Oxide mineral formation during the serpentinization of a Cr-spinel seam: Insights from rock magnetic experiments-Reference-Cited by-同舟云学术

Oxide mineral formation during the serpentinization of a Cr-spinel seam: Insights from rock magnetic experiments

Published:2009-01 Issue:1 Volume:10 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

O'Driscoll Brian,Petronis Michael S.¹

Affiliation:

1. Environmental Geology, Natural Resource Management Department; New Mexico Highlands University; Ivan Hilton Science Technology Building,; Las Vegas; New Mexico; 87701; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference36 articles.

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2. Chapter 4.MAGNETIC PROPERTIES OF FE-TI OXIDES

3. Present day serpentinisation in New Caledonia, Oman, and Yugoslavia;Barnes;Geochim. Cosmochim. Acta,1978

4. Younging directions in the Dawros Peridotite, Connemara;Bennett;J. Geol. Soc.,1983

5. Magnetization during low-temperature oxidation of seafloor basalts: No large-scale chemical remagnetization;Beske-Diehl;J. Geophys. Res.,1990

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2. Earthquakes in the Mantle? Insights From Rock Magnetism of Pseudotachylytes;Journal of Geophysical Research: Solid Earth;2017-11

3. Parental magma composition of the syntectonic Dawros Peridotite chromitites, NW Connemara, Ireland;Geological Magazine;2011-10-14

4. Magmatic influence on reaction paths and element transport during serpentinization;Chemical Geology;2010-07