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使用长周期大地电磁测深网 (Network -MT)等技术 ,在长春和三岔河等地对太平洋板块弧后的上地幔电导率结构进行了探测。用陆地电话线或电缆接收长基线的电场 ,由设置在长春地磁台的三分量磁通门磁力仪记录磁场变化 ,得到Network -MT等观测资料的最长周期可达 10 5～10 6 s,反演结果的深度可达约 10 0 0km。 1)在两个区的 10 0～ 2 0 0 ,30 0 ,50 0～ 6 0 0km深度附近存在电性间断面 ;2 )长春测区的 850km深度存在电性间断面 ;3)平滑模型的电导率随深度增大而单调增加 ;4 )三岔河测区 6 0 0km深度、长春测区 850km深度的电导率达到 1S/m。上述结果表明 ,地幔内存在不连续界面和不均匀性 ,有些结果可与岩石学的研究结果对比 相似文献
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利用1957—2012年长春地磁台地磁观测数据资料对长春地磁台地磁场的长期变化进行分析研究,系统地总结了长春地磁台地磁场长期变化的规律,揭示了长春地磁台地磁场是以波峰波谷,波浪式的缓慢递增和递减趋势,存在一定的周期性。 相似文献
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为准确评价地下水污染质空间分布,本文以长春地区地下水重要组分NO3-为例,利用统计学的熵—矩检验法对长春地区2008年56个水质采样点的检测数据的概率分布进行了检验,得出数据不服从正态分布的结论.在此基础上,选择不要求总体服从正态分布的非参数Kruskal-Wallis检验方法对长春地区所属的各个行政子区域地下水中的N... 相似文献
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长春地震台地电供电系统对地磁观测影响的试验分析于凯锋（吉林省地震局长春１３００２２）主题词：地磁测量，大地电流，干扰分析１前言长春地震台的地电和地磁两种观测手段建在一起，观测结果表明地电供电系统对地磁观测造成了不同程度的干扰。主要干扰表现为ＧＳＩ仪器... 相似文献
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正还鱼儿一片干净的荷塘,还市民一条清澈的河流。"灭黑消臭"是近来公众关注的一大焦点。2016年初至今,已经有30余个城市公布了黑臭水体排查清单,纷纷将黑臭水体整治作为今年的重点工作。长春:整治37处黑臭水体吉林省长春市政府近日印发《长春市落实水污染防治行动计划工作方案》(长府发〔2016〕4号)。长春将以改善水环境质量、保障饮用水安全为核心,全面启动水污染防治工作。计 相似文献
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从地质构造、波列特征、S-P到时差、震中距、主要震相、震源深度等方面对长春地震台2000年以来记录到的国内5级以上地震进行分析研究,总结出国内不同区域地震在长春地震台的波形记录特征和分析方法。 相似文献
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<正>0全球火山活动概况2022年10—12月全球共有67座火山出现活动,其中,警戒级别Ⅰ级的火山15座,警戒级别Ⅱ级的火山21座,警戒级别Ⅲ级的火山27座,警戒级别Ⅳ级的火山4座(表1)。从空间分布上看,绝大多数活动火山位于环太平洋火山带上,少数分布在地中海火山带西南段,个别活动火山处于板块交汇处和板块内部(图1);从分布国家来看,活动火山多集中在美国、俄罗斯、印度尼西亚、日本等国;“一带一路”沿线有7座火山出现活动,其中,印度尼西亚5座,意大利2座。2022年10—12月全球火山活动水平有所减弱, 相似文献
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A study is presented of spectral features of volcanic tremor recorded at Mount Etna (Sicily, Italy) following the methods of analysis suggested by the resonant scattering formalism of Gaunaurd and Überall (1978, 1979a, 1979b) and the model for hydraulic origin of Seidl et al. (1981). The periods investigated include summit and flank eruptions that occurred between 1984 and 1993. Recordings from a permanent station located near the top of the volcano were used, and the temporal patterns associated with (a) the average spacing (
) between consecutive spectral peaks in the frequency range 1–6 Hz, (b) the spectral shape and (c) the overall spectral amplitude were analyzed.
values are thought to depend on the physical properties of magma, such as its density, which, in turn, is controlled by the degree of gas exsolution. Variations in the spectral shape are tentatively attributed to changes in the geometrical scattering from the boundary of resonant conduits and magma batches. Finally, the overall amplitude at the station should essentially reflect the state of turbulence of magma within the superficial ascending path. A limit in the application of the resonant scattering formalism to the study of volcanic tremor is given by the fact that the fundamental modes and integer harmonics are difficult to identify in the frequency spectra, as tremor sources are likely within cavities of very complex geometry, rather than in spherical or cylindrical chambers, as expected by theory. This study gives evidence of some correlations between the analyzed temporal patterns and the major events in the volcanic activity, related to both lava flow and explosions at the summit vents. In particular, relatively high values of
have been attained during the SE crater eruption of 1984, the complex eruptive phases of September–October 1989 and the 1991–1993 flank eruption, suggesting the presence of a relatively dense magma for all of these events. Conversely, very low values have been recorded in coincidence with the December 1985 activity and the paroxysmal explosions at the summit craters of early 1990, which are interpreted here as fed by fluid-vesiculated magma. Appreciable modifications in the spectral shape have been observed in relation to changes of the volcanic activity that probably preceded the opening and disactivation of shallow dykes or magma batches. Finally, the overall amplitude seems to be a sensitive indicator of the state of gas turbulence within the shallow conduits, as is suggested by the high values attained during phases of intense volcanic activity. 相似文献