In the early days of paleomagnetism, David Strangway was interested in understanding why igneous rocks are faithful recorders of the Earthâ s magnetic field. He recognized that ferromagnetic (s.l.) grains that could be discerned by optical microscopy were too large to carry a stable remanent magnetization, and speculated whether fine-grained, ferromagnetic (s.l.) inclusions or exsolutions in silicate minerals are responsible. When these inclusions or exsolutions are randomly oriented, or the silicate hosts are randomly oriented in a rock, they can be a good recorder of the field. If these minerals, however, show an alignment within the silicate host, and the host is preferentially aligned due to flow structures or deformation, then the pal...
Magnetic anisotropy analysis presents an alternative and fast method for obtaining and quantifying c...
The low and high-field magnetic anisotropy (AMS, HFA) of the various sedimentary and anchimetamorphi...
New experimental and computational approaches to interpret orientation and intensity of natural rema...
In the early days of paleomagnetism, David Strangway was interested in understanding why igneous roc...
In the early days of paleomagnetism, David Strangway was interested in understanding why igneous roc...
Empirical relationships between magnetic fabrics and deformation have long served as a fast and effi...
The magnetic fabric of a rock, defined by the anisotropy of magnetic susceptibility (AMS), is often ...
Pyroxenes constitute an important component in mafic igneous and metamorphic rocks. They often posse...
The anisotropy of magnetic susceptibility (AMS) has been used as a petrofabric indicator since the e...
Cambrian and Silurian, low-grade, pelitic rocks of the single-phase deformed Brabant Massif consiste...
A regional analysis of the anisotropy of the magnetic susceptibility on low-grade metamorphic, chlor...
Mantle flow dynamics can cause preferential alignment of olivine crystals that results in anisotropy...
Samples of different rocks, which possess high values of the anisotropy of magnetic susceptibility, ...
Pioneering works on the magnetic anisotropy of rocks were carried out during the 1940s and 1950s (I...
Exsolved iron oxides in silicate minerals can be nearly ideal paleomagnetic recorders, due to their ...
Magnetic anisotropy analysis presents an alternative and fast method for obtaining and quantifying c...
The low and high-field magnetic anisotropy (AMS, HFA) of the various sedimentary and anchimetamorphi...
New experimental and computational approaches to interpret orientation and intensity of natural rema...
In the early days of paleomagnetism, David Strangway was interested in understanding why igneous roc...
In the early days of paleomagnetism, David Strangway was interested in understanding why igneous roc...
Empirical relationships between magnetic fabrics and deformation have long served as a fast and effi...
The magnetic fabric of a rock, defined by the anisotropy of magnetic susceptibility (AMS), is often ...
Pyroxenes constitute an important component in mafic igneous and metamorphic rocks. They often posse...
The anisotropy of magnetic susceptibility (AMS) has been used as a petrofabric indicator since the e...
Cambrian and Silurian, low-grade, pelitic rocks of the single-phase deformed Brabant Massif consiste...
A regional analysis of the anisotropy of the magnetic susceptibility on low-grade metamorphic, chlor...
Mantle flow dynamics can cause preferential alignment of olivine crystals that results in anisotropy...
Samples of different rocks, which possess high values of the anisotropy of magnetic susceptibility, ...
Pioneering works on the magnetic anisotropy of rocks were carried out during the 1940s and 1950s (I...
Exsolved iron oxides in silicate minerals can be nearly ideal paleomagnetic recorders, due to their ...
Magnetic anisotropy analysis presents an alternative and fast method for obtaining and quantifying c...
The low and high-field magnetic anisotropy (AMS, HFA) of the various sedimentary and anchimetamorphi...
New experimental and computational approaches to interpret orientation and intensity of natural rema...