We have been developing high sensitivity, high spatial resolution magnetometry techniques for applications to geologic samples.   One of the main techniques we have been using is scanning superconducting quantum interference device (SQUID) microscopy (Weiss et al. 2007; Lima and Weiss 2009), which maps the vertical component of the magnetic field above room-temperature geologic samples with a moment resolution of of 1e-15 Am2 and a spatial resolution of 100 μm.  This performance is about ~1,000 times and ~100 times, respectively, better than existing superconducting moment magnetometers. This allows us to directly map the three components of the magnetic field of individual grains and textures in thin sections.

We have also developed a scanning magnetic tunnel junction (MTJ) microscope (Lima et al. 2014) based on room‐temperature sensors that typically achieves spatial resolution better than 7 μm with a moment resolutionf of 1e-14 Am2.  This represents an improvement in sensitivity by a factor between 10 and 30 compared to similar scanning MTJ microscopes based on conventional bias-detection schemes.   

Over the last decade, we have used magnetic microscopy to adapt standard paleomagnetic techniques like thermal and alternating field demagnetization (Fu et al. 2014), paleointensity methods (Weiss et al. 2007; 2008), conglomerate tests (Fu et al. 2014), and even magnetostratigraphy (Oda et al. 2011) to microscale samples like meteorites and single silicate crystals.