Magnetization during low-temperature oxidation of seafloor basalts: No large scale chemical remagnetization

Author:

Beske-Diehl S. J.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference81 articles.

1. The magnetic and opaque petrological response of basalts to regional hydrothermal alteration;Ade-Hall;Geophys. J. R. Astron. Soc.,1971

2. Rock magnetism of basalts, leg 34;Ade-Hall;Initial Rep. Deep Sea Drill. Proj.,1976

3. Hydrothermal alteration of a 1-km section through the upper oceanic crust, Deep Sea Drilling Project hole 504B: Mineralogy, chemistry, and evolution of seawater-basalt interaction;Alt;J. Geophys. Res.,1986

4. Zeolite facies metamorphism, geochemistry, and some aspects of trace element redistribution in altered basalts of DSDP, leg 37;Andrews;Initial Rep. Deep Sea Drill. Proj.,1977

5. Domain state of Ti-rich titanomagnetites deduced from domain structure observations and susceptibility measurements;Appel;J. Geophys.,1985

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