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Mercury: Assessment of the Geology of Late Eruptions and Volatiles

Project description

Understanding volatiles distribution in Mercury’s subsurface

The MESSENGER mission revealed explosive volcanic deposits on Mercury, despite the planet’s extreme proximity to the Sun. The BepiColombo mission will further analyse Mercury’s composition using its Mercury Imaging X-ray Spectrometer (MIXS). However, key groundwork is still needed before its arrival in 2026. Supported by the Marie Skłodowska-Curie Actions programme, the MAGLEV project will study materials from Mercury’s Caloris Basin to better understand the distribution of volatiles in its subsurface and their role in magma formation. It will also analyse late-stage lavas in impact craters to explore Mercury’s thermal history, as well as test MIXS responses to synthetic analogues of key surface terrains.

Objective

The MESSENGER mission imaged explosive volcanic deposits on Mercury: a surprising result because Mercury’s proximity to the Sun should have depleted its constituents in volatiles. Mercury’s large core suggests its rocky shell was stripped by some process, which most likely would have removed its volatiles too. The volatiles’ species, how Mercury retained them, and how they were concentrated in Mercury’s magmas are unknown. Mercury’s volcanic plains formed ≥3.5 billion years ago, before magma ascent routes were closed by global contraction, but some impact craters liberated magmas for an unknown time afterward. The University of Leicester-built Mercury Imaging X-ray Spectrometer on the ESA-JAXA BepiColombo mission will measure Mercury’s composition. Mercury’s explosive volcanic deposits are important targets, but it is unknown how MIXS will respond to their exotic physical and chemical properties under different observation conditions. Vital groundwork remains to be done before BepiColombo arrives in 2026. Through the Mercury: Assessment of the Geology of Late Eruptions and Volatiles (MAGLEV) action, I will: (1) conduct an interdisciplinary study of materials excavated by Mercury’s Caloris basin to provide the deepest constraint on Mercury’s volatile subsurface distribution to assess how they were concentrated in Mercury’s magmas, with implications for the planet’s formation; (2) measure the volumes and ages of late-stage lavas found within impact craters, to inform us about the thermal evolution of Mercury and Mercury-like exoplanets, and; (3) quantify the response of the University of Leicester’s MIXS emulator to synthetic analogues of key Mercury terrains, to optimise MIXS operating parameters. By conducting MAGLEV at the Institute for Space based at Space Park Leicester, I will gain new research skills, planetary perspectives, teaching opportunities, and space mission experience, all of which will enhance my short-to-long term career development.

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HORIZON-TMA-MSCA-PF-EF - HORIZON TMA MSCA Postdoctoral Fellowships - European Fellowships

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Call for proposal

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(opens in new window) HORIZON-MSCA-2024-PF-01

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Coordinator

UNIVERSITY OF LEICESTER
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.

€ 260 347,92
Address
UNIVERSITY ROAD
LE1 7RH Leicester
United Kingdom

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Region
East Midlands (England) Leicestershire, Rutland and Northamptonshire Leicester
Activity type
Higher or Secondary Education Establishments
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Total cost

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