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Nanomagnetic Tomography: Unlocking the Vortex Realm for Paleomagnetism and Rock-magnetism

Project description

Harnessing special particles to reconstruct the Earth’s magnetic history

Hidden magnetic data stored in tiny, stable particles within geological materials hold the key to understanding Earth’s magnetic history. Known as vortex-state particles, these particles are predicted to reliably record the Earth’s magnetic field. However, current methods cannot detect or analyse them, leaving much of this valuable information inaccessible. The ERC-funded SPARK project will pioneer a new technique called nanomagnetic tomography. This method isolates and analyses magnetic signals from these tiny, reliable vortex-state particles. By systematically studying their stability based on size, shape and mineral composition, SPARK will create reliable protocols to reconstruct the Earth’s magnetic field.

Objective

The Earth’s magnetic field plays a pivotal role in the Earth Sciences: magnetic signals stored in geological materials, such as igneous rocks, provide a record of Earth’s magnetic history and are essential for understanding e.g. tectonic processes, planetary dynamics, and the behavior of the geomagnetic field itself. Much of this record, however, remains inaccessible because not all magnetic particles in a sample reliably record the Earth’s magnetic field. Small, sub-micron vortex-state particles are predicted to be stable and reliable recorders, but they are undetectable by current micromagnetic methods. SPARK propels paleomagnetism into the nano realm by isolating and analyzing magnetic signals exclusively from these tiny but reliable particles, unlocking a wealth of hidden paleomagnetic data.

Therefore, SPARK will pioneer Nanomagnetic Tomography, a technique designed to isolate and analyze signals from only the most reliable vortex-state particles in a sample. By systematically assessing their magnetic stability as function of their size, shape, and mineralogy, SPARK will identify which particles are dependable recorders and which should be excluded. Building on this foundation, it will develop robust and efficient protocols to reconstruct the past direction and intensity of the Earth’s magnetic field, especially from magnetically complex materials that conventional methods cannot reliably analyze.

This transformative approach will revolutionize paleomagnetic research, providing unprecedented insights into enigmatic periods of Earth’s magnetic history, such as the Devonian and Ediacaran, as well as the dynamics of geomagnetic reversals and anomalies like the South Atlantic Anomaly. Beyond igneous rocks, SPARK’s methodologies will redefine studies of e.g. the oldest rocks on Earth, meteorites, and extraterrestrial samples, opening entirely new frontiers in understanding planetary evolution across the Solar System.

Fields of science (EuroSciVoc)

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Programme(s)

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Topic(s)

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Funding Scheme

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HORIZON-ERC - HORIZON ERC Grants

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Call for proposal

Procedure for inviting applicants to submit project proposals, with the aim of receiving EU funding.

(opens in new window) ERC-2025-COG

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Host institution

UNIVERSITEIT UTRECHT
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 2 977 831,00
Address
HEIDELBERGLAAN 8
3584 CS Utrecht
Netherlands

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Activity type
Higher or Secondary Education Establishments
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Total cost

The total costs incurred by this organisation to participate in the project, including direct and indirect costs. This amount is a subset of the overall project budget.

€ 2 977 831,00

Beneficiaries (1)

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