Reduction–oxidation (redox) reactions occur during burial because sediments contain
reactive mixtures of oxidised and reduced components. Diagenetic chemical reactions …

Magnetic iron oxide minerals, principally magnetite, maghemite, hematite, and goethite are
formed in well-drained soils in response to a suite of physical, chemical, and biological …

For 40 years magnetic anisotropy has provided successful geological interpretations of
magnetic ellipsoid orientations; in contrast the interpretation of anisotropy magnitudes is far …

Magnetic hysteresis measurements of sediments have resulted in widespread reporting of
“pseudo‐single‐domain”‐like magnetic properties. In contrast, the ideal single domain (SD) …

This book describes the paleomagnetism of sediments and sedimentary rocks, how
sediments and sedimentary rocks become magnetized, and how the physical and chemical …

Pelagic carbonates are deposited far from continents, usually at water depths of 3000–6000
m, at rates below 10 cm/kyr, and are a globally important sediment type. Recent advances …

Chemical remagnetization is a very common phenomenon in sedimentary rocks and
developing a greater understanding of the mechanisms has several benefits. Acquisition of …

Results of a paleomagnetic, rock magnetic, geochemical, and petrographic study on
Jurassic and Cretaceous carbonates in the Vocontian trough support a hypothesized …

Cette étude examine l'écoulement des paléo-fluides à travers les aquifères de carbonate du
Dévonien dans la partie profonde du Bassin de l'ouest de l'Alberta, en utilisant la distribution …

In several recent published studies, paleomagnetic results from greigite-bearing sediments
reveal characteristic remanences that are anti-parallel to those carried by coexisting detrital …