Geology of the Michelangelo quadrangle (H12), Mercury

The Michelangelo quadrangle of Mercury (H12) encompasses the area between latitudes 22.5°S–65°S and longitudes 180°E–270°E. The quadrangle covers almost 6.5% of the planet’s surface with a total area of almost 5 million km2. Geologic contacts and linear features were drawn at a mapping scale between...

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Main Authors: Salvatore Buoninfante, Valentina Galluzzi, Luigi Ferranti, David A. Rothery, Harald Hiesinger, Laura Guzzetta, Felix Prüße, Benjamin Man, Annie R. Lennox, Alistair Blance, Maurizio Milano, Pasquale Palumbo
Format: Article
Language:English
Published: Taylor & Francis Group 2025-12-01
Series:Journal of Maps
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Online Access:https://www.tandfonline.com/doi/10.1080/17445647.2025.2451791
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author Salvatore Buoninfante
Valentina Galluzzi
Luigi Ferranti
David A. Rothery
Harald Hiesinger
Laura Guzzetta
Felix Prüße
Benjamin Man
Annie R. Lennox
Alistair Blance
Maurizio Milano
Pasquale Palumbo
author_facet Salvatore Buoninfante
Valentina Galluzzi
Luigi Ferranti
David A. Rothery
Harald Hiesinger
Laura Guzzetta
Felix Prüße
Benjamin Man
Annie R. Lennox
Alistair Blance
Maurizio Milano
Pasquale Palumbo
author_sort Salvatore Buoninfante
collection DOAJ
description The Michelangelo quadrangle of Mercury (H12) encompasses the area between latitudes 22.5°S–65°S and longitudes 180°E–270°E. The quadrangle covers almost 6.5% of the planet’s surface with a total area of almost 5 million km2. Geologic contacts and linear features were drawn at a mapping scale between 1:300,000 and 1:600,000, based on photointerpretation of MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) Mercury Dual Imaging System (MDIS) imagery. We distinguish three geomorphological plains units (smooth, intermediate, and intercrater plains) and, based on their degradation state, three morpho-stratigraphic classes of craters with diameter ≥ 20 km. The surface of this quadrangle is dominated by intermediate plains and by degraded crater materials of class c2. The geological map at 1:3,000,000 scale improves the existing 1:5,000,000 map based on Mariner-10 data. This work is a contribution to the Mercury geological map series planned to foster observational strategies of the ESA-JAXA BepiColombo mission.
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spelling doaj-art-f462e4d073584ed1888f3d95ee6a7c812025-01-27T16:32:26ZengTaylor & Francis GroupJournal of Maps1744-56472025-12-0121110.1080/17445647.2025.2451791Geology of the Michelangelo quadrangle (H12), MercurySalvatore Buoninfante0Valentina Galluzzi1Luigi Ferranti2David A. Rothery3Harald Hiesinger4Laura Guzzetta5Felix Prüße6Benjamin Man7Annie R. Lennox8Alistair Blance9Maurizio Milano10Pasquale Palumbo11Dipartimento di Scienze della Terra, dell’Ambiente e delle Risorse (DiSTAR), Università degli Studi di Napoli Federico II, Naples, ItalyIstituto di Astrofisica e Planetologia Spaziali (IAPS), INAF, Rome, ItalyDipartimento di Scienze della Terra, dell’Ambiente e delle Risorse (DiSTAR), Università degli Studi di Napoli Federico II, Naples, ItalySchool of Physical Sciences, The Open University, Milton Keynes, UKInstitut für Planetologie, Universität Münster, Münster, GermanyOsservatorio Astrofisico di Catania, INAF, Catania, ItalyInstitut für Planetologie, Universität Münster, Münster, GermanySchool of Physical Sciences, The Open University, Milton Keynes, UKSchool of Physical Sciences, The Open University, Milton Keynes, UKSchool of Physical Sciences, The Open University, Milton Keynes, UKDipartimento di Scienze della Terra, dell’Ambiente e delle Risorse (DiSTAR), Università degli Studi di Napoli Federico II, Naples, ItalyIstituto di Astrofisica e Planetologia Spaziali (IAPS), INAF, Rome, ItalyThe Michelangelo quadrangle of Mercury (H12) encompasses the area between latitudes 22.5°S–65°S and longitudes 180°E–270°E. The quadrangle covers almost 6.5% of the planet’s surface with a total area of almost 5 million km2. Geologic contacts and linear features were drawn at a mapping scale between 1:300,000 and 1:600,000, based on photointerpretation of MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) Mercury Dual Imaging System (MDIS) imagery. We distinguish three geomorphological plains units (smooth, intermediate, and intercrater plains) and, based on their degradation state, three morpho-stratigraphic classes of craters with diameter ≥ 20 km. The surface of this quadrangle is dominated by intermediate plains and by degraded crater materials of class c2. The geological map at 1:3,000,000 scale improves the existing 1:5,000,000 map based on Mariner-10 data. This work is a contribution to the Mercury geological map series planned to foster observational strategies of the ESA-JAXA BepiColombo mission.https://www.tandfonline.com/doi/10.1080/17445647.2025.2451791MercuryGeological map seriesMichelangelo quadrangleH12
spellingShingle Salvatore Buoninfante
Valentina Galluzzi
Luigi Ferranti
David A. Rothery
Harald Hiesinger
Laura Guzzetta
Felix Prüße
Benjamin Man
Annie R. Lennox
Alistair Blance
Maurizio Milano
Pasquale Palumbo
Geology of the Michelangelo quadrangle (H12), Mercury
Journal of Maps
Mercury
Geological map series
Michelangelo quadrangle
H12
title Geology of the Michelangelo quadrangle (H12), Mercury
title_full Geology of the Michelangelo quadrangle (H12), Mercury
title_fullStr Geology of the Michelangelo quadrangle (H12), Mercury
title_full_unstemmed Geology of the Michelangelo quadrangle (H12), Mercury
title_short Geology of the Michelangelo quadrangle (H12), Mercury
title_sort geology of the michelangelo quadrangle h12 mercury
topic Mercury
Geological map series
Michelangelo quadrangle
H12
url https://www.tandfonline.com/doi/10.1080/17445647.2025.2451791
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