Geology of the Derain quadrangle (H10), Mercury

ABSTRACTWe present the results of geological mapping of Mercury’s Derain (H10) quadrangle (0°-72°E and 22.5°N-22.5°S) using data from the MESSENGER spacecraft. The map is presented on a scale of 1:3,000,000, for which linework was drawn at 1:300,000. We distinguish three major morphological plains u...

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Main Authors: Christopher C. Malliband, David A. Rothery, Matthew R. Balme, Susan J. Conway, David L. Pegg, Jack Wright
Format: Article
Language:English
Published: Taylor & Francis Group 2023-12-01
Series:Journal of Maps
Subjects:
Online Access:https://www.tandfonline.com/doi/10.1080/17445647.2022.2112774
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author Christopher C. Malliband
David A. Rothery
Matthew R. Balme
Susan J. Conway
David L. Pegg
Jack Wright
author_facet Christopher C. Malliband
David A. Rothery
Matthew R. Balme
Susan J. Conway
David L. Pegg
Jack Wright
author_sort Christopher C. Malliband
collection DOAJ
description ABSTRACTWe present the results of geological mapping of Mercury’s Derain (H10) quadrangle (0°-72°E and 22.5°N-22.5°S) using data from the MESSENGER spacecraft. The map is presented on a scale of 1:3,000,000, for which linework was drawn at 1:300,000. We distinguish three major morphological plains units: Smooth, Intermediate, and Intercrater Plains. We produced two versions of the map, with craters classified according to a 3- and 5-class degradation system. This allows compatibility with other MESSENGER-era maps and Mariner 10-era maps. This map will help provide science context for the ESA-JAXA BepiColombo mission to Mercury.
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spelling doaj.art-f1dceda5ff6042e4b7906184bfaf097e2023-06-20T20:31:50ZengTaylor & Francis GroupJournal of Maps1744-56472023-12-0119110.1080/17445647.2022.2112774Geology of the Derain quadrangle (H10), MercuryChristopher C. Malliband0David A. Rothery1Matthew R. Balme2Susan J. Conway3David L. Pegg4Jack Wright5Department of Physical Sciences, The Open University, Walton Hall, Milton Keynes, UKDepartment of Physical Sciences, The Open University, Walton Hall, Milton Keynes, UKDepartment of Physical Sciences, The Open University, Walton Hall, Milton Keynes, UKCNRS, UMR 6112 Laboratoire de Planétologie et Géodynamique, Université de Nantes, Nantes, FranceDepartment of Physical Sciences, The Open University, Walton Hall, Milton Keynes, UKDepartment of Physical Sciences, The Open University, Walton Hall, Milton Keynes, UKABSTRACTWe present the results of geological mapping of Mercury’s Derain (H10) quadrangle (0°-72°E and 22.5°N-22.5°S) using data from the MESSENGER spacecraft. The map is presented on a scale of 1:3,000,000, for which linework was drawn at 1:300,000. We distinguish three major morphological plains units: Smooth, Intermediate, and Intercrater Plains. We produced two versions of the map, with craters classified according to a 3- and 5-class degradation system. This allows compatibility with other MESSENGER-era maps and Mariner 10-era maps. This map will help provide science context for the ESA-JAXA BepiColombo mission to Mercury.https://www.tandfonline.com/doi/10.1080/17445647.2022.2112774Mercuryplanetary geologyDerainimpact processesplanetary resurfacing
spellingShingle Christopher C. Malliband
David A. Rothery
Matthew R. Balme
Susan J. Conway
David L. Pegg
Jack Wright
Geology of the Derain quadrangle (H10), Mercury
Journal of Maps
Mercury
planetary geology
Derain
impact processes
planetary resurfacing
title Geology of the Derain quadrangle (H10), Mercury
title_full Geology of the Derain quadrangle (H10), Mercury
title_fullStr Geology of the Derain quadrangle (H10), Mercury
title_full_unstemmed Geology of the Derain quadrangle (H10), Mercury
title_short Geology of the Derain quadrangle (H10), Mercury
title_sort geology of the derain quadrangle h10 mercury
topic Mercury
planetary geology
Derain
impact processes
planetary resurfacing
url https://www.tandfonline.com/doi/10.1080/17445647.2022.2112774
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