东德干火山省曼德拉裂片逐流古场及虚偶极矩分析

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Bhuvan K. Tamta, Vamdev Pathak, J. P. Shrivastava, Arun Kumar Gupta, Girish Ch. Kothyari
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引用次数: 0

摘要

了解地球的地球动力学过程是具有挑战性的,因为有限的数据和地球的深层内部难以接近。大陆洪水玄武岩(如德干火山省(DVP))的虚拟偶极矩(VDM)和磁场强度(古场)的研究,为理解过去的磁场行为和核幔边界(CMB)相互作用提供了有价值的代理。本研究首次尝试通过对DVP东部曼德拉叶36条不同熔岩流的渐进AF和热消磁来确定逐流古场和VDM分析。可靠的平均VDM和古场值是基于满足可靠性标准的样本计算的,并与PINT数据库全局相关。从东部DVP获得的平均VDM值为1.58±0.43 × 1022 Am2,这与从西部DVP的Koyna地区报告的VDM值一致,表明地球磁场持续微弱。从8个物理上不同的中极性熔岩流中获得的最低VDM值为0.62±0.19 × 1022 Am2,表明这些熔岩流在弱地球磁场期间喷发,这意味着非突然的极性反转。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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.

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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
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 See Instructions for Authors on the right hand side.
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