Detrital input and early diagenesis in sediments from Lake Baikal revealed by rock magnetism
- 27 January 2005
- journal article
- Published by Elsevier BV in Global and Planetary Change
- Vol. 46 (1-4), 145-166
- https://doi.org/10.1016/j.gloplacha.2004.11.010
Abstract
No abstract availableKeywords
This publication has 46 references indexed in Scilit:
- Biological and environmental changes in Lake Baikal during the late Quaternary inferred from carbon, nitrogen and sulfur isotopesEarth and Planetary Science Letters, 2004
- Magnetite dissolution in siliceous sedimentsGeochemistry, Geophysics, Geosystems, 2003
- Theory and application of the Day plot (Mrs/MsversusHcr/Hc) 2. Application to data for rocks, sediments, and soilsJournal of Geophysical Research, 2002
- Theory and application of the Day plot (Mrs/Ms versus Hcr/Hc) 1. Theoretical curves and tests using titanomagnetite dataJournal of Geophysical Research, 2002
- Grain size limit for SD hematitePhysics of the Earth and Planetary Interiors, 2002
- Low‐temperature magnetic properties of pelagic sediments (Ocean Drilling Program Site 805C): Tracers of maghemitization and magnetic mineral reductionJournal of Geophysical Research, 2000
- Fractals in studies of faulting and seismicity in the Baikal rift zoneTectonophysics, 1999
- A gyroremanent magnetisation in anisotropic magnetic materialNature, 1980
- THE USE OF ANISOTROPY OF MAGNETIC SUSCEPTIBILITY IN THE ESTIMATION OF SEDIMENTARY FABRIC1Sedimentology, 1965
- Magnetic anisotropy and fabric of some foliated rocks from S.E. AustraliaPure and Applied Geophysics, 1960