-gashes, pull-apart and faulted basins, likely caused by left-lateral strike-slip faulting. More than 30 pressure ridges can be distinguished with various rectangular, elliptical or elongated shapes. Most long axis of the ridges are oblique(90°N~140°E)to, but a few are nearly parallel to the surface rupture strike. The ridge sizes vary also, with heights from 1 to 15m, widths from several to 60m, and lengths from 10 to 100m. The overall size of these pressure ridges is similar to those found along the Altyn Tagh Fault, for instance, south of Pingding Shan or across Xorkol. Right-stepping 0.5~1m-deep gashes or sub-faults, with lengths from a few meters to several hundred meters, are distributed obliquely between ridges at an angle reaching 30°. The sub-faults are characterized with SE or NW facing 0.5~1m-high scarps. Several pull-apart and faulted basins are bounded by faults along the eastern part of the surface rupture. One large pull-apart basins are 6~7m deep and 400m wide. A faulted basin, 80m wide, 500m long and 3m deep, is bounded by 2 left-stepping left-lateral faults and 4 right-stepping normal faults. Two to three m-wide gashes are often seen on pressure ridges, and some ridges are left-laterally faulted and cut into several parts, probably owing to the occurrence of repetitive earthquakes. The OSL dating indicates that the most recent rupture might occur during Holocene.
Southwestwards the rupture trace disappears a few hundred meters north of a south dipping thrust scarp bounding uplifted and folded Plio-Quaternary sediments to the south. Thrust scarps can be followed southwestward for another 12km and suggest a connection with the south Pingding Shan Fault, a left-lateral splay of the main Altyn Tagh Fault. To the northeast the rupture trace progressively veers to the east and is seen cross-cutting the bajada south of Datonggou Nanshan and merging with active thrusts clearly outlined by south facing cumulative scarps across the fans. The geometry of this strike-slip fault trace and the clear young seismic geomorphology typifies the present and tectonically active link between left-lateral strike-slip faulting and thrusting along the eastern termination of the Altyn Tagh Fault, a process responsible for the growth of the Tibetan plateau at its northeastern margin. The discrete relation between thrusting and strike-slip faulting suggests discontinuous transfer of strain from strike-slip faulting to thrusting and thus stepwise northeastward slip-rate decrease along the Altyn Tagh Fault after each strike-slip/thrust junction.     

磁暴主相的經度不对称性

太阳带电粒子流通过磁边界层的中性点或阻塞点,由于极化电場的漂移运动或雷萊-泰勒（Rayleish-Taylor）不稳定运动,穿透磁层而进入地磁場被輻射带所捕获。这些被捕获的电子将向东漂移而形成西向电流。在它們围繞地球一周形成封閉的电流环以前,由于地球的自轉以及这个电流弧对地球各地的相对位置的不同,电流分布以及它在地面磁赤道附近所产生的磁場分布都将是不均匀的,对經度来耕是不对称的。本文假定电子繞地球的漂移周期为两天,計算了当磁暴开始时位于地方时00,06,12及18小时的台站記录的磁場随“暴时”T_st变化的曲线。理論結果与用佘山及洪伽幼地磁台站得到的統計結果是一致的。     

经向型持续性特大暴雨的合成分析

本文考察了10次经向型持续性特大暴雨,发现它们是由发生在能量锋前的中尺度强雨暴系统产生的。合成分析结果表明,在暴雨区北方和东方各有一阻塞高压,二者同时出现所构成的稳定大形势,是形成经向型特大暴雨的基本环流背景;和这二者相联系的高空副热带急流和低空偏南风急流,是产生暴雨的直接动力条件。它们既提供了形成暴雨所必需的能源,又造成了释放不稳定能量的启动条件;形势的稳定少变,又能使暴雨在同一地区数日维持。合成分析还说明,各种有利条件的组合必然使暴雨局限在一中尺度区域,以外的地区则不会同时具备发生暴雨的各个条件。     

基于VB可视化集成环境的测量学试题库管理系统研制

VB可视化集成开发环境以事件驱动、面向对象、图形用户界面等为特点 ,在设计试题库管理系统方面有着独特的优越性。本文通过测量学试题库管理系统的研制 ,对基于 VB建立试题库管理系统的一般方法 ,试题库的结构及功能模块、使用、特点进行研究。     

层次分析法在彩票抽奖方案选择中的应用

采用层次分析法对29种彩票抽奖方案进行排序,较为科学地解决了比较多种方案优劣程度的问题,得到了彩票抽奖方案选择问题的优化解.     

语义Web本体语言及OWL研究

面对Internet应用模式的变化和Web海量信息的冲击,Web信息个性化、智能化的研究不断深入.语义Web规划对当前的万维网进行扩展,期望用加入信息中的语义内容导航信息资源检索并提高网络服务的智能化,使机器自动与人协同工作.目前,虽然语义Web还是个理想模型,但将语义Web融入现有Web结构进行信息智能开发的初步努力已经展开.特别是随着对本体技术研究的日渐深入,OWL本体理论探索和应用开发逐渐受到广泛重视.     

基于整合理论的高校教师管理

整合理论实质就是对组织所拥有的资源进行优化配置,使其协调发展,产生最大效益.对于高校,教师是所拥有的不可缺少,最具有潜力的资源,这种资源所发挥的协同作用存在巨大的潜力.从整合理论的角度,分析了高校教师管理方面的整合问题,提出了高校教师管理过程中应该注意的问题.