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本文简要介绍泉州市地震局依靠各级政府、有关部门和全社会的共同努力 ,以落实地震应急预案为楔机促进“预、防、救”三大体系工全面发展的工作经验 :一、以落实《地震应急预案》为抓手 ,争取项目 ,以项目带动一切 ;二、结合社会转型全面加大防震减灾知识宣传力度 ;三、不以经费的来源划分你我 ,动员全社会的力量建立健全预警应急机制。 相似文献
144.
沉积学的发展历程与未来展望 总被引:6,自引:0,他引:6
沉积学的概念自提出以来,其发展经历了:萌芽、初步形成、专业研究、总结提高、理论升华及学科渗透与综合 7个发展阶段,每一阶段都充分表现出,一方面受科学技术进步的影响,另一方面对全球经济的发展与进步又起到了不可忽视的推动作用,尤其是在各种沉积矿床和油气的寻找方面。随着地质勘探与开发实践的不断进行,已陆续在沉积体中发现了油气、煤、黄金、铀、金刚石、钾、水晶、铂、铝、锰、膏盐及天然气水合物等多种重要矿产,为全球经济的发展做出了不可磨灭的贡献。沉积学未来的发展在 7个方面表现出明显的规律性:层次上,由宏观向微观;方法上,由定性向定量;目的上,由理论向应用;形式上,由静态向动态;学科上,由单学科向多学科;手段上,由手工向计算机;领域上,由地区向全球发展的总体趋势。 相似文献
145.
藏南特提斯喜马拉雅带中段二叠纪-白垩纪的火山活动(Ⅰ):分布特点及其意义 总被引:12,自引:1,他引:12
在野外实地考察和追索的基础上,详细厘定了特提斯喜马拉雅带中段晚古生代以来火山岩的分布特点和迁移规律。结果表明,在特提斯喜马拉雅带中段晚古生代以来的地层系统中,从二叠纪→三叠纪→侏罗纪→白垩纪,共有11个层位含规模不等的火山岩,它们以透镜体、薄夹层或以块状玄武岩、玄武质安山岩等形式产出于不同地层系统中;从二叠纪→早中三叠世→晚三叠世→侏罗纪和白垩纪,具有由西向东、从南→北→南→北的迁移规律。这些火山活动的发现和厘定,对填补特提斯喜马拉雅带火山岩研究的空白,了解陆下岩石圈地幔和软流圈地幔之间的相互作用和新特提斯洋盆的形成演化都具有一定的指示意义。 相似文献
146.
阐述了大汶河流域洪涝灾害的特点,并对洪涝灾害发生的原因进行了分析,提出了预防为主、综合治理、系统防治和重点防治相结合、标本兼治的防治思路及具体防治对策. 相似文献
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B. Takano K. Suzuki K. Sugimori T. Ohba S. M. Fazlullin A. Bernard S. Sumarti R. Sukhyar M. Hirabayashi 《Journal of Volcanology and Geothermal Research》2004,135(4):299-329
A bathymetric survey of Kawah Ijen crater lake was conducted by acoustic sounding in 1996 to compare the lake morphology with those measured in 1922, 1925 and 1938, and to calculate the present lake volume. Even though the lake experienced several hydrothermal eruptions, the maximum depth became shallower (182 m) than before (200 m), resulting in a reduced lake volume (3.0×107 m3).Fifty-two major and minor constituents including rare earth elements and polythionates (PT) of the lake waters at various depths were determined by ICP-AES, ICP-MS and HPLC, respectively. These ions except for several volatile elements are taken up by lake fringe through congruent dissolution of pyroclastics of Kawah Ijen volcano. Most ions are homogeneously distributed throughout the lake, although PT showed a considerable vertical variation. Rare earth elements (REE) in the Kawah Ijen water as well as those from other hyper-acidic crater lakes show distribution patterns likely due to the three rock dissolution (preferential, congruent and residual) types, and their logarithmic concentrations linearly depend upon the pH values of the lake waters.Using the PT degradation kinetics data, production rates of PT, injection rates of SO2 and H2S into the lake were estimated to be 114, 86 and 30 tons/day, respectively. Also travel time of the spring water at the Banyupahit Riverhead from Kawah Ijen was estimated to be 600–1000 days through the consideration of decreasing rates of PT. Molten sulfur stocks containing Sn, Cu, Bi sulfides and Pb-barite exposed on the inner crater slope were presumed to be extinct molten sulfur pools at the former lake bottom. This was strongly supported by the barite precipitation temperature estimated through the consideration of the temperature dependence of Pb-chlorocomplex formation. 相似文献
149.
Perceptions of hazard and risk on Santorini 总被引:1,自引:0,他引:1
Dale Dominey-Howes Despina Minos-Minopoulos 《Journal of Volcanology and Geothermal Research》2004,137(4):4
Santorini, Greece is a major explosive volcano. The Santorini volcanic complex is composed of two active volcanoes—Nea Kameni and Mt. Columbo. Holocene eruptions have generated a variety of processes and deposits and eruption mechanisms pose significant hazards of various types. It has been recognized that, for major European volcanoes, few studies have focused on the social aspects of volcanic activity and little work has been conducted on public perceptions of hazard, risk and vulnerability. Such assessments are an important element of establishing public education programmes and developing volcano disaster management plans. We investigate perceptions of volcanic hazards on Santorini. We find that most residents know that Nea Kameni is active, but only 60% know that Mt. Columbo is active. Forty percent of residents fear that negative impacts on tourism will have the greatest effect on their community. In the event of an eruption, 43% of residents would try to evacuate the island by plane/ferry. Residents aged >50 have retained a memory of the effects of the last eruption at the island, whereas younger residents have no such knowledge. We find that dignitaries and municipal officers (those responsible for planning and managing disaster response) are informed about the history, hazards and effects of the volcanoes. However, there is no “emergency plan” for the island and there is confusion between various departments (Civil Defense, Fire, Police, etc.) about the emergency decision-making process. The resident population of Santorini is at high risk from the hazards associated with a future eruption. 相似文献
150.
新疆双峰山浅成低温热液金矿床特征与成矿机制 总被引:1,自引:0,他引:1
双峰山矿床位于新疆东天山北部西伯利亚板块陆缘晚古生代岛弧南部边缘,靠近克拉麦里板块缝合带.该矿区早石炭世浅海相玄武一安山质熔浆喷溢转为陆相流纹质熔浆喷发初期,火山热泉沿NW-NWW向线形管道(F2)形成以低Au品位硅质岩为中心的蚀变矿物晕(带);火山间隙性隐爆,潜火山热液于硅质岩裂隙间发育微细石英(冰长石)网脉,构成矿体.这两个成矿阶段同源同位的蚀变矿物晕(带)套叠,显示双峰山矿床蚀变分带与成矿模式,从上至下为隐爆硅质角砾岩化带、低Au品位硅质岩化带、石英(冰长石)网脉带(矿体)、黄铁矿蒙脱石化带和青磐岩化带.铅、硫同位素和稀土元素等研究表明,该矿床成矿流体与晚古生代岛弧早石炭世流纹质熔浆的陆相喷发相联系:火山热泉循环形成蚀变晕阶段加入大气降水,潜火山热液成矿阶段发育的低温微细石英网脉含冰长石和绢云母,它是一处晚古生代火山地区冰长石-绢云母型浅成低温热液金矿床。 相似文献