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The Chromite Record of Mafic Crustal Growth

Project description

Exploring Earth's mafic crustal growth using chromite analysis

Current understanding of Earth's crustal growth relies heavily on zircon analysis, primarily revealing felsic crustal growth while overlooking early Earth's mafic crust. The ERC-funded project ChroMCrust aims to deepen knowledge of Earth's mafic crustal development, essential for studying tectonic evolution and early continent formation. Moving beyond zircon, this study analyses detrital chromite in Archaean Craton sedimentary rocks. Chromite’s chemical properties and Re-Os isotope dating will help identify the origins and ages of mafic terranes. Key goals include developing chromite analysis techniques for ancient rocks, constructing a mafic-ultramafic growth timeline for an Archaean continental nucleus, and seeking Earth's earliest mafic crust. This novel approach will broaden our knowledge of sedimentary provenance, uncover mafic crustal development, and provide new insights into Earth's primitive crust.

Objective

Understanding Earth's crustal growth is crucial to understanding the evolution of its tectonics, the birth of the first continents, and the fundamental changes that transformed Earth into a habitable planet. However, much of our understanding of Earth's crustal growth is predicated on a single mineral - zircon - that is strongly biased towards detecting felsic crustal growth. This is particularly problematic for the early Earth, where average crustal compositions were far more mafic than today, and the very first protocrust may be entirely undetectable using conventional methods. I propose to access the mafic to ultramafic crustal growth record using detrital chromite preserved in sedimentary rocks from Archaean Cratons. Like zircon, chromite chemical compositions reflect the magmas that they crystallised from, and can be used to identify the provenance of the mafic portions of a sedimentary rock. Furthermore, they can be dated using Re-Os isotopes, to identify the age of eroded mafic terranes. This project has three main objectives:

1. Develop techniques to identify the age and composition of chromite sources in ancient sedimentary rocks.
2. Use a range of detrital chromite samples from sedimentary sequences in the Superior Craton, to reconstruct a mafic-ultramafic crustal growth curve for the craton.
3. Search for evidence of Earth's mafic protocrust in some of the oldest known chromite-bearing sedimentary rocks.

These achievements will open a new avenue for studying sedimentary provenance, unlock the archive of mafic crustal growth throughout Earth history, and provide insights on the nature and survival of Earth's earliest crust. The techniques developed will be broadly applicable, paving the way for a better understanding of Earth's crustal evolution.

Fields of science (EuroSciVoc)

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Keywords

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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

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(opens in new window) ERC-2023-STG

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Host institution

KOBENHAVNS UNIVERSITET
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.

€ 1 499 536,00
Address
NORREGADE 10
1165 KOBENHAVN
Denmark

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Region
Danmark Hovedstaden Byen København
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.

€ 1 499 536,00

Beneficiaries (1)

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