{"title":"Clusters of irregular patches on the Moon: A new GIS-based catalog","authors":"H.I. Hargitai , P. Brož","doi":"10.1016/j.icarus.2024.116439","DOIUrl":null,"url":null,"abstract":"<div><div>The aim of this work was to systematically map cluster-forming Irregular Patches (IPs) on the Moon. These features, formerly termed “Irregular Mare Patches”, are enigmatic features situated on the near side of the Moon, mostly in mare regions. IPs are pristine-looking features with textures at the meter scale, suggesting they formed millions of years ago on top of several-billion-year-old mare basalts. Morphologic and spectral studies could not provide conclusive evidence of their formative processes, or their age. Theories on their formation concentrate around three conflicting models - that they are formed by compact basalts and are only a few tens of millions of years old; that they are formed by mass wasting processes capable to remove regolith to this day; or that they are composed of lava foams and their age is the same as the host terrain's, i.e. billions of years. We present a GIS-based analysis to examine which formation model is supported by their geography. Previous catalogs mapped IPs ambiguously, with one single coordinate representing one unit or a group of units, with many isolated units around them remaining unmapped. To change that, we mapped isolated IPs individually as polygons because we wanted to reveal their areas and their local-scale distribution patterns, which were not identifiable from previous mapping efforts. We named the isolated, elemental depressions <em>Irregular Patches</em> to differentiate them from previous works. After the mapping, we grouped these IPs into clusters. This new mapping revealed that over 2700 Irregular Patches form more than 100 clusters, often displaying characteristic patterns. Their geologic context suggests that these patterns are controlled by subsurface geologic structures and processes. This way even without penetrating radar, recognizing the clustered nature of IPs on the Moon enables us to infer details of the IP hosting regions' subsurface structures and infer subsurface processes that led to their formation.</div></div>","PeriodicalId":13199,"journal":{"name":"Icarus","volume":"429 ","pages":"Article 116439"},"PeriodicalIF":2.5000,"publicationDate":"2024-12-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Icarus","FirstCategoryId":"101","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0019103524004998","RegionNum":2,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ASTRONOMY & ASTROPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
The aim of this work was to systematically map cluster-forming Irregular Patches (IPs) on the Moon. These features, formerly termed “Irregular Mare Patches”, are enigmatic features situated on the near side of the Moon, mostly in mare regions. IPs are pristine-looking features with textures at the meter scale, suggesting they formed millions of years ago on top of several-billion-year-old mare basalts. Morphologic and spectral studies could not provide conclusive evidence of their formative processes, or their age. Theories on their formation concentrate around three conflicting models - that they are formed by compact basalts and are only a few tens of millions of years old; that they are formed by mass wasting processes capable to remove regolith to this day; or that they are composed of lava foams and their age is the same as the host terrain's, i.e. billions of years. We present a GIS-based analysis to examine which formation model is supported by their geography. Previous catalogs mapped IPs ambiguously, with one single coordinate representing one unit or a group of units, with many isolated units around them remaining unmapped. To change that, we mapped isolated IPs individually as polygons because we wanted to reveal their areas and their local-scale distribution patterns, which were not identifiable from previous mapping efforts. We named the isolated, elemental depressions Irregular Patches to differentiate them from previous works. After the mapping, we grouped these IPs into clusters. This new mapping revealed that over 2700 Irregular Patches form more than 100 clusters, often displaying characteristic patterns. Their geologic context suggests that these patterns are controlled by subsurface geologic structures and processes. This way even without penetrating radar, recognizing the clustered nature of IPs on the Moon enables us to infer details of the IP hosting regions' subsurface structures and infer subsurface processes that led to their formation.
期刊介绍:
Icarus is devoted to the publication of original contributions in the field of Solar System studies. Manuscripts reporting the results of new research - observational, experimental, or theoretical - concerning the astronomy, geology, meteorology, physics, chemistry, biology, and other scientific aspects of our Solar System or extrasolar systems are welcome. The journal generally does not publish papers devoted exclusively to the Sun, the Earth, celestial mechanics, meteoritics, or astrophysics. Icarus does not publish papers that provide "improved" versions of Bode''s law, or other numerical relations, without a sound physical basis. Icarus does not publish meeting announcements or general notices. Reviews, historical papers, and manuscripts describing spacecraft instrumentation may be considered, but only with prior approval of the editor. An entire issue of the journal is occasionally devoted to a single subject, usually arising from a conference on the same topic. The language of publication is English. American or British usage is accepted, but not a mixture of these.