地幔热柱成矿作用研究进展

地幔热柱构造是地球内部热传导的基本形式，只是地球的不同演化阶段其表现形式和强度有所不同。研究表明，燕山期强烈的地幔热柱活动沟通了深部成矿物质来源，金、银等元素随地幔热柱多级演化以气态→气—液混合相向上运移，在地幔热柱演化的三级单元——幔枝构造的有利部位聚集成矿。并据幔枝构造的成矿模式提出了华北地区燕山、秦岭、太行、胶辽等主要成矿集中区都是河淮地幔亚热柱控制下的幔枝成矿系列。成矿作用均伴随有强烈的构造—岩浆活动，成矿时代多集中在２６０～１２０Ｍａ。金、银多金属矿床具明显的相似性、同源性和深源性     

Structural condition assessment of long-span suspension bridges using long-term monitoring data

<正>This paper focuses on developing an online structural condition assessment technique using long-term monitoring data measured by a structural health monitoring system.The seasonal correlations of frequency-temperature and beam-end displacement-temperature for the Runyang Suspension Bridge are performed,first.Then,a statistical modeling technique using a six-order polynomial is further applied to formulate the correlations of frequency-temperature and displacement-temperature,from which abnormal changes of measured frequencies and displacements are detected using the mean value control chart.Analysis results show that modal frequencies of higher vibration modes and displacements have remarkable seasonal correlations with the environmental temperature and the proposed method exhibits a good capability for detecting the micro damage-induced changes of modal frequencies and displacements.The results demonstrate that the proposed method can effectively eliminate temperature complications from frequency and displacement time series and is well suited for online condition monitoring of long-span suspension bridges.     

配置630 MPa级高强钢筋的混凝土柱抗震损伤指数模型修正

为了验证各种Park-Ang损伤指数修正模型能否对630 MPa级超高强钢筋混凝土柱的地震损伤进行准确评估。在配置630 MPa级高强钢筋的混凝土柱拟静力试验现象和实测数据的基础上,首先利用6种模型分别计算了8根典型试件的损伤指数,并与试验实测损伤指数范围进行了对比,分析了6种模型的适用性;然后在试验实测数据的基础上,对计算结果存在较大偏差的4种模型进行了参数拟合和模型修正。研究结果表明:Kunnath模型、Chai模型、修正的傅剑平模型、修正的王东升模型和修正的付国模型均能准确模拟630 MPa级高强钢筋柱的损伤指数发展规律,而修正后的Kumar模型计算结果反而偏小,效果较差。     

Large-scale Circulation Control of the Occurrence of Low-level Turbulence at Hong Kong International Airport

This study identifies the atmospheric circulation features that are favorable for the occurrence of low-level turbulence at Hong Kong International Airport [below 1600 feet(around 500 m)]. By using LIDAR data at the airport, turbulence and nonturbulence cases are selected. It is found that the occurrence of turbulence is significantly related to the strength of the southerly wind at 850 h Pa over the South China coast. On the other hand, the east–west wind at this height demonstrates a weak relation to the occurrence. This suggests that turbulence is generated by flow passing Lantau Island from the south. The southerly wind also transports moisture from the South China Sea to Hong Kong, reducing local stability. This is favorable for the development of strong turbulence. It is also noted that the strong southerly wind during the occurrence of low-level turbulence is contributed by an anomalous zonal gradient of geopotential in the lower troposphere over the South China Sea. This gradient is caused by the combination of variations at different timescales. These are the passage of synoptic extratropical cyclones and anticyclones and the intraseasonal variation in the western North Pacific subtropical high. The seasonal variation in geopotential east of the Tibetan Plateau leads to a seasonal change in meridional wind, by which the frequency of low-level turbulence is maximized in spring and minimized in autumn.     

超压条件下的油藏地球化学特征

烃源岩成烃演化时，除了温度和时间的重要影响外，压力在油气生成演化过程中的作用也日益引起重视。压力对烃源岩中干酪根的热降解有阻滞作用，压力升高不仅使干酪根的化学键更稳定且不宜断裂，还使干酪根分子与烃源岩矿物结合更加牢固。通过歧北地区古近系深层超压油气藏研究，从油藏地球化学角度出发，较为细致的分析了超压条件下的油气生成、运移、聚集特征。     

镍锗尖晶石位错域的高温蠕变实验研究

利用人工合成的多晶材料研究了镍锗尖晶石在位错域的高温蠕变性质.多晶材料的颗粒尺寸约8μm.单轴压缩试件为圆柱状,使用气体介质围压筒.常压蠕变试验过程中,围压为300MPa,温度为1373—1523K,应力在55—330MPa范围内.从实验结果得出了镍锗尖晶石在位错域的流动律,应力指数n=29±01,表明流动的微观机制为位错蠕变.与其他尖晶石进行对比可以发现一个力学同构群,虽然在正尖晶石和反尖晶石之间存在一定的差异.在位错蠕变域,尖晶石与橄榄石归一化的强度类似.由于尖晶石的剪切模量比橄榄石高50%,其实际强度也比橄榄石高.将橄榄石和尖晶石的蠕变数据外推到地球内部条件时,由于其高应力指数,橄榄石则有可能比尖晶石的强度高.     

Tectonic ore-controlling in the middlesouthern segment of Da Hinggan Ling, Northeast China

1INTRODUCTION THEMIDDLE SOUTHERNSEGMENTOFDAHINGGANLING ISONEOFTHEIMPORTANTORE CONCENTRATEDAREASOFCHI NA.INRECENTYEARSGREATSTRIDESHAVEBEENMADEIN THEORETICALGEOLOGICALRESEARCHANDGEOLOGICALEXPLOITA TION(SHAOJI’ANETAL.,1998,1999;ZHANGLUQIAOET AL.,1998;XIAOCH…     

甲基卡矿区含矿伟晶岩堆积体成因初探及几点启示

甲基卡矿区是川西稀有金属资源量最丰富的地区之一,前人在矿区开展野外地质调查工作时,因矿区第四系覆盖严重,加之矿区所处自然地理环境十分恶劣,部分砾石中又见到磨光面、冰川擦痕等标志。因此,认为矿区出露的含矿伟晶岩堆积体是第四系冰碛物。然而,在对甲基卡矿区开展了细致的野外地质勘查工作后,结合堆积体分布形态、地形地貌特征、找矿勘探结果等证据,认为矿区含矿伟晶岩堆积体并非第四系冰碛物,而是伟晶岩原地堆积物。基于这一认识,不仅促使甲基卡矿区地质找矿工作实现了较大突破,而且为川西地区今后的地质找矿工作提供了新思路、新方向,值得深入总结和探讨。     

大尺度环境场对热带气旋影响的动力分析

应用常规气象资料、FY-2E卫星资料、加密自动站资料和NCEP FNL再分析资料, 对2012年8月3—4日辽宁持续性暴雨的成因进行了分析。结果表明：此次暴雨过程是在热带、副热带、西风带“三带”系统共同作用下出现的。副热带高压的稳定维持,三台风的共同影响利于水汽和能量向辽宁输送,是此次暴雨过程水汽充分、暖湿空气条件好的原因;高空急流右后方辐散与低层东南急流左前方辐合叠加区域长时间在辽宁中、西部维持,动力上升作用得以发展和维持;1210号台风倒槽在辽宁长时间停留,强降水区移动缓慢。鄂霍茨克海阻塞高压使得西风带和极地冷空气共同影响辽宁。暖湿、冷干空气长时间在辽宁作用,对称不稳定维持和对流不稳定快速重建,中尺度对流云团不断发展形成持续性暴雨。

     

波群对垂直桩柱的作用力

在波浪槽中进行了具有不同群因子和连长的随机波群对三种直径的桩柱作用力的实验研究,指出波浪峰力的比值不随波群的连长变化,而随波群因子的增加而增大。由于桩柱是一非线性系统,作用力的群团子大于波浪的群因子,其连长小于波浪的连长。波浪峰力的比值不仅随KC数的增加而增大,还随波群因子GF的增加而增大。