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Geology of the Derain quadrangle (H10), Mercury
by
Balme, Matthew R.
, Malliband, Christopher C.
, Conway, Susan J.
, Pegg, David L.
, Rothery, David A.
, Wright, Jack
in
Derain
/ Earth Sciences
/ Geologic mapping
/ Geological mapping
/ Geology
/ impact processes
/ Mapping
/ Mercury
/ Mercury (planet)
/ Mercury surface
/ MESSENGER Mission
/ MESSENGER Spacecraft
/ Morphology
/ Physical sciences
/ planetary geology
/ planetary resurfacing
/ Planetology
/ Sciences of the Universe
/ Space missions
/ Spacecraft
/ Topography
2023
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Geology of the Derain quadrangle (H10), Mercury
by
Balme, Matthew R.
, Malliband, Christopher C.
, Conway, Susan J.
, Pegg, David L.
, Rothery, David A.
, Wright, Jack
in
Derain
/ Earth Sciences
/ Geologic mapping
/ Geological mapping
/ Geology
/ impact processes
/ Mapping
/ Mercury
/ Mercury (planet)
/ Mercury surface
/ MESSENGER Mission
/ MESSENGER Spacecraft
/ Morphology
/ Physical sciences
/ planetary geology
/ planetary resurfacing
/ Planetology
/ Sciences of the Universe
/ Space missions
/ Spacecraft
/ Topography
2023
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Geology of the Derain quadrangle (H10), Mercury
by
Balme, Matthew R.
, Malliband, Christopher C.
, Conway, Susan J.
, Pegg, David L.
, Rothery, David A.
, Wright, Jack
in
Derain
/ Earth Sciences
/ Geologic mapping
/ Geological mapping
/ Geology
/ impact processes
/ Mapping
/ Mercury
/ Mercury (planet)
/ Mercury surface
/ MESSENGER Mission
/ MESSENGER Spacecraft
/ Morphology
/ Physical sciences
/ planetary geology
/ planetary resurfacing
/ Planetology
/ Sciences of the Universe
/ Space missions
/ Spacecraft
/ Topography
2023
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Journal Article
Geology of the Derain quadrangle (H10), Mercury
2023
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Overview
We 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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