{"title":"建立古地磁数据质量评估的统计框架:基于最大角偏差的显著性检验","authors":"D. Heslop, A. P. Roberts","doi":"10.1029/2025JB031417","DOIUrl":null,"url":null,"abstract":"<p>Paleomagnetic data underpin our understanding of Earth's ancient magnetic field and are essential to paleogeographic reconstructions. At the specimen level, paleomagnetic analysis relies upon stepwise demagnetization to enable isolation and quantification of magnetic remanence components in geological materials. This quantification is performed typically using principal component analysis (PCA) to fit a line to stepwise demagnetization data. The quality of such PCA fits is assessed via the so-called maximum angular deviation (MAD), which is used in a heuristic fashion to represent directional uncertainty and as a selection criterion for identifying poorly or well behaved specimens. We present here a significance test that employs MAD as a statistic to compare demagnetization data against a null hypothesis of random behavior. This places MAD within a formal statistical framework that can be used to test the quality of demagnetization data before undertaking more detailed analysis. Tables of numerically estimated significance levels are provided to enable ready application of the proposed test and recommendations are made concerning the number of demagnetization data needed for statistical inference.</p>","PeriodicalId":15864,"journal":{"name":"Journal of Geophysical Research: Solid Earth","volume":"130 6","pages":""},"PeriodicalIF":3.9000,"publicationDate":"2025-06-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2025JB031417","citationCount":"0","resultStr":"{\"title\":\"Establishing a Statistical Framework for Assessing Paleomagnetic Data Quality: A Significance Test Based on Maximum Angular Deviation\",\"authors\":\"D. Heslop, A. P. Roberts\",\"doi\":\"10.1029/2025JB031417\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Paleomagnetic data underpin our understanding of Earth's ancient magnetic field and are essential to paleogeographic reconstructions. At the specimen level, paleomagnetic analysis relies upon stepwise demagnetization to enable isolation and quantification of magnetic remanence components in geological materials. This quantification is performed typically using principal component analysis (PCA) to fit a line to stepwise demagnetization data. The quality of such PCA fits is assessed via the so-called maximum angular deviation (MAD), which is used in a heuristic fashion to represent directional uncertainty and as a selection criterion for identifying poorly or well behaved specimens. We present here a significance test that employs MAD as a statistic to compare demagnetization data against a null hypothesis of random behavior. This places MAD within a formal statistical framework that can be used to test the quality of demagnetization data before undertaking more detailed analysis. Tables of numerically estimated significance levels are provided to enable ready application of the proposed test and recommendations are made concerning the number of demagnetization data needed for statistical inference.</p>\",\"PeriodicalId\":15864,\"journal\":{\"name\":\"Journal of Geophysical Research: Solid Earth\",\"volume\":\"130 6\",\"pages\":\"\"},\"PeriodicalIF\":3.9000,\"publicationDate\":\"2025-06-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2025JB031417\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Geophysical Research: Solid Earth\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1029/2025JB031417\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Solid Earth","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2025JB031417","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Establishing a Statistical Framework for Assessing Paleomagnetic Data Quality: A Significance Test Based on Maximum Angular Deviation
Paleomagnetic data underpin our understanding of Earth's ancient magnetic field and are essential to paleogeographic reconstructions. At the specimen level, paleomagnetic analysis relies upon stepwise demagnetization to enable isolation and quantification of magnetic remanence components in geological materials. This quantification is performed typically using principal component analysis (PCA) to fit a line to stepwise demagnetization data. The quality of such PCA fits is assessed via the so-called maximum angular deviation (MAD), which is used in a heuristic fashion to represent directional uncertainty and as a selection criterion for identifying poorly or well behaved specimens. We present here a significance test that employs MAD as a statistic to compare demagnetization data against a null hypothesis of random behavior. This places MAD within a formal statistical framework that can be used to test the quality of demagnetization data before undertaking more detailed analysis. Tables of numerically estimated significance levels are provided to enable ready application of the proposed test and recommendations are made concerning the number of demagnetization data needed for statistical inference.
期刊介绍:
The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology.
JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields.
JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.