Anisotropy of Full and Partial Anhysteretic Remanence Across Different Rock Types: 1—Are Partial Anhysteretic Remanence Anisotropy Tensors Additive?
Author:
Affiliation:
1. Institute for Rock Magnetism University of Minnesota, Twin Cities Minneapolis MN USA
2. Institute of Geological Sciences University of Bern Bern Switzerland
3. Dougherty Family College University of St. Thomas Minneapolis MN USA
Funder
National Science Foundation
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005284
Reference100 articles.
1. Internal flow structures in columnar jointed basalt from Hrepphólar, Iceland: II. Magnetic anisotropy and rock magnetic properties
2. Composite ferromagnetic fabrics (magnetite, greigite) measured * by AMS and partial AARM in weakly strained sandstones from western Makran, Iran
3. Paleomagnetism of the Beaver Bay Complex, Minnesota
4. Grain-size-dependent remanence anisotropy and its implications for paleodirections and paleointensities – Proposing a new approach to anisotropy corrections
5. Magnetic fabrics in the Bjerkreim Sokndal Layered Intrusion, Rogaland, southern Norway: Mineral sources and geological significance
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4. Beyond the second-order magnetic anisotropy tensor: higher-order components due to oriented magnetite exsolutions in pyroxenes, and implications for palaeomagnetic and structural interpretations;Geophysical Journal International;2020-07-25
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