As iron‐bearing minerals—ferrimagnetic minerals in particular—are sensitive to stress,
temperature, and presence of fluids in fault zones, their magnetic properties provide …

Magnetic properties from the Reinfjord Ultramafic Complex, in northern Norway, which
formed as part of a deep magmatic conduit system, have been investigated to determine the …

Serpentinization of ultramafic rocks is fundamental to modern plate tectonics and for volatile
(re‐) cycling into the mantle and magmatic arcs. Serpentinites are also highly reactive with …

Satellite magnetic surveys have revealed features consistent with magnetization at depth in
the lithosphere. Previous studies have reported magnetic minerals preserved in mantle …

Scanning magnetic microscopy (SMM) is a modern magnetometry technique that maps the
magnetic anomalies resulting from small‐scale variations of remanent magnetization within …

Abstract The Seiland Igneous Province (SIP) is a large province of mafic and ultramafic (UM)
complexes interpreted to be relics of a giant plumbing system feeding the Ediacaran Central …

Recent advances in magnetic microscopy have enabled studies of geological samples
whose weak and spatially nonuniform magnetizations were previously inaccessible to …

Abstract Development in instrumentation and technology now allows for mapping of
magnetic anomalies, caused by spatial variations in magnetization in the source material …

Distinct crustal remanent magnetic anomalies are a strong indicator of rocks with stable
natural remanent magnetization (NRM) carriers. The latter are able to store information on …

We present developments and applications of a high resolution scanning superconducting
quantum interference device (SQUID) microscope for imaging magnetic field of geological …