Shock remagnetization associated with meteorite impact at planetary surfaces

Shock remagnetization is a significant mode of alteration of the intensity and direction of magnetization in planetary crustal rocks subjected to the dynamic and thermochemical effects associated with meteorite impact. Shock remagnetization will take place almost instantaneously during and following the transient shock episode, and over longer times depending on residual temperature effects associated with shock heating and the production of impact melt. Remagnetization will follow certain demagnetization effects. The following transitions and residual effects will result in remagnetization of planetary crustal material:

1. First order reversible crystallographic transitions in bodycentered cubic iron-nickel alloys.
2. Second order Curie temperature transitions in face-centered cubic iron-nickel alloys.
3. Shock induced uniaxial anisotropy due to magnetoelasstic coupling of magnetic vectors to the shock wave.
4. Shock melting of iron containing silicates.
5. Subsolidus reduction and FeO decomposition.
6. Partial ther moremanence due to post-shock temperature.
7. Total thermoremanence due to post-shock temperature.
8. Production of a superparamagnetic distribution of iron which is sensitive to surface temperature fluctuation.
9. Thermal effects in metal and alloy phases.

Lunar breccia and soil samples are generally more reduced than crystalline rocks and some of th's reduction is subsolidus probably associated with the transient thermal effects due to meteorite impact in teh porous reglith.