Micron to sub‐micron sized ferromagnetic inclusions in rock forming silicate minerals may
give rise to particularly stable remanent magnetizations. When a population of inclusions …

Plagioclase-hosted submicrometer to micrometer-sized oriented needle-and lath-shaped
magnetite micro-inclusions with their elongation direction aligned parallel to the plagioclase …

Submicroscopic, needle-shaped titanomagnetite inclusions exsolved in silicate minerals
commonly occur in mafic intrusive rocks and are protected from alteration by their silicate …

Plagioclase hosted, oriented magnetite micro-inclusions are a frequently observed
phenomenon in magmatic and metamorphic rocks. Understanding the orientation …

Oriented needle-, lath-and plate-shaped magnetite micro-inclusions in rock forming
plagioclase from mafic intrusive rocks, were investigated using correlated optical microscopy …

Plagioclase hosted needle-and lath-shaped magnetite micro-inclusions from oceanic
gabbro dredged at the mid-Atlantic ridge at 13° 01–02′ N, 44° 52′ W were investigated to …

Randomly oriented phlogopite crystals from a pegmatite contain submicroscopic inclusions
of magnetite. The inclusions have oblate magnetic fabrics, subparallel to the ab crystal …

Titanomagnetite inclusions in pyroxene and plagioclase are carriers of stable magnetic
remanence in some slowly cooled rocks such as gabbros, anorthosites, granulites, and …

In the early days of paleomagnetism, David Strangway was interested in understanding why
igneous rocks are faithful recorders of the Earth's magnetic field. He recognized that …

Granitoids are widespread in Precambrian terranes as well as the Phanerozoic orogenic
belts, but they have garnered little attention in paleomagnetic studies, because granitoids …