AMS:磁化率各向异性
“磁化率各向异性”(Anisotropy of Magnetic Susceptibility)在物理学和地球科学等学术领域应用广泛。为便于书写和表达,该术语常被缩写为AMS。它描述了材料在不同方向上的磁化率差异特性,是研究岩石磁学、构造地质学的重要参数。
Anisotropy of Magnetic Susceptibility具体释义
Anisotropy of Magnetic Susceptibility的英文发音
例句
- The study of anisotropy of magnetic susceptibility for two types of granitoids was carried in Guangdong province, China.
- 广东省两类不同成因类型花岗岩磁化率各向异性(AMS)研究表明:Ⅰ型花岗岩的磁化率的数值较大,一致性较好;
- Magnetic field is a novel way to control the crystal growth since it can induce the crystal to grow along the direction of lower magnetic energy because of the anisotropy of magnetic susceptibility.
- 磁场可以诱导磁各向异性材料沿着磁能较小的方向生长,达到控制晶体生长的目的。
- The relationship between anisotropy of magnetic susceptibility and the tectonic setting for granitoid ── as exemplified by two kinds of genetic granitoids in Guangdong province, china the studies of magnetic susceptibility anisotropy of rock samples, i. E.
- 磁化率各向异性(AMS)与花岗岩形成的构造背景&以广东两类不同成因类型花岗岩为例岩石样品磁化率各向异性(AMS),即磁性组构的研究,已逐渐引起人们注意。
- The study of the new tectonics in valley of the Qingjiang River with the anisotropy of magnetic susceptibility of the Quaternary
- 研究鄂西南清江流域的新构造运动&利用第四纪沉积物的磁化率各向异性(AMS)特征
- The anisotropy of rock magnetic susceptibility, caused by the oriented arrangement of magnetic minerals effected by then magnetic field, reflects the feature of the rock magnetic fabric.
- 由于磁性矿物受当时磁场作用往往呈定向排列,导致岩石磁化率各向异性(AMS),反映了岩石的磁组构特征。
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