| Twelve specimens were studied from different dykes in a Proterozoic dolerite dyke swarm (U-Pb date of 1,277 {dollar}pm{dollar} 3 Ma) located near Nain, Labrador. Each specimen carried a stable westerly-directed remanence that was likely acquired soon after crystallization. Alternating-field demagnetization curves of the natural remanent magnetization (NRM) of each specimen had a quadratic shape. The median destructive field (MDF), which is the alternating field required to reduce intensity by half, ranged from 18mT to 47.5mT for NRM. These properties suggest that remanence is carried by single-domain (SD) or pseudo-single-domain (PSD) grains of magnetite rather than by large multidomain (MD) grains. Median destructive fields were similar for anhysteretic remanent magnetization (ARM) and NRM but were smaller for saturation isothermal remanent magnetization (SIRM).; Apparatus was built to measure remanence intensity as a function of temperature in cooling cycles to near liquid nitrogen temperature. Low-temperature demagnetization experiments were done for NRM, ARM and SIRM for all specimens.; For the three specimens with highest median destructive fields ({dollar}sim{dollar}40mT for NRM) low temperature cycling had relatively little effect on remanence as expected if the remanence was controlled by shape anisotropy. Similar low-temperature behaviour was reported by others for synthetic magnetites of less than.31{dollar}mu{dollar}m grain size. (Abstract shortened by UMI.)... |
