- 更多网络例句与地磁相关的网络例句 [注：此内容来源于网络，仅供参考]
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To measure the horizontal component of geomagnetism , the "bifilar balance method" is used, together with an additional adjustable magnetic field to compensate the geomagnetic field.
采用"双悬线平衡法"，并利用外加可调磁场与地磁水平分量补偿的方法对地磁水平分量进行了测量。
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Using the observed data obtained from stations all over the world and the related interplanetary and geomagnetic material, we study the response of global ionospheric F〓-layer parameter NmF〓 and hmF〓 to five typical different type geomagnetic disturbance events induced by different interplanetary magnetic cloud, by dividing the global ionosphere into high, middle and low latitude a ccording the variations of magnetic latitude, and adopting the UT/LT (universal time /local time) method.
利用全球电离层台站提供的观测资料及有关行星际、地磁观测资料，根据磁纬变化将全球分成高、中、低纬三个不同的区域，并采用了UT/LT的方法，分析了全球电离层F2层参数NmF2和hmF2对于五次由不同行星际磁云引起的不同类型地磁扰动事件的响应。
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And the corresponding geomagnetic field charts and geomagnetic anomaly charts are drawn.
并绘制相应的地磁图和地磁异常图。
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Magnetic meridian: The direction of the horizontal component of the earth's magnetic field; the direction of magnetic north.
地磁子午线：地球磁场的水平分量方向；地磁北极方向。
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Based on the criterion of reliability of paleomagnetic data, we report the paleomagnetic data of Tarim, which was our achievement in past 10 years. Combined with the paleomagnetic results of other researchers, an integrated paleomagnetic data of Tarim, since Phanerozoic, is published here.
本文依据古地磁数据可靠性判别国际公认的一些基本原则，积集作者近年来在对塔里木盆地研究中获得的古地磁新成果，并结合其他学者发表的古地磁数据，编制了塔里木盆地显生宙以来的古地磁综合数据表。
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According to the three component absolute survey data of 118 geomagnetic stations observed during 1998~2000 and 39 geomagnetic observatories and IGRF 2000, the spherical cap harmonic models of the geomagnetic field for 2000 (the truncation order is 8), and the geomagnetic secular variation for 2000~2005 (the truncation oder is 6) are calculated.
根据1998～2000年完成的118个地磁测点和39个地磁台的三分量绝对测量资料以及IGRF2000，计算2000年中国地磁场冠谐模型（截断阶数为8），以及2000～2005年中国地磁长期变化冠谐模型（截断阶数为6）。
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According to the geomagnetic 3 component absolute survey data of China for 1950～1990, and using the method of spherical cap harmonic analysis, this study calculates the spherical cap harmonic models of the geomagnetic residual field in China for 1950～1990 and draws corresponding residual maps.
根据中国1950、1960、1970、1980年和1990年地磁三分量绝对测量资料，使用球冠谐和分析方法，分别计算1950～1990年各个年代中国地磁剩余场冠谐模型。
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Based on the spherical cap harmonic models of the geomagnetic field and its secular variation, the geomagnetic charts, the anomaly charts for 2000 and the secular variation charts for 2000~2005 are drawn.
依据地磁场及其长期变化的冠谐模型，分别绘制2000年中国地磁图和异常磁场图，以及2000～2005年地磁长期变化图。
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Based on the geomagnetic survey data in the eastern and central region of China for 1936, and DGRF1935 and DGRF1940, using the method of spherical cap harmonic analysis, the spherical cap harmonic model of the Chinese geomagnetic reference field for 1936(CGRF1936) is calculated.
根据 1936年中国东部和中部地区的地磁测量资料，以及国际地磁参考场DGRF1935和DGRF194 0 ，用冠谐分析方法计算 1936年中国地磁参考场的冠谐模型。
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Refer to the research findings of CHengDu Research Institute of Geosciences and Minerals(1990) and Nanjing Research Institute of Geography and Lake of Chinese Academy of Sciences(1989), according to the Guidebook of China Stratum(2000), the chronostratigraphy of Kunming Basin is divided into 4 age: the bottom of the Quaternary corresponding to M/G Boundary, age is 2.6Ma;the Bottom of the Mid-Pleistocene corresponding to B/M Boundary, age is 0.78Ma;the Bottom of the Upper-Pleistocene corresponding to the Blake event, age is 0.128Ma;the Bottom of the Holocene corresponding to the Gothenburg event,age is 0.012Ma.
本次研究获得了大量的测年数据，参考成都地质矿产研究所(1990)及中科院南京地理与湖泊研究所(1989)等的研究成果，按照中国地层指南(2000)的方案，厘定了昆明盆地第四纪年代地层划分：第四系底界对应古地磁松山反向期与高斯正向期界线处，年龄为2.6Ma；更新统中部底界对应古地磁布容正向期与松山反向期界线，年龄为0.78Ma；更新统上部底界对应古地磁布莱克事件附近，年龄约0.128Ma：全新统底界对应古地磁哥德堡事件附近，年龄约0.012ma。
- 更多网络解释与地磁相关的网络解释 [注：此内容来源于网络，仅供参考]
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polarity chron：地磁极性期,地磁极性时
极性 polarity | 地磁极性期,地磁极性时 polarity chron | 极性反向 polarity reversal
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geomagnetic：地磁的
geomagnetic time scale 地磁年代表 | geomagnetic 地磁的 | geomagnetism 地磁
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geomagnetic：地磁 地磁的
geologysteeltube 地质钢管 | geomagnetic 地磁 地磁的 | geomagneticactivity 地磁活动
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geomagnetic electro kinetograph：电地磁流量计
地磁海流计 geomagnetic electro kinetograph | 电地磁流量计 geomagnetic electro kinetograph | 地磁要素 geomagnetic element
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geomagnetic electro kinetograph：地磁电流量计地磁海流计电地磁流量计
地磁的 geomagnetic | 地磁电流量计地磁海流计电地磁流量计 geomagnetic electro kinetograph | 地磁海流计 geomagnetic electro kinetograph
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geomagnetic electro kinetograph：地磁海流计
地磁电流量计地磁海流计电地磁流量计 geomagnetic electro kinetograph | 地磁海流计 geomagnetic electro kinetograph | 电地磁流量计 geomagnetic electro kinetograph
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geomagnetic electro kinetograph：地磁动电计
geomagnetic electro kinetograph 电流海流计 | geomagnetic electro-kinetograph 地磁动电计 | geomagnetic electrokinetograph 地磁电动测速仪,地磁动电测流计
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earth magnetism：地磁=>地磁気
earth magnetic field balance 地磁场平衡器 | earth magnetism 地磁=>地磁気 | earth magnetosphere 地球磁层
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Geomagnetic storms：地磁风暴
Geomagnetism 地磁 | Geomagnetic Storms 地磁风暴 | Geomagnetic Pulsation 地磁脉动
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earth inductor compass：地磁感应罗盘,地磁感应器
earth inductor ==> 地磁感应器 | earth inductor compass ==> 地磁感应罗盘,地磁感应器 | earth insulation ==> 对地绝缘,主绝缘(电机的)