Natural remanent magnetization carriers in rocks can contain mixtures of magnetic minerals
that interact in complex ways and are challenging to characterize by current measurement …

Rapid global changes since the last deglaciation can be well documented in marginal sea
sediments, while isolating individual paleoenvironmental signals is still challenging. Here …

岩石磁学是研究自然以及人工合成磁性矿物性质变化的应用型学科. 海底岩石和海洋沉积物等
海洋样品中含有不同成因及来源的磁性矿物. 这些磁性矿物蕴含了全球气候变化, 微生物矿化 …

The relationships among the abundance of magnetofossils, the ensuing magnetic
properties, and the controlling paleoenvironmental factors in marine sediments remain …

We make fundamental observations of the particle size variability of magnetic properties
from 71 core tops that span the southern Greenland and Norwegian Seas. These data …

Crystal habit in igneous rocks provides a window to understand magmatic processes or
reveal crystallization environments. Generally, we can obtain the two-dimensional (2D) …

Magnetite and hematite mixtures occur widely in nature. Magnetic unmixing of the signals
recorded by these minerals can be important for assessing the origin of their respective …

Continental shelf sediments along the northeast continental margin of North America contain
a magnetofossil‐rich interval deposited during the Paleocene‐Eocene Thermal Maximum …

The characterization of magnetic minerals in rocks often uses methods that measure
induced magnetization. When rocks, sediments or soils contain two magnetic phases, in …

Magnetic parameters are used extensively to interpret magnetic mineral assemblage
variations in environmental studies. Conventional room temperature measurements of bulk …