Fig. 9From: Geomagnetic relative paleointensity and direction during the last 40,000 years obtained from a sediment core in the Nankai TroughTransmission electron microscope (TEM) images of magnetofossils extracted from sediments at (a) 8.9 kry cal BP and (b) 28.4 kyr cal BP. scale bar: a 50 nm and b 100 nmBack to article page