Comparison and calibration of nonheating paleointensity methods: A case study using dusty olivine
Author:
Affiliation:
1. Department of Earth SciencesUniversity of CambridgeCambridge UK
2. Institute for Rock Magnetism, University of MinnesotaMinneapolis Minnesota USA
3. Department of Earth Science and EngineeringImperial College LondonLondon UK
Funder
EPSRC and the Cambridge European Trust
Institute for Rock Magnetism (IRM)
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ggge.20141
Reference39 articles.
1. Micromagnetic coercivity distributions and interactions in chondrules with implications for paleointensities of the early solar system
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3. Solid-state reduction of iron in olivine—planetary and meteoritic evolution
4. Single-domain grain size limits for metallic iron
5. Magnetic evidence for a partially differentiated carbonaceous chondrite parent body
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