鄂尔多斯北缘强震背景分析及未来地震趋势判断

基于鄂尔多斯块体的地质构造演变过程及历史强震活动规律,阐述南北地震带和龙门山断裂带强震时空分布规律对鄂尔多斯北缘的可能影响,对比分析鄂尔多斯其他3缘与北缘的地震活动.结果表明,青藏块体强震对鄂尔多斯北缘中强地震具有一定的触发作用;南北地震带中强以上地震的空间迁移特征表明,鄂尔多斯北缘将是未来中强以上地震的有利发震区域.2005年以来中小地震活动特征表明,鄂尔多斯北缘兼有Ms≥4.0地震平静和西北缘ML≥3.0地震活跃两种异常特征.综合地震地质背景和近期地震活动研究结果分析认为,今后一段时间鄂尔多斯北缘有可能发生中强以上地震.     

应用于MEMS加速度计的小型恒温系统的实现

介绍一种小型恒温系统的实现方法,使MEMS加速度计的工作区域温度保持恒定,从而改善MEMS加速度计的相关技术指标.小型恒温系统采用独特工艺,实现简单;恒温点可以根据环境温度的变化而改变,以降低功耗.实验结果表明,应用该系统的MEMS加速度计,由温度所引起的零点漂移值明显减小.     

冀东地区东梁金矿床地质特征及成因

东梁矿区位于冀东地区宽城凹褶束东南边缘。金矿床主要产于燕山期火成岩与中元古界长城系、蓟县系碳酸盐岩地层的接触带部位,受构造、岩浆活动控制。矿区岩(矿)石地球化学分析结果表明,成矿流体中的硫、铅主要来源于深部,与深部岩浆活动有关;氢、氧同位素分析结果显示,成矿流体主要来源于原生岩浆水;金矿床成矿温度125~305℃,成矿深度1.5km,成矿时代为燕山期火山活动晚期。认为在燕山期板块构造影响下,东梁金矿床成矿物质主要来源于深部活化变质岩系,属岩浆热液型中低温金矿床。     

Analysis on spatial distribution characteristics and geographical factors of Chinese National Geoparks

This study presents the Pearson correlation analyses of the various factors influencing the Chinese National Geoparks. The aim of this contribution is to offer insights on the Chinese National Geoparks by describing its relations with geoheritage and their intrinsic linkages with geological, climatic controls. The results suggest that: 1) Geomorphologic landscape and palaeontology National Geoparks contribute to 81.65% of Chinese National Geoparks. 2) The NNI of geoparks is 0.97 and it belongs to causal distributional patternwhose regional distributional characteristics may be best characterized as’ dispersion in overall and aggregation in local’. 3) Spatial distribution of National Geoparks is wide. The geographic imbalance in their distribution across regions and types of National Geoparks is obvious, with 13 clustered belts, including Tianshan-Altaishan Mountain, Lesser Higgnan-Changbai, Western Bohai Sea, Taihangshan Mountain, Shandong, Qilianshan-Qinling Mountain, Annulus Tibetan Plateau, Dabashan Mountain, Dabieshan Mountain, Chongqing-Western Hunan, Nanling Mountain, Wuyishan Mountain, Southeastern Coastal, of which the National Geoparks number is 180, accounting for 82.57%. 4) Spatial distribution of National Geoparks coincide with latitudinal tectonic zone and longitude tectonic zone of geological structure features, which is consistent with the areas around the Pacific Rim of volcanic tectonic zones. The coupling relationships are obvious between the spatial distributional pattern and the natural and geological conditions.     

基于S7核糖体蛋白基因部分序列的石鲈属鱼类分子系统进化关系

基于核DNA分子标记S7核糖体蛋白基因内含子1部分序列对分布于南海及美洲,非洲,大洋洲等周边海区的石鲈属鱼类11种,结合石鲈亚科其他属如仿石鲈属,异孔石鲈属,八带石鲈属及锯鳃石鲈属等21种鱼类的系统进化关系进行了研究分析。利用最大简约法以及贝叶斯法构建了系统进化树。进化树上,石鲈属的种类并没有形成一个单系,除了大斑石鲈,断斑石鲈等6种石鲈属鱼类聚成一石鲈属的分支外,其他石鲈属种类都位于进化树的不同位置。侧扁石鲈与八带石鲈聚在一起,大棘石鲈与异孔石鲈属聚在一起。红海石鲈与纵带石鲈与仿石鲈属的种类关系较近,佩氏石鲈最先分化出来,位于整个石鲈亚科分支基部。该分类关系与其各自的地理分布情况有着一定的联系。     

西藏墨竹工卡县过经拉矿区成矿条件 及找矿前景分析

西藏拉萨市墨竹工卡县过经拉矿区位于著名的冈底斯成矿带东段的北侧,是冈底斯成矿带北带的重要组成部分。近年来,冈底斯成矿带因其丰富的矿产资源日益受到国内外地质学者的广泛关注（侯增谦等,2003;李光明等,2004,2006,2009;杨志明等,2008;唐菊兴等,2009;佘宏全等,2009;肖波等,2011）。     

秦祁结合部位天水地区磨石沟变基性火山岩锆石U-Pb年代学、地球化学及其构造意义

秦祁结合部位天水地区新阳镇磨石沟新发现一套绿片岩相基性火山岩系,原岩为玄武岩,伴随有少量碳硅质岩和辉绿岩脉产出。磨石沟变基性火山岩SiO2含量为47.32%～50.18%,MgO含量为4.71%～7.33%,Al2O3含量(12.33%～14.97%)较低,TiO2含量为0.98%～1.98%(平均为1.44%),与洋脊玄武岩的Al2O3、TiO2含量相近,类似于E-MORB。∑REE为46.52×10-6～113.21×10-6,LREE/HREE为2.00～4.01,δEu为0.86～1.09(平均为0.98),(La/Yb)N为1.18～3.59。磨石沟变基性火山岩属于拉斑玄武岩系列,高场强元素及相关比值表明具有E-MORB特征,其岩浆源区为弱富集—富集地幔,岩石成分主要受岩浆熔融区控制,玄武质岩浆上升过程中遭受到不同程度的地壳物质或俯冲组分的混入,但地壳和俯冲带物质对岩浆源区和成岩过程的贡献较少。结合其地球化学性状与构造环境判别图解判断,磨石沟变基性火山形成于弧后盆地后期演化阶段。LA-ICP-MS锆石U-Pb测年结果表明其形成时代为中志留世Wenlock期(432.6±3.8Ma)。磨石沟变基性火山岩代表的弧后盆地的形成与中志留世"天水-武山"古洋盆向北的俯冲作用密切相关,说明秦祁结合部位早古生代构造格局是由一个较完整的洋-弧-盆体系组成。     

云雾室人造云雾控制及其技术发展

自然云雾是影响精确光学制导武器命中精度的重要大气环境因素,但由于自然云雾的不可再现性,科研人员很难对制导武器受其影响的程度进行研究。为了更好地评估精确光学制导武器装备的作战使用效能受云雾的影响,开展云雾室模拟自然云雾是非常必要的。在简要介绍国内外人造云雾研究现状、云雾实验室主要功能的基础上,对云雾室人造云雾过程中的喷雾、催化剂释放、温度、湿度、气流、照明等方面的控制进行了详细的介绍,并对人造云雾今后的发展趋势进行了探讨。     

Understanding the Surface Temperature Cold Bias in CMIP5 AGCMs over the Tibetan Plateau

The temperature biases of 28 CMIP5 AGCMs are evaluated over the Tibetan Plateau(TP) for the period 1979–2005. The results demonstrate that the majority of CMIP5 models underestimate annual and seasonal mean surface 2-m air temperatures(T_(as)) over the TP. In addition, the ensemble of the 28 AGCMs and half of the individual models underestimate annual mean skin temperatures(T_s) over the TP. The cold biases are larger in T_(as) than in T_s, and are larger over the western TP. By decomposing the T_s bias using the surface energy budget equation, we investigate the contributions to the cold surface temperature bias on the TP from various factors, including the surface albedo-induced bias, surface cloud radiative forcing, clear-sky shortwave radiation, clear-sky downward longwave radiation, surface sensible heat flux, latent heat flux,and heat storage. The results show a suite of physically interlinked processes contributing to the cold surface temperature bias.Strong negative surface albedo-induced bias associated with excessive snow cover and the surface heat fluxes are highly anticorrelated, and the cancelling out of these two terms leads to a relatively weak contribution to the cold bias. Smaller surface turbulent fluxes lead to colder lower-tropospheric temperature and lower water vapor content, which in turn cause negative clear-sky downward longwave radiation and cold bias. The results suggest that improvements in the parameterization of the area of snow cover, as well as the boundary layer, and hence surface turbulent fluxes, may help to reduce the cold bias over the TP in the models.     

广东河源白石冈岩体：一个高分异的Ⅰ型花岗岩

广东河源白石冈岩体位于近东西向展布的佛冈花岗岩带的东端,主体岩性为中粗粒黑云母花岗岩,主要组成矿物为石英(25%～35%)、微纹长石(45%～50%)、斜长石(An=20～30,15%～20%)和黑云母(5%～10%).锆石U-Pb定年结果表明其形成年龄为148.5±1.6 Ma,属晚侏罗世岩浆活动的产物.化学成分上,该岩体铝弱过饱和,A/NKC值主要变化于1.0～1.1之间;富硅,富钾(K2O/Na20=1.31～1.70),全碱含量中等偏低(K2O+Na2O=7.44%～8.48%),碱铝指数(AKI值)为0.75～0.88,可归为高钾钙碱性岩系.微量和稀土元素组成上,岩体富Rb、Th、U、Pb和轻稀土,贫Ba、Sr、P、Ti,Rb/Sr比值高,K/Rb比值低,铕负异常显著(δEu=0.05～0.28),Nb、Ta、Zr、Hf等高场强元素含量及104×Ga/Al比值(2.43～3.26)较之典型A型花岗岩均偏低.岩体的εNd(t)值为-5.99～-7.51,TDM值偏低(1.42～1.54Ga),综合地球化学资料指示其应属高分异的Ⅰ型花岗岩.结合对区域动力地质背景的全面分析,表明白石冈岩体形成于后造山的伸展引张环境,是由底侵的幔源基性岩浆及其诱发的长英质岩浆在深部岩浆房混合,并经高程度分离结晶的产物.