山西临汾太原大同盆地小地震活动A(b)-N法时序特征对比研究     

张瑞芳  梁向军  宋美琴  赵晓云  贾建喜  荆红亮 《山西地震》2005,(Z1):2-2

以山西临汾、太原、大同遥测地震台网记录的14 a的观测资料为基础,依据一定时期内地震活动的起伏性即发生的周期性、重复性、阶段性和密集平静等变化特点,运用A(b)-N法显示小地震活动的起伏现象适用于区域地震活动性分析的原理、计算机汇编程序,录入数据,计算得到了各盆地的地震活动性指标异常值,绘制了地震活动参数曲线,得到了预测未来发生地震的时间、空间、强度三要素的参考指标.通过与以前震例的对比分析,进一步得到运用此方法预测地震的可信度.  相似文献   

Isotopic evidence of TSR origin for natural gas bearing high H_2S contents within the Feixianguan Formation of the northeastern Sichuan Basin, southwestern China   总被引：9，自引：0，他引：9  

ZHU Guangyou  ZHANG Shuichang  LIANG Yingbo  DAI Jinxing & LI Jian Research Institute of Petroleum Exploration  Development  PetroChina  Beijing  China 《中国科学D辑(英文版)》2005,48(11)

Isotopic evidence of TSR origin for natural gas bearing high H2S contents 1961 As the hazardous component of natural gas, the ex-istence of H2S, due to its extremely strong toxicity and corrosivity, not only decreases the percentage of hy-drocarbon gas within natural gas and reduces its in-dustrial value, it also threatens each aspect of drilling and exploitation. It frequently causes serious safety accidents[1] and leads to the E&P cost and risk of natural gas with higher H2S contents be…  相似文献   

Studies on wind environment around high buildings in urban areas     

LIU Huizhi  JIANG Yujun  LIANG Bin  ZHU Fengrong  ZHANG Boyin  SANG Jianguo 《中国科学D辑(英文版)》2005,48(Z2)

High buildings or architectural complex in urban areas remarkably distort the urban surface wind fields. As the air flow approaches,local strong wind may appear around the buildings. The strong wind makes the pedestrians on sidewalks, entrances and terrace very uncomfortable and causes the pedestrian level wind environment problem. In this studies, hot-wire wind measurement, wind scouring in wind tunnel and numerical computation were carried out to evaluate the wind environment of tall buildings in the prevailing flow conditions in Beijing areas. The results obtained by three techniques were compared and mutually verified. The conclusions drawn from three approaches agree with each other. Also the advantages and limitations of each method were analyzed. It is suggested that the combination of different techniques may produce better assessment of wind environment around high buildings.  相似文献   

深基坑支护方案的分析与优化   总被引：3，自引：0，他引：3  

尹双  张仲先  王勇 《岩土工程技术》2005,19(3):152-154,F003

针对武汉市南湖岸边复杂的地质条件及周边环境,在某高层建筑的深基坑支护结构设计中,结合实际因地制宜地对基坑的支护方法进行了分析比较。支护效果及实测数据表明,该工程所采用的混合式支护实施方案技术安全可靠,经济合理,可为同类型基坑工程设计提供借鉴。  相似文献   

金龙——丘岭金矿床成矿流体的储运规律及区域找金方向     

刘新会 刘爽李渊  魏宽义 《地质找矿论丛》2005,20(8):10-14

金龙山——丘岭金矿区含金矿源为层上泥盆统南羊山组和下石炭统袁家沟组。组成含金矿源层岩石为高频互层的细碎屑岩-碳酸盐岩，其中细砂岩、粉砂岩、碳酸盐岩含成矿流体物性较好．页岩、板岩含成矿流体物性较差，构成屏蔽层。金鸡岭Ⅰ级复式向斜控制着金、砷、锑等异常范围；松枣Ⅱ级复式背斜控制着金的矿化带；金龙山-丘岭金矿Ⅲ级背斜控制着金的矿（化）体；镇安——板岩镇断裂的次级断裂是金矿化体的容矿有利位置。在成矿过程中，构造变形与成矿流体的形成、运移及储集密切相关。其规律是：①原生构造导致成矿流体的初次聚集。②第一期构造变形导致成矿流体的聚集。③第二期构造变形导致成矿流体运移及金矿床形成。此期变形是金的主要成矿期。④第三期构造变形使成矿流体进一步聚集和金矿体的富集。⑤第四期构造变形是石英方解石脉的形成时期。总结出矿床形成模式。据此提出了在4种不同的构造部位找金的方向。  相似文献   

城市旅游形象塑造与传播策略     

梁海燕 《亚热带资源与环境学报》2005,20(4):40-42

城市旅游形象是当今城市旅游发展的热点探索领域,城市旅游形象的塑造和传播是城市旅游的生命力所在,是促发人们前来旅游的动力,也是城市旅游发展的战略制胜点.在分析城市旅游形象塑造原则的基础上,探讨借助于多样化的手段,形成全方位的立体传播网络,使城市旅游保持长久的吸引力.  相似文献   

湖南寒武系第三统混积岩沉积特征与成因探讨     

梁薇  牟传龙  周恳恳  王瑞华  葛祥英  徐鹏辉  郑斌嵩  谭志远 《地质论评》2016,62(4):881-896

湖南地区寒武系第三统发育大量的混积岩及混积层系,其沉积特征、成因及时空分布,对研究寒武纪中上扬子地区东南缘的沉积环境及碳酸盐台地的形成演化具有重要的意义。本文采用野外观察、微观岩石学分析方法对混积岩时空分布、沉积特征、矿物组分进行了研究,首次系统总结了湖南地区寒武系第三统发育的混积层系类型与组合方式,及其分布的6类不同的岩相分区,并按照成分分类依据划分出4种混积岩类型。研究表明,混积岩分布在湘西北地区及湘中地区,靖州—涟源—隆回—宁乡一线以北的区域。混积层系的沉积特征表明,其形成于受周期性强风浪、风暴作用影响的浅水混积陆棚环境或风暴浪基面以下的深水混积陆棚环境,主要成因为机械成因的相缘渐变沉积混合及事件突变沉积混合。混积陆棚的存在,表明寒武纪第三世时期,中上扬子东南缘湘西北地区不发育台缘相带,未建立起完整的镶边碳酸盐台地模式,而为相对平缓的碳酸盐岩为主的浅海混积陆棚模式,混有碎屑岩沉积物。  相似文献   

Spatial variations in immediate greenhouse gases and aerosol emissions and resulting radiative forcing from wildfires in interior Alaska     

Shengli Huang  Heping Liu  Devendra Dahal  Suming Jin  Shuang Li  Shuguang Liu 《Theoretical and Applied Climatology》2016,123(3-4):581-592

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Characteristics of the two active stages of lightning activity in two hailstorms   总被引：1，自引：1，他引：0  

徐爽  郑栋  王咏青  胡鹏宇 《Acta Meteorologica Sinica》2016,30(2):265-281

Two hailstorms that occurred in Beijing and Tianjin, respectively, are investigated, based mainly on the total lightning data observed by the System d’Alerte Fondre par Interferometric Radioelecctrique (SAFIR3000), the cloud-to-ground (CG) lightning data of a CG lightning location system, and the echo data of a Doppler radar. Both hailstorms exhibited two lightning frequency peaks: the first was before the hailfall and the second was after the hailfall, with the second peak greater than the first. The dominant polarity of the CG lightning was positive in the stage around the first frequency peak, but changed to negative in the stage around the second frequency peak. The evolution of radar echoes and the height distribution of lightning radiation sources are explored, revealing that both hailstorms had stronger convection and the main positive charge occurred at mid levels during the stage around the first frequency peak. However, whilst the Beijing hailstorm experienced the enhancement of convection, with the main positive charge at upper levels around the second frequency peak, the Tianjin hailstorm generated its second frequency peak during the period when the convection kept weakening and the main positive charge dropped to mid–lower levels. Through evaluation of the radar parameters, we investigate the mechanisms responsible for the second stage of active lightning discharge. Furthermore, the lightning activity exhibited a close relationship with radar echo parameters and hailfall. Lightning jump signals were found before the hailfall and were associated with the change ratio of the 40-dBZ echo volume above the ?15°C level, which demonstrates the application value of lightning data in severe weather warning.  相似文献   

南京市灰霾天气的长时间变化特征及其气候原因探讨          下载免费PDF全文

吴丹  于亚鑫  夏俊荣  龚宇麟  刘刚  李凤英  杨孟  曹双 《大气科学学报》2016,39(2):232-242

以南京市1954—2012年的逐日气象数据分析南京市灰霾天的长时间变化规律并从气候角度探讨其变化原因。南京市的霾日数近60 a来呈现明显上升趋势,从20世纪50年代的40 d/a已增加至21世纪的230 d/a左右,气象行业标准界定的霾日与人工观测的霾日长期变化趋势一致,前者在南京市具有较好的适用性。南京市雾霾混合日呈现出先增加后下降的趋势,其对应的相对湿度在不断降低,这可能是雾霾日向霾日转换,雾霾日数降低而霾日数增多的关键因素。南京地区能见度不断降低,近30 a里约下降8.4 km,霾日数与能见度相关系数高达-0.91,随着能见度的降低,灰霾天数几乎线性增加。南京地区的年平均相对湿度在1985年以后大幅降低,已从约80%下降至68%左右,湿度与霾日的相关系数为-0.72,随着湿度的降低,霾日呈上升趋势。南京年平均温度1985年后明显上升,升高了1.8℃,其中冬季上升幅度最大,夏季上升幅度最小;年均温度与霾日数呈现出明显正相关,和相对湿度呈现明显负相关,温度的升高将造成相对湿度的降低,进而造成霾日增多。南京的年平均风速1978年后不断降低,到20世纪末约降低1.5 m/s,风速与霾日呈现出显著的负相关,随着平均风速的降低,霾日数不断增多。在全球变暖的大气候背景下,南京市霾的长时间变化受到各种气候因子的影响,能见度、相对湿度、温度和风速都是重要的影响因素。  相似文献