Paleointensities from Tertiary basalts, Inner Mongolia and Hebei Province, northeastern China

Abstract

A paleointensity study using the Thellier's method was made on Tertiary basaltic rocks in Inner Mongolia and Hebei Province, northeastern China. K-Ar ages were previously reported for all the rocks, which range around 6-8 Ma and 28-32 Ma. Sample selection was based on total quality of remanence behavior and rock magnetism. High stability to AF and thermal demagnetization, small difference between the heating and cooling curves of magnetic susceptibility vs. temperature measurements, and PSD to SD characteristics in the Day plot of the hysteresis parameters were required. Experiments in vacuum using Coe's procedure were applied to 54 specimens from nine flows. Experiments were successful for 34 specimens, giving seven flow mean paleointensities. Excluding two flow means (in one flow, only two specimens from the same sample survived and in the other, the within-site error amounts to 42%) the final success rate was 29 out of 54 (54%), which is not low. The obtained results range from 54 to 65 μT, except for one lava which gave 23 μT. These results indicate that although the paleointensity in the Tertiary was generally smaller than the present-day value, there were large fluctuations in the dipole moment, and paleointensities of the present-day level were often attained.

Palaeointensity determinations and magnetic properties on Eocene rocks from Izu-Bonin-Mariana forearc (IODP Exp. 352)

“…Our data are plotted with the full black symbols together with their error bars (squares: Thellier-Thellier results; stars: MSP results). Data represented by-crosses: Goguitchaishvili et al (2004); circled crosses: Carvallo et al (2004); filled diamonds: Shcherbakova et al (2012); empty diamonds: Juárez et al (1998); triangles pointing rightward: Tauxe (2006); triangles pointing leftward: Riisager et al (2002); upward triangles: Perrin et al (1999); downward triangles: Riisager et al (1999); diamonds and crosses: Riisager et al (2004); empty circles: Riisager & Abrahamsen (2000) without transitional flows; stars: Tanaka et al (2007); empty squares: Tarduno & Cottrell (2005); black circle: Hill et al (2002). Data from Juárez et al (1998) and Tauxe (2006) come from submarine basaltic glass; data from Tarduno & Cottrell (2005) come from single-crystals; all other are from whole rocks.…”