Magnetic properties of variably serpentinized abyssal peridotites

Author:

Oufi Omar

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

Reference91 articles.

1. Oxygen isotopic constraints on serpentinization processes in ultramafic rocks from the Mid-Atlantic Ridge (lat. 23°N), in the MARK area;Agrinier;Proc. Ocean Drill. Program Sci. Results,1997

2. Stable isotope composition (18O/16O, D/H, and 14C/12C) of oceanic crust and upper mantle rocks in the Hess Deep near the Galapagos Triple Juction;Agrinier;Earth Planet. Sci. Lett.,1996

3. Petrology of ultramafic rocks from site 395;Arai;Initial Rep. Deep Sea Drill. Proj.,1978

4. Low-temperature and high-temperature hysteresis of small multidomain magnetites (215–540 nm);Argyle;J. Geophys. Res.,1990

5. Single-domain behaviour of multidomain magnetite grains (abstract);Argyle;Eos Trans. AGU,1994

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