1) horizontal intensity of geomagnetic field
地磁场水平强度
2) horizontal magnetic intensity
水平磁场强度
3) geomagnetic horizontal intensity
地磁水平强度
4) geomagnetic field intensity
地磁场强度
1.
According to the available paleogeomagnetic field intensity data,this study simulated instantaneous and time-integrated 10Be production rates over the last 200.
在103-105a的尺度上,地磁场强度变化是影响陆地宇生核素生成速率的主要因素,其影响程度取决于样品的地理位置和暴露时间。
2.
In view of the problem that the second environmental forces are weak and not easy to be measured,a three-axis magnetic sensor is used to detect the geomagnetic field intensity on the muzzle based on the directivity of the geomagnetic field.
针对非旋或微旋弹引信第二环境力微弱和不容易识别的问题,考虑到地磁场强度的方向性,提出应用三轴磁传感器检测炮口地磁信号,获取弹丸出炮口信息,以此作为引信冗余保险激励环境信息。
3.
In this paper, the influence character of the geomagnetic field intensity and inclination on SNMR signal has been discussed and analyzed, and the influence in Chinese region\'s have been discussed.
本文论述并分析了诸多影响因素中的地磁场强度和磁倾角对NMR信号的影响特点,进而分析了我国区域地磁场强度和磁倾角对SNMR信号的影响规律,对我国进行区域性水文地质调查中运用SNMR方法时提供了重要的参考资料。
5) Geomagnetic paleointensity
古地球磁场强度
6) paleointensity of the geomagnetic field
地球磁场古强度
1.
It is unveiled that during most of the Mesozoic (200~100 Ma) the paleointensity of the geomagnetic field was very low, only one-third of the mean Cenozoic value, that the geomagnetic field shows no reversals from 124 to 83 Ma, and that the true polar wander (TPW) almost remained a standstill from 170 to 110 Ma.
本文介绍了90年代以来地球物理学在地球磁场方面(地球磁场古强度,地磁场极性反转频率以及真极移)的研究成果,揭示了200～100Ma全球低的地球磁场古强度;124～83Ma低的极性反转频率以及170～110Ma近乎停滞的真极移。
补充资料：地磁
1.地球所具有的磁性现象，在不同的地区和时间都有变化。罗盘指南和磁力探矿都是地磁的利用。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条