The Impact of Grain‐Size Distributions of Iron‐Oxides on Paleomagnetic Measurements
Abstract Magnetic signals in igneous rocks arise from assemblages of iron‐oxide bearing minerals that differ in for example, size, shape, and chemistry. Paleomagnetic measurements on bulk samples measure millions of such grains simultaneously, producing a statistical ensemble of the magnetic moments...
| Published in: | Geochemistry, Geophysics, Geosystems |
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| Main Authors: | , , , |
| Format: | Article |
| Language: | English |
| Published: |
Wiley
2024-04-01
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| Subjects: | |
| Online Access: | https://doi.org/10.1029/2024GC011512 |
| _version_ | 1849857709092896768 |
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| author | Frenk Out Rosa A. deBoer John Walmsley Lennart V. deGroot |
| author_facet | Frenk Out Rosa A. deBoer John Walmsley Lennart V. deGroot |
| author_sort | Frenk Out |
| collection | DOAJ |
| container_title | Geochemistry, Geophysics, Geosystems |
| description | Abstract Magnetic signals in igneous rocks arise from assemblages of iron‐oxide bearing minerals that differ in for example, size, shape, and chemistry. Paleomagnetic measurements on bulk samples measure millions of such grains simultaneously, producing a statistical ensemble of the magnetic moments of the individual grains. Scanning magnetometry techniques such as the Quantum Diamond Microscope (QDM) measure magnetic signals on micrometer scales, allowing the identification of magnetic moments of individual grains in a sample using for example, Micromagnetic Tomography (MMT). Here we produce a grain‐size distribution of iron‐oxides in a typical Hawaiian basalt from the superparamagnetic threshold (∼40 nm) to grains with a diameter of 10 µm. This grain‐size distribution is obtained by combining FIB‐SEM and MicroCT data from sister specimens, and normalizing them to the mineral surface area of non‐magnetic minerals. Then we use this grain‐size distribution to determine the contributions of individual magnetic carriers to bulk magnetic measurements and surface magnetometry. We found that measurements on bulk samples are sensitive to relatively small grain sizes in the realm of single domain or vortex states (<200 nm), while signals in surface magnetometry arise mainly from larger grains with diameters >1 µm. This implies that bulk measurements cannot be compared straightforwardly to signals from surface magnetometry from the same sample. Moreover, our observations explain why MMT results are insensitive to the presence of many small grains in a sample that intuitively should hamper their outcome. |
| format | Article |
| id | doaj-art-b18c75e9edea4d4abc73cfd84d912fbe |
| institution | Directory of Open Access Journals |
| issn | 1525-2027 |
| language | English |
| publishDate | 2024-04-01 |
| publisher | Wiley |
| record_format | Article |
| spelling | doaj-art-b18c75e9edea4d4abc73cfd84d912fbe2025-08-20T01:21:11ZengWileyGeochemistry, Geophysics, Geosystems1525-20272024-04-01254n/an/a10.1029/2024GC011512The Impact of Grain‐Size Distributions of Iron‐Oxides on Paleomagnetic MeasurementsFrenk Out0Rosa A. deBoer1John Walmsley2Lennart V. deGroot3Department of Earth Sciences Paleomagnetic Laboratory Fort Hoofddijk Utrecht University Utrecht The NetherlandsDepartment of Earth Sciences Paleomagnetic Laboratory Fort Hoofddijk Utrecht University Utrecht The NetherlandsDepartment of Materials Science & Metallurgy University of Cambridge Cambridge UKDepartment of Earth Sciences Paleomagnetic Laboratory Fort Hoofddijk Utrecht University Utrecht The NetherlandsAbstract Magnetic signals in igneous rocks arise from assemblages of iron‐oxide bearing minerals that differ in for example, size, shape, and chemistry. Paleomagnetic measurements on bulk samples measure millions of such grains simultaneously, producing a statistical ensemble of the magnetic moments of the individual grains. Scanning magnetometry techniques such as the Quantum Diamond Microscope (QDM) measure magnetic signals on micrometer scales, allowing the identification of magnetic moments of individual grains in a sample using for example, Micromagnetic Tomography (MMT). Here we produce a grain‐size distribution of iron‐oxides in a typical Hawaiian basalt from the superparamagnetic threshold (∼40 nm) to grains with a diameter of 10 µm. This grain‐size distribution is obtained by combining FIB‐SEM and MicroCT data from sister specimens, and normalizing them to the mineral surface area of non‐magnetic minerals. Then we use this grain‐size distribution to determine the contributions of individual magnetic carriers to bulk magnetic measurements and surface magnetometry. We found that measurements on bulk samples are sensitive to relatively small grain sizes in the realm of single domain or vortex states (<200 nm), while signals in surface magnetometry arise mainly from larger grains with diameters >1 µm. This implies that bulk measurements cannot be compared straightforwardly to signals from surface magnetometry from the same sample. Moreover, our observations explain why MMT results are insensitive to the presence of many small grains in a sample that intuitively should hamper their outcome.https://doi.org/10.1029/2024GC011512paleomagnetismiron‐oxidesgrain‐size distributionmicromagnetic tomographyFIB‐SEMghost grains |
| spellingShingle | Frenk Out Rosa A. deBoer John Walmsley Lennart V. deGroot The Impact of Grain‐Size Distributions of Iron‐Oxides on Paleomagnetic Measurements paleomagnetism iron‐oxides grain‐size distribution micromagnetic tomography FIB‐SEM ghost grains |
| title | The Impact of Grain‐Size Distributions of Iron‐Oxides on Paleomagnetic Measurements |
| title_full | The Impact of Grain‐Size Distributions of Iron‐Oxides on Paleomagnetic Measurements |
| title_fullStr | The Impact of Grain‐Size Distributions of Iron‐Oxides on Paleomagnetic Measurements |
| title_full_unstemmed | The Impact of Grain‐Size Distributions of Iron‐Oxides on Paleomagnetic Measurements |
| title_short | The Impact of Grain‐Size Distributions of Iron‐Oxides on Paleomagnetic Measurements |
| title_sort | impact of grain size distributions of iron oxides on paleomagnetic measurements |
| topic | paleomagnetism iron‐oxides grain‐size distribution micromagnetic tomography FIB‐SEM ghost grains |
| url | https://doi.org/10.1029/2024GC011512 |
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