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本文对福建泉州地磁台白水营老址与丰州镇董埔村候选新台址,使用高灵敏度,快速记录的磁通门磁力仪,对台址周围观测环境进行了全面对比监测,从地磁短周期脉冲干扰,地磁场变化形态,日变幅、时均值相关分析等方面进行评估,指出老址的周围环境干扰量已超出0.1nT的<<地磁台站观测规范>>要求,新址符合<<地磁台站观测规范>>要求,适宜建立永久性地磁基本台。 相似文献
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分量质子旋进磁力仪观测误差分析 总被引:1,自引:1,他引:0
朱兆才 《地震地磁观测与研究》2000,21(2):48-53
分析了影响质子旋进磁力仪和分量质子旋进磁力仪观测质量的因素 ,给出了分量质子旋进磁力仪补偿线圈电流允许误差、补偿线圈定向 (特别是线圈磁南北方向 )应满足的关系式和定向允许误差。提出了分量质子旋进磁力仪的使用要点 相似文献
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地磁观测条件的特殊性决定了仪器观测室建设具有难度,本文介绍了大连地震台按照《地震及前兆数字指导规范(试行)》要求建设磁通门仪器室的过程及结果。 相似文献
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“九五”地磁数字化改造项目仪器配置分为两个部分,绝对观测仪-CTM-磁力仪和相对记录仪-GM3磁通门磁力仪,大连台自仪器装备以来,经过精心安装调试与观测摸索出一套仪器维护与高精度观测的经验,资料精度逐步达到规范要求,2001年11月9日通过验收,被专家组评价为“达到国内领先水平”。 相似文献
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Both magnetospheric and solid Earth geophysicists often employ two-dimensional arrays of recording variometers to reconstruct the spatial distribution of transient magnetic field variations at the Earth's surface. These discrete data are typically interpolated over a dense grid and the results, for example, are contoured. Few studies, however, have explored the efficacy of employing various polynomial forms for interpolating the same data set, nor have they examined how regional polynomial forms relate to magnetic variation sources on a global scale. The present study addresses some of these concerns. We quantify the characteristics of various smoothed models (i.e., low-order polynomial trend surfaces) for the same data set from a subglobal network of magnetic variometers. Using a relatively quiet interval of undisturbed diurnal variation, we characterize the spatial distribution of the three individual magnetic vector components at a single instant of time—or for what we call a ‘time slice’. We then explore how our model functions are affected by the presence or absence of various site data, i.e., what is the ‘information content’ of a particular site in our array and how important is it to constraining the final smooth model function that we derive? Finally, we explore how such local model functions are affected by including data from outside the array by studying the relation between our local polynomial forms and the global source fields from which they derive. 相似文献
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B. R. Arora 《Journal of Earth System Science》1990,99(4):693-716
Significant results from several array of magnetometers deployed in India to probe deep geoelectrical structures of the crust
and the upper mantle are reviewed in this paper. Emphasis is on critical appraisal of earlier results so that the article
summarizes what has been done so far and what caution is to be taken on future work.
Two large-scale arrays over northwest and peninsular India during 1979–80, have been followed up with six more linear or two-dimensional
arrays over different parts of the country.
“Trans-Himalayan” conductor aligned along the strike of Aravalli range, delineated by arrays over northwest India, essentially
represents one of the major continental induction anomalies mapped by electromagnetic methods. Efforts for quantifying the
induction effects through numerical models are shown to be constrained due to the large inter-station spacing, lack of information
on the regional background conductivity distribution and the non-inclusion of the frequency dependence of induction effects.
A more comprehensive modelling, not biased by these factors, enables approximating the Trans-Himalayan conductor as an asymmetric
domal upwarp in the middle and lower crust located between Delhi-Hardwar ridge and Moradabad fault. Numerical modelling results
for southern peninsular, despite the constraints, indicate that the strong and complex induction pattern can be adequately
attributed to the combination of conductors connected with triple junction between Indo-Ceylon Graben, Comorin ridge and the
west coast rifting.
Induction features derived from the Valsad array, operated over basalt-covered region of western India, demarcate an enhanced
conducting zone beneath Plume-associated triple junction in the Gulf of Cambay, apart from characterizing the presently active
seismic zone as a resistive block. 相似文献
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