Speleothems are of interest for high‐resolution reconstruction of the Earth's magnetic field.
However, little is known about the influence of speleothem morphologies on their natural …

We provide a high‐resolution and complete paleomagnetic study from a middle‐Holocene
(~ 4,100–3,300 years Before Common Era, BCE) dome‐shaped speleothem (SPAIV) from …

The magnetic recordings preserved in calcite speleothems and the nature of their
constituent magnetic minerals hold enormous potential for paleomagnetic and …

Environmental magnetism of speleothems is still in its early stage of development. Here we
report on our investigation of the environmental and paleomagnetic information that has …

Magnetic hysteresis data determine the suitability of rocks for paleomagnetic work, provide
clues to paleo‐environment and paleo‐climate and they may characterize depositional …

Paleogeographic reconstructions largely rely on paleomagnetic data, mostly in the form of
paleomagnetic poles. Compilations of poles are used to determine so called apparent polar …

In directional archaeomagnetic studies, it is rarely analysed whether the combustion
structures display anisotropy of their thermoremanent magnetization (ATRM). It has been …

Magnetic anisotropy studies have recently come to the forefront as accurate, fast and
inexpensive methods in the investigation of the rock fabric. In this paper we summarize the …

Speleothems are potentially excellent archives of the Earth's magnetic field, capable of
recording its past variations. Their characteristics, such as the continuity of the record, the …

To further evaluate the potential of magnetic anisotropy techniques for determining the origin
of the natural remanent magnetization (NRM) in sedimentary rocks, several new remanence …