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

Publisher Summary This chapter describes properties and behavior of iron in clay minerals.
Because of their great abundance, high specific surface area, layer charge, laminar …

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

Low-temperature oxidation under atmospheric conditions affects the magnetic properties of
magnetite in natural rocks: the coercivities of magnetite grains increase and other …

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

Continental shelves serve as a bridge between the continent and ocean and sediments in
this region are sensitive to land-sea interaction, sea-level variation and local subsidence. In …

Authigenic formation of fine-grained magnetite is responsible for widespread chemical
remagnetization of many carbonate rocks. Authigenic magnetite grains, dominantly in the …

Abstract Comparison of the paleomagnetic pole positions of late Paleozoic secondary
magnetizations with a time-averaged reference apparent polar wander path for North …

As iron‐bearing minerals—ferrimagnetic minerals in particular—are sensitive to stress,
temperature, and presence of fluids in fault zones, their magnetic properties provide …

Paleomagnetic, rock magnetic, and geochemical results from Mesozoic carbonates in the
Vocontian trough in southeast France support a hypothesized acquisition of a chemical …