Both detailed rock magnetism and structural analysis suggest that the routine anisotropy of
magnetic susceptibility (AMS) measurements can not suffice for the interpretations of …

Palaeomagnetic studies of Apollo samples indicate that the Moon generated a magnetic
field for at least 2 billion years,. However, the geometry of the lunar magnetic field is still …

The magnetic anisotropy carried by strongly magnetic particles such as magnetite or
ferrofluid‐filled pores is generally composed of shape anisotropy and distribution anisotropy …

目前实验条件下获得的AMS (磁化率各向异性) 是岩石内所有磁性矿物磁化率各向异性叠加的
综合响应, 详细的岩石磁学和构造地质学的综合分析表明常规AMS 测试结果通常无法揭示岩石 …

Magnetic fabrics are powerful tools in structural geology and tectonic studies, because they
provide a fast and efficient measurement of mineral alignment, which helps interpret a rock's …

Heterogeneities in the magnetic signature along intraplate shear zones complicate their
correlation with the physical processes that are involved in the geodynamic evolution of …

Exsolved iron oxides in silicate minerals can be nearly ideal palaeomagnetic recorders, due
to their single-domain-like behaviour and the protection from chemical alteration by their …

Anisotropy of isothermal remanent magnetization (AIRM) is useful for describing the fabrics
of high-coercivity grains, or alternatively, the fabrics of all remanence-carrying grains in …

Paleomagnetic studies of Apollo samples indicate that the Moon generated a core 18
dynamo lasting for at least 2 billion years1, 2, 3. However, the geometry of the lunar 19 …