Geology of the Neruda quadrangle (H13), Mercury

IF 1.9 4区 地球科学 Q2 GEOGRAPHY
Benjamin Man, David A. Rothery, Matthew R. Balme, Susan J. Conway, Jack Wright, David L. Pegg, Annie R. Lennox, Salvatore Buoninfante
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引用次数: 0

Abstract

We present the first geological map of the Neruda Quadrangle (H13), Mercury. H13 is in Mercury’s southern hemisphere between latitudes 22.5°S–65°S, and longitudes 90°E–180° covering a total area of just under 5 million km², equivalent to 6.5% of the planet’s surface. Map digitisation was carried out at scales between 1:300,000 and 1:700,000 for final presentation at 1:3,000,0000, from end-of-mission data products from NASA’s MESSENGER mission. We distinguish three main photogeologic plains units: intercrater, intermediate, and smooth plains. We also distinguish all craters and their materials ≥ 20 km in diameter based on their degradation state. We have completed two versions of the map, one using a three-class crater degradation scheme and one using a five-class crater degradation scheme. In addition, specific geological units were charted for the Rembrandt impact basin. This map has been constructed to provide context and targets for the ESA-JAXA BepiColombo mission to Mercury.
聂鲁达四边形的地质(H13),水星
我们展示了水星聂鲁达四边形(H13)的第一张地质图。H13位于水星的南半球,在纬度22.5°S - 65°S,经度90°E-180°之间,总面积不到500万平方公里,相当于水星表面的6.5%。地图数字化以1:30万至1:70万的比例进行,最终以1:30万的比例呈现,这些数据来自美国宇航局信使号任务的任务结束数据产品。我们区分了三个主要的光地质平原单位:火山口间平原、中间平原和平滑平原。我们还根据陨石坑的降解状态来区分直径≥20 km的陨石坑及其材料。我们已经完成了两个版本的地图,一个使用三级火山口降解方案,另一个使用五级火山口降解方案。此外,还绘制了伦勃朗撞击盆地的具体地质单元图。这张地图为ESA-JAXA的BepiColombo水星任务提供了背景和目标。
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来源期刊
Journal of Maps
Journal of Maps 地学-自然地理
CiteScore
4.30
自引率
9.10%
发文量
83
审稿时长
6-12 weeks
期刊介绍: The Journal of Maps is a peer-reviewed, inter-disciplinary, online journal that aims to provide a forum for researchers to publish maps and spatial diagrams.
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