Early diagenesis in an organic-rich turbidite and pelagic clay sequence from the Cape Verde Abyssal Plain, NE Atlantic: magnetic and geochemical signals

Author:

Robinson S.G

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference114 articles.

1. Arthur, M.A., Dean, W.E., Stow, D.A.V., 1984. Models for the deposition of Mesozoic-Cenozoic fine-grained, organic-carbon-rich, sediment in the deep-sea. In: Stow, D.A.V., Piper, D.J.W. (Eds.), Fine-Grained Sediments: Deep-Water Processes and Facies, Geol. Soc. Lond. Spec. Publ., 15, 527–560.

2. Magneto-mineralogical studies of metalliferous sediments and ferromanganese concretions from the East Pacific Rise;Bagin;Phys. Solid Earth (USSR),1977

3. Alternating field characteristics of pseudo-single-domain (2–14μm) and multidomain magnetite;Bailey;Earth Planet. Sci. Lett.,1983

4. A rapid method for magnetic granulometry with applications to environmental studies;Banerjee;Geophys. Res. Lett.,1981

5. Biomineralisation of iron sulfides in magnetotactic bacteria from sulfidic environments;Bazylinski,1990

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