Bhuvan K. Tamta, Vamdev Pathak, J. P. Shrivastava, Arun Kumar Gupta, Girish Ch. Kothyari
{"title":"东德干火山省曼德拉裂片逐流古场及虚偶极矩分析","authors":"Bhuvan K. Tamta, Vamdev Pathak, J. P. Shrivastava, Arun Kumar Gupta, Girish Ch. Kothyari","doi":"10.1007/s00024-025-03679-1","DOIUrl":null,"url":null,"abstract":"<div><p>Understanding Earth’s geodynamo processes is challenging due to limited data and the inaccessibility of Earth’s deep interior. Investigations of the Virtual Dipole Moment (VDM) and magnetic field intensity (paleofield) from continental flood basalts, such as the Deccan Volcanic Province (DVP), serve as valuable proxies for understanding past magnetic field behavior and core-mantle boundary (CMB) interactions. This study presents the first attempt to determine flow-by-flow paleofield and VDM analysis through progressive AF and thermal demagnetization of 36 distinct lava flows from the Mandla lobe, eastern DVP. Reliable mean VDM and paleofield values were calculated based on specimens that met reliability criteria and were globally correlated with the PINT database. The mean VDM value obtained from the eastern DVP is 1.58 ± 0.43 × 10<sup>22</sup> Am<sup>2</sup>, which aligns with VDM values reported from the Koyna region, western DVP, indicating a persistently weak Earth’s magnetic field across the DVP. The lowest VDM value of 0.62 ± 0.19 × 10<sup>22</sup> Am<sup>2</sup>, obtained from eight physically distinct lava flows of intermediate polarity, suggests these flows erupted during periods of weak Earth’s magnetic field, implying non-sudden polarity reversals.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"182 2","pages":"571 - 586"},"PeriodicalIF":1.9000,"publicationDate":"2025-02-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Flow-by-Flow Paleofield and Virtual Dipole Moment Analysis in the Mandla Lobe, Eastern Deccan Volcanic Province\",\"authors\":\"Bhuvan K. Tamta, Vamdev Pathak, J. P. Shrivastava, Arun Kumar Gupta, Girish Ch. Kothyari\",\"doi\":\"10.1007/s00024-025-03679-1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Understanding Earth’s geodynamo processes is challenging due to limited data and the inaccessibility of Earth’s deep interior. Investigations of the Virtual Dipole Moment (VDM) and magnetic field intensity (paleofield) from continental flood basalts, such as the Deccan Volcanic Province (DVP), serve as valuable proxies for understanding past magnetic field behavior and core-mantle boundary (CMB) interactions. This study presents the first attempt to determine flow-by-flow paleofield and VDM analysis through progressive AF and thermal demagnetization of 36 distinct lava flows from the Mandla lobe, eastern DVP. Reliable mean VDM and paleofield values were calculated based on specimens that met reliability criteria and were globally correlated with the PINT database. The mean VDM value obtained from the eastern DVP is 1.58 ± 0.43 × 10<sup>22</sup> Am<sup>2</sup>, which aligns with VDM values reported from the Koyna region, western DVP, indicating a persistently weak Earth’s magnetic field across the DVP. The lowest VDM value of 0.62 ± 0.19 × 10<sup>22</sup> Am<sup>2</sup>, obtained from eight physically distinct lava flows of intermediate polarity, suggests these flows erupted during periods of weak Earth’s magnetic field, implying non-sudden polarity reversals.</p></div>\",\"PeriodicalId\":21078,\"journal\":{\"name\":\"pure and applied geophysics\",\"volume\":\"182 2\",\"pages\":\"571 - 586\"},\"PeriodicalIF\":1.9000,\"publicationDate\":\"2025-02-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"pure and applied geophysics\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s00024-025-03679-1\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"pure and applied geophysics","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s00024-025-03679-1","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Flow-by-Flow Paleofield and Virtual Dipole Moment Analysis in the Mandla Lobe, Eastern Deccan Volcanic Province
Understanding Earth’s geodynamo processes is challenging due to limited data and the inaccessibility of Earth’s deep interior. Investigations of the Virtual Dipole Moment (VDM) and magnetic field intensity (paleofield) from continental flood basalts, such as the Deccan Volcanic Province (DVP), serve as valuable proxies for understanding past magnetic field behavior and core-mantle boundary (CMB) interactions. This study presents the first attempt to determine flow-by-flow paleofield and VDM analysis through progressive AF and thermal demagnetization of 36 distinct lava flows from the Mandla lobe, eastern DVP. Reliable mean VDM and paleofield values were calculated based on specimens that met reliability criteria and were globally correlated with the PINT database. The mean VDM value obtained from the eastern DVP is 1.58 ± 0.43 × 1022 Am2, which aligns with VDM values reported from the Koyna region, western DVP, indicating a persistently weak Earth’s magnetic field across the DVP. The lowest VDM value of 0.62 ± 0.19 × 1022 Am2, obtained from eight physically distinct lava flows of intermediate polarity, suggests these flows erupted during periods of weak Earth’s magnetic field, implying non-sudden polarity reversals.
期刊介绍:
pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys.
Long running journal, founded in 1939 as Geofisica pura e applicata
Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences
Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research
Coverage extends to research topics in oceanic sciences
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