跨海高程传递方法的评价

针对跨海高程传递的最新进展,介绍了几种高程传递的实用方法,对优缺点和适用范围进行了分析与评价。初步试验结果分析表明,对于10km内的高程传递,几种方法均满足三等水准的精度要求,对于更远距离的跨海高程传递还需进一步研究。     

11年《海洋测绘》论文综述

针对2011年《海洋测绘》刊载的论文情况,从海洋测绘学科发展角度,通过对各专业论文发表情况的统计分析,对海洋大地测量、水深测量、潮汐观测与水位控制、海洋遥感应用、海图制图、卫星定位与导航等专业的发展现状,进行了归纳总结和简要评述。旨在为广大测绘工作者提供参考。     

土地定级估价的分析研究与实践——以新疆拜城县为例

近几年来,经济发展迅速,土地级别划分及地价水平已有较大的变化,原有的基准地价体系已不能适应现时经济发展的要求,地价体系也亟需修正更新。该文结合拜城县的具体情况,并遵循所选因子与土地的相关性,确定拜城县城区土地定级因素,在分析各定级因素权重的基础上,计算各因素的分值,划分土地等级。通过对拜城县城区的土地进行定级估价作出修正和更新,将对土地的监督管理工作起到良好的促进作用。     

1999-2007 年中国粮食安全的关键影响因素

选取耕地保护“新政”时期的1999-2007 年为研究时段,以耕地面积与粮食产量变化的分歧原因—耕地生产力变化为切入点,通过比较分析、空间与计量分析探寻粮食安全的关键影响因素。结果表明:农民种粮积极性变化决定着耕地集约利用是影响粮食安全的关键;2003-2007 年农民种粮积极性的持续提高主要来自市场粮价的上涨;粮食直补仅在开始实施的年份激发了农民对种粮收益的预期。此外,本文从提高农民种粮积极性、优化粮食生产投入及改进耕地保护模式3方面,提出了耕地保护发展的政策建议。     

Sedimentary characteristics of paleo-aeolian dune sands of Salawusu Formation in the Salawusu River Valley

The Salawusu Formation of Milanggouwan section in Salawusu River Valley in-cludes 7 layers of paleo-mobile dune sands, and 4 layers of paleo-fixed and semi-fixed dune sands. Their structures have been observed and their grain size, surface textural features and several main chemical elements have been analyzed. The results showed that: 1) Some of the aeolian structural characteristics of these dune sands are similar to that of the recent dune sands. 2) They are also similar to the recent dune sands in grain size components, and parameters of Mz, σ, Sk and Kg, as well as in several main chemical components. 3) The scattergrams of Mz-σ and SiO2–Al2O3+TOFE and the probability curves of grain size showed that these paleo-dune sands are different from paleosols and fluvio-lacustrine facies, but are consistency with recent dune sands. 4) Quartz sands have well roundness and surface textural features such as dish-shaped pits, crescent-shaped pits, pockmarked pits, upturned cleavage plates, siliceous precipitates and siliceous crevasses, indicating that they had been carried for a long time by the wind. As the 11 layers of paleo-dune sands possess the aeolian characteristics in structure, grain size, surface textural features and chemical elements, the origin of their formation should be attributed to eolation.     

Impact of the equivalent center of mass separating from the sliding surface on the isolation performance of friction pendulum bearings

A new equivalent center of mass model of FPBs(friction pendulum bearings) is introduced, and based on this model, coefficient j of the equivalent center of mass separating from the sliding surface is defined. It is thought in theory that j has a significant impact on the isolation parameter of FPBs, since the equivalent post-yielding stiffness and friction coefficients are not simply determined by sliding radius and sliding friction pairs. The results of numerical simulation analysis using ABAQUS conducted on two groups of FPBs support this viewpoint. For FPBs with the same sliding radius and sliding friction pairs, the FPB modules of structural analysis software such as ETABS could only distinguish the equivalent transformation using j one by one. The seismic response data obtained in a base isolation calculation example of FPBs are very different, which reveals that j's impact on the isolation effectiveness of FPBs cannot be ignored. The introduction of j will help improve the classical structural theory of FPBs and the weak points of structural analysis software based on this theory, which is important in achieving more accurate analyses in structural design.     

广东锡坪钼铜多金属矿床辉钼矿Re-Os同位素定年及其地质意义

广东锡坪钼铜多金属矿床位于钦杭成矿带的西南端,为一大型的斑岩型矿床。本文利用辉钼矿Re-Os同位素定年方法对锡坪钼铜多金属矿床4件辉钼矿样品进行了成矿年代学测定,获得的模式年龄为85.15~88.34Ma,加权平均值为86.1±2.3Ma,对应的等时线年龄为89.9±3.4Ma,模式年龄和等时线年龄结果在误差范围内基本一致,指示锡坪钼铜多金属矿床的成矿时限为晚白垩世。锡坪钼铜多金属矿辉钼矿样品的Re含量较低,表明其成矿物质可能主要来自于壳源。钦杭成矿带成岩成矿作用以中生代燕山期为主,存在180~150Ma、110~80Ma两个爆发期,两期成岩成矿作用可能均与太平洋板块的俯冲有一定的关系。锡坪钼铜多金属矿床是在岩石圈伸展减薄环境下发生的大规模成矿作用的产物。     

攀枝花大田铀矿床年代学特征及其意义

文章以康滇地轴典型热液型铀矿——大田铀矿床为研究对象,开展了围岩、构造蚀变带脉岩中的锆石和矿石晶质铀矿U-Pb法定年,以及年代学特征研究,获得如下认识:1)大田地区混合岩的原岩形成于晚元古代早期之前(900Ma);2)混合岩化作用发生于840~900Ma;3)铀矿区F3碱性构造蚀变岩带形成于混合岩化晚期(820~840Ma);4)大田铀矿床的成矿年龄为777Ma左右。因此笔者认为,康滇地轴的形成与发展、包括铀在内的成矿作用,是与罗迪尼亚大陆的形成及裂解演化所导致的构造岩浆作用密切相关。大田地区的构造演化对铀成矿具有重要的意义。     

诸广中段中山地区铀矿床地质特征及找矿潜力分析

文章简要介绍了诸广中段中山地区的地质背景,认为其具有较好的铀成矿地质条件。区内铀矿体具有"三层楼"式的空间分布特征,主要成脉状、透镜体状产出。铀矿石类型主要为碎裂岩型、硅质角砾岩型及微晶石英脉型。通过对控矿因素的详细分析,认为铀矿化受地层、岩体及其内外接触带和构造的多重控制,但以构造控矿为主,蚀变对矿化具有一定的影响;铀矿化富集中心深部及外围尚有较大的找矿空间,具备较大的找矿潜力,有望进一步扩大铀资源规模。     

南海南部陆坡晚第四纪沉积物稀土元素及环境意义

采用电感耦合等离子质谱(ICP-MS)法,对南海南部86GC柱状沉积物样品的稀土元素(REE)含量进行测量,并对其地球化学特征进行系统分析。结果表明,自大约31kaBP以来,该海域的沉积物具有基本相同的物质来源,物源区的气候环境变化可能是影响沉积物中REE指标纵向变化的主要因素。各指标的综合分析显示,末次冰期南海南部海域的沉积物源区具有较强的化学风化作用,冰后期则相对减弱,这就意味着南海南部及周边地区末次冰期期间依然盛行热带气候,冰后期的气候环境则可能较为多变。另外,在柱状样深度分别为17cm和100cm处均记录了指标的突变,前者可能是8k事件在南海南部的记录,后者代表的事件还有待进一步研究。