Paleointensity record from the 2.7 Ga Stillwater Complex, Montana
Article first published online: 23 DEC 2008
Copyright 2008 by the American Geophysical Union.
Geochemistry, Geophysics, Geosystems
Volume 9, Issue 12, December 2008
How to Cite
2008), Paleointensity record from the 2.7 Ga Stillwater Complex, Montana, Geochem. Geophys. Geosyst., 9, Q12023, doi:10.1029/2008GC001950., , , and (
- Issue published online: 23 DEC 2008
- Article first published online: 23 DEC 2008
- Manuscript Accepted: 26 SEP 2008
- Manuscript Revised: 25 JUN 2008
- Manuscript Received: 23 JAN 2008
- Stillwater Complex;
- modified Thellier–Coe method;
- core processes
 The record of geomagnetic intensity captured in the 2.7 Ga Stillwater Complex (Montana, USA) provides a statistical description of the Archean geodynamo. We present results of modified Thellier paleointensity experiments on 441 core specimens, 114 of which pass strict reliability criteria. The specimens are from 53 sites spanning most of the Banded Series rocks in the Stillwater Complex. On the basis of thermochronologic and petrologic evidence, we interpret the highest temperature component of remanence to be a late Archean thermoremanence, though the possibility remains that it is a thermochemical remanence. Thermal models indicate that the highest temperature magnetization component at each of the sites averages ∼20–200 ka of geomagnetic secular variation. The suite of sites as distributed through the Banded Series samples a roughly a 1 Ma time interval. The average of the most reliable paleointensity measurements, uncorrected for the effects of anisotropy or cooling rate, is 38.2 ± 11.3 μT (1σ). Remanence anisotropy, cooling rate, and the nonlinear relationship between applied field and thermoremanence have a significant effect on paleointensity results; a corrected average of 30.6 ± 8.8 μT is likely a more appropriate value. Earth's average dipole moment during the late Archean (5.05 ± 1.46 × 1022 Am2, λpmag = 44.5°) was well within the range of estimates from Phanerozoic rocks. The distribution of site-mean paleointensities around the mean is consistent with that expected from slow cooling over timescales expected from thermal models and with secular variation comparable to that of the Phanerozoic field.