EarthRef.org Reference Database (ERR)
Development and Maintenance by the EarthRef.org Database Team

Detailed Reference Information
Sumita et al. 2001
Sumita, I., Hatakeyama, T., Yoshihara, A. and Hamano, Y. (2001). Paleomagnetism of late Archean rocks of Hamersley Basin, Western Australia and the paleointensity at early Proterozoic. Physics of the Earth and Planetary Interiors 128: 223-241. doi: 10.1016/S0031-9201(01)00288-6.
We report the results of paleomagnetic and rock magnetic measurements of late Archean rocks from Hamersley basin, Western Australia, and the paleointensity determination for early Proterozoic. Basalts and banded iron formations have two to four components of remanent magnetization, and have consistent directions for different localities, indicative of geomagnetic origin. Rock magnetic measurements of basalts reveal that the main magnetic mineral is a fine-grained magnetite present in approximately 10 ppm in mass, which do not alter when heated up to its blocking temperature. We interpret the stable component up to approximately 390 degrees C as the post-tilting thermal overprint from uplift at congruent to 2.0 Ga, and the higher temperature component as the pre-tilting thermoviscous remanence during burial metamorphism. From the Thellier type paleointensity experiments using the thermal overprint component, we obtain a mean virtual dipole moment (VDM) estimate of (1.8-3.6)X10 (super 22) Am (super 2). This suggests that early Proterozoic was characterized by a 1 weak geomagnetic field of less than one-half of the present.
DATABASE QUICK LINKS

MagIC Database

BACKGROUND DATA FILES

Experimental Methods
Thellier Method
Shaw Method

MagIC SmartBook v1
MagIC SmartBook v2

Keywords
anhysteretic remanent magnetization, Archean, Australasia, Australia, burial metamorphism, demagnetization, dipole moment, experimental, studies, Hamersley Basin, isothermal remanent magnetization, magnetic, field, magnetic intensity, magnetic minerals, magnetic susceptibility, magnetization, metabasalt, metaigneous rocks, metamorphic rocks, metamorphism, metasedimentary rocks, natural remanent magnetization, overprinting, paleomagnetism, Paleoproterozoic, Precambrian, Proterozoic, remanent magnetization, saturation magnetization, thermal, effects, thermoremanent magnetization, upper Archean, upper, Precambrian, Western Australia, 12 Stratigraphy, 18 Solid-earth geophysics
Journal
Physics of the Earth and Planetary Interiors
http://www.elsevier.com/locate/pepi
Publisher
Elsevier Science
P.O. Box 211
1000 AE Amsterdam
The Netherlands
(+31) 20 485 3757
(+31) 20 485 3432
nlinfo-f@elsevier.com
Click to clear formClick to return to previous pageClick to submit