On the reliability of the AMS ellipsoid by statistical methods
Weak magnetic materials whose susceptibility values are close to the instrument's accuracy show very large errors in the direct evaluation of their ellipsoid parameters. This may lead to misinterpretation of the magnetic fabric, which is often used as a geological indicator. In order to estimat...
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Published in: | Tectonophysics Vol. 629; pp. 75 - 86 |
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Abstract | Weak magnetic materials whose susceptibility values are close to the instrument's accuracy show very large errors in the direct evaluation of their ellipsoid parameters. This may lead to misinterpretation of the magnetic fabric, which is often used as a geological indicator. In order to estimate the measurement uncertainties, several statistical methods have been proposed. Within the available statistical methods, the Linear Perturbation Analysis (Hext, 1963) and the non-parametric bootstrap (Constable and Tauxe, 1990) technique have been widely used. In this paper, we make a complete study about these methods to estimate their limitations when applied to n measurements of a single sample. We will analyze which method is better in terms of uncertainties, we will determine when the methods do not provide reliable results and we will establish a measuring protocol. For that, we run simulations for the Linear Perturbation Analysis and the non-parametric bootstrap varying i) the number of measurements, ii) the instrumental error and iii) the shape parameter and the anisotropy degree of the AMS ellipsoid. The results show that both methods are not reliable when the difference between eigenvalues is too close in relation to the instrumental error, but increasing the number of measurements can improve the results.
[Display omitted]
•Analyzing the reliability of Hext and bootstrap methods to estimate the AMS ellipsoid.•Using different configurations of errors, AMS parameters and number of measurements.•Methods are not reliable when the eigenvalues are too close.•Increasing number of measurements provide smaller errors and better reliability. |
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AbstractList | Weak magnetic materials whose susceptibility values are close to the instrument's accuracy show very large errors in the direct evaluation of their ellipsoid parameters. This may lead to misinterpretation of the magnetic fabric, which is often used as a geological indicator. In order to estimate the measurement uncertainties, several statistical methods have been proposed. Within the available statistical methods, the Linear Perturbation Analysis (Hext, 1963) and the non-parametric bootstrap (Constable and Tauxe, 1990) technique have been widely used. In this paper, we make a complete study about these methods to estimate their limitations when applied to n measurements of a single sample. We will analyze which method is better in terms of uncertainties, we will determine when the methods do not provide reliable results and we will establish a measuring protocol. For that, we run simulations for the Linear Perturbation Analysis and the non-parametric bootstrap varying i) the number of measurements, ii) the instrumental error and iii) the shape parameter and the anisotropy degree of the AMS ellipsoid. The results show that both methods are not reliable when the difference between eigenvalues is too close in relation to the instrumental error, but increasing the number of measurements can improve the results Weak magnetic materials whose susceptibility values are close to the instrument's accuracy show very large errors in the direct evaluation of their ellipsoid parameters. This may lead to misinterpretation of the magnetic fabric, which is often used as a geological indicator. In order to estimate the measurement uncertainties, several statistical methods have been proposed. Within the available statistical methods, the Linear Perturbation Analysis (Hext, 1963) and the non-parametric bootstrap (Constable and Tauxe, 1990) technique have been widely used. In this paper, we make a complete study about these methods to estimate their limitations when applied to n measurements of a single sample. We will analyze which method is better in terms of uncertainties, we will determine when the methods do not provide reliable results and we will establish a measuring protocol. For that, we run simulations for the Linear Perturbation Analysis and the non-parametric bootstrap varying i) the number of measurements, ii) the instrumental error and iii) the shape parameter and the anisotropy degree of the AMS ellipsoid. The results show that both methods are not reliable when the difference between eigenvalues is too close in relation to the instrumental error, but increasing the number of measurements can improve the results. [Display omitted] •Analyzing the reliability of Hext and bootstrap methods to estimate the AMS ellipsoid.•Using different configurations of errors, AMS parameters and number of measurements.•Methods are not reliable when the eigenvalues are too close.•Increasing number of measurements provide smaller errors and better reliability. |
Author | Martín-Hernández, F. Guerrero-Suarez, S. |
Author_xml | – sequence: 1 givenname: S. surname: Guerrero-Suarez fullname: Guerrero-Suarez, S. email: saguerre@ucm.es – sequence: 2 givenname: F. surname: Martín-Hernández fullname: Martín-Hernández, F. |
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CitedBy_id | crossref_primary_10_1016_j_pepi_2024_107159 crossref_primary_10_1016_j_earscirev_2020_103385 crossref_primary_10_1016_j_tecto_2014_06_002 |
Cites_doi | 10.1007/BF01613632 10.1029/JB095iB06p08383 10.1093/biomet/50.3-4.353 10.1007/s11200-010-0079-6 10.1029/95GL01910 10.1046/j.1365-246X.2002.01731.x 10.1016/j.jappgeo.2012.10.008 10.1046/j.1365-246x.2000.00174.x 10.1029/92RG00733 10.1038/356511a0 10.1007/s00024-008-0361-5 10.1016/S0012-8252(96)00044-X 10.1016/S0079-1946(97)00090-6 10.1029/95RG00341 10.1016/j.tecto.2005.12.019 10.1016/j.jsg.2009.09.006 10.1029/1999GL008439 10.1016/0031-9201(93)90101-E 10.1016/0040-1951(81)90110-4 10.1016/0377-0273(94)00110-3 10.3150/08-BEJ154 |
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Keywords | Bootstrap Anisotropy of Magnetic Susceptibility Linear Perturbation Analysis Rock magnetism |
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Geophys. doi: 10.1029/92RG00733 contributor: fullname: Rochette – volume: 356 start-page: 511 year: 1992 ident: 10.1016/j.tecto.2014.04.010_bb0050 article-title: Evidence from magnetic fabric for the flow pattern of magma in the Mackenzie giant radiating dyke swarm publication-title: Nature doi: 10.1038/356511a0 contributor: fullname: Ernst – volume: 165 start-page: 1411 year: 2008 ident: 10.1016/j.tecto.2014.04.010_bb0025 article-title: Induced magnetization of magnetite–titanomagnetite in alternating fields ranging from 400a/m to 80,000a/m; low-field susceptibility (100–400a/m) and beyond publication-title: Pure Appl. Geophys. doi: 10.1007/s00024-008-0361-5 contributor: fullname: Borradaile – volume: 42 start-page: 49 year: 1997 ident: 10.1016/j.tecto.2014.04.010_bb0010 article-title: Tectonic applications of magnetic susceptibility and its anisotropy publication-title: Earth Sci. Rev. doi: 10.1016/S0012-8252(96)00044-X contributor: fullname: Borradaile – volume: 22 start-page: 131 year: 1997 ident: 10.1016/j.tecto.2014.04.010_bb0150 article-title: Experimental designs for determination of the anisotropy of remanence-test of the efficiency of least-square and bootstrap methods applied to metamorphic rocks from southern Poland publication-title: Phys. Chem. Earth doi: 10.1016/S0079-1946(97)00090-6 contributor: fullname: Werner – volume: 71–80 year: 1982 ident: 10.1016/j.tecto.2014.04.010_bb0100 article-title: The Fisher–Bingham distribution on the sphere publication-title: J. R. Stat. Soc. Ser. B Methodol. contributor: fullname: Kent – year: 1998 ident: 10.1016/j.tecto.2014.04.010_bb0140 contributor: fullname: Tauxe – volume: 33 start-page: 129 year: 1995 ident: 10.1016/j.tecto.2014.04.010_bb0105 article-title: Magnetic fabrics publication-title: Rev. Geophys. doi: 10.1029/95RG00341 contributor: fullname: Kodama – volume: Volume 1 year: 1997 ident: 10.1016/j.tecto.2014.04.010_bb0040 contributor: fullname: Davison – volume: 418 start-page: 63 year: 2006 ident: 10.1016/j.tecto.2014.04.010_bb0130 article-title: Magnetic anisotropy of calcite at room-temperature publication-title: Tectonophysics doi: 10.1016/j.tecto.2005.12.019 contributor: fullname: Schmidt – volume: 32 start-page: 1519 year: 2010 ident: 10.1016/j.tecto.2014.04.010_bb0020 article-title: Structural geology, petrofabrics and magnetic fabrics (AMS, AARM, AIRM) publication-title: J. Struct. Geol. doi: 10.1016/j.jsg.2009.09.006 contributor: fullname: Borradaile – volume: 27 start-page: 2985 year: 2000 ident: 10.1016/j.tecto.2014.04.010_bb0115 article-title: Statistical analysis of normalized and unnormalized second-rank tensor data, with application to measurements of anisotropy of magnetic susceptibility publication-title: Geophys. Res. Lett. doi: 10.1029/1999GL008439 contributor: fullname: Owens – volume: 77 start-page: 237 year: 1993 ident: 10.1016/j.tecto.2014.04.010_bb0070 article-title: Theoretical models of magnetic anisotropy to strain relationship revisited publication-title: Phys. Earth Planet. Inter. doi: 10.1016/0031-9201(93)90101-E contributor: fullname: Hrouda – volume: 79 start-page: T63 year: 1981 ident: 10.1016/j.tecto.2014.04.010_bb0095 article-title: Characterization of the magnetic fabric of rocks publication-title: Tectonophysics doi: 10.1016/0040-1951(81)90110-4 contributor: fullname: Jelinek – year: 1993 ident: 10.1016/j.tecto.2014.04.010_bb0135 contributor: fullname: Tarling – volume: Volume 3 year: 2001 ident: 10.1016/j.tecto.2014.04.010_bb0045 contributor: fullname: Dunlop – volume: 65 start-page: 249 year: 1995 ident: 10.1016/j.tecto.2014.04.010_bb0030 article-title: Magnetic fabric and flow direction in basaltic pahoehoe lava of xitle volcano, Mexico publication-title: J. Volcanol. Geotherm. Res. doi: 10.1016/0377-0273(94)00110-3 contributor: fullname: Cañón-Tapia – volume: 15 start-page: 380 year: 2009 ident: 10.1016/j.tecto.2014.04.010_bb0055 article-title: Tie-respecting bootstrap methods for estimating distributions of sets and functions of eigenvalues publication-title: Bernoulli doi: 10.3150/08-BEJ154 contributor: fullname: Hall |
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Snippet | Weak magnetic materials whose susceptibility values are close to the instrument's accuracy show very large errors in the direct evaluation of their ellipsoid... |
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SubjectTerms | Anisotropy of Magnetic Susceptibility Bootstrap Eigenvalues Ellipsoids Error analysis Errors Estimates Linear Perturbation Analysis Perturbation methods Rock magnetism Statistical methods Uncertainty |
Title | On the reliability of the AMS ellipsoid by statistical methods |
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