1. Last Time: Gravity Modeling Gravitational attraction of an arbitrary body: Gravity anomaly due to a sphere: (represents only the vertical component of the total vector!) Anomalies for: horizontal cylinder: vertical cylinder: fault-bounded basin : Geology 5660/6660 Applied Geophysics 24 Mar 2014 © A.R. Lowry 2014 For Wed 26 Mar: Burger 429-449 (§7.1–7.3)

2. Magnetics: Like gravity, a potential field method governed by Laplace’s equation:  2 u = f (sources) Unlike gravity, source term is a vector rather than a scalar Gravity : Monopole source  field is always directed radially toward a “sink” location Magnetics : Dipole source  field direction & strength depend on one “source”, one “sink” S N

3. Coulomb’s Law describes the force of attraction exerted between two magnetic poles: where is the distance & direction between two poles p 1 & p 2 are pole strengths  is magnetic permeability, a property of the medium (usually ~1) p1p1 p2p2 Magnetic Field Strength is the force that would be exerted on a hypothetical “unit monopole” p 2 due to p 1 : (MKS units of Tesla; magnetic anomalies usually given in nT or  s)

4. Definitions: Magnetic Dipole Moment : Two poles +p and –p separated by a distance l have moment Intensity of Magnetization : (where V is volume) is a material property of the magnetic source. *** If a material that can produce a magnetic field (  > 1 ) is placed within an external magnetic field H, then intensity of the induced magnetization is where k =  – 1 is magnetic susceptibility of the material. (e.g., magnetite-rich body)

5. Most Earth materials are diamagnetic :  very small negative k ~ –10 -5 (e.g., quartz) Fe-Mg silicates (pyroxene, amphibole, olivine) are paramagnetic (moments can align within small magnetic domains )  k ~ 0.02 to 0.2 Hematite (“rust” in aeolian soils) is antiferromagnetic : domains align, equal amounts parallel & antiparallel  k ~ 0.05 positive and non-negligible, but still small Magnetite is ferrimagnetic : domains align parallel & antiparallel but one dominates: k ~ 0.5 to 10 ! (Also titanomagnetite, ilmenite, pyrrhotite) Crystalline iron, nickel, cobalt are ferromagnetic : domains align parallel (not common in crust, but common in the core!)

6. Gravity Anomaly Magnetic Anomaly Magnetic Prospecting : Measure magnitude H of the total field, subtract out magnitude H E of the Earth’s (core dynamo- derived) main field to get a magnetic anomaly

7. However despite the complexities of modeling, magnetic anomalies are heavily used (particularly by the mining industry and for investigations of basement structure)

8. Induced magnetization is always in the direction of the ambient field  Must know strength & direction of the Earth’s ambient field to determine location and magnetic susceptibility k of a source body! Magnetic field strength falls off proportional to 1/r 3 Total intensity of magnetization where remanent magnetization I R is in the direction of H E at the time of magnetization…