Petrologic Characteristics of the Lunar Surface

Petrologic analysis of the lunar surface is critical for determining lunar formation and evolution. Here, we report the first global petrologic map that includes the five most important lunar lithological units: the Ferroan Anorthositic (FAN) Unit, the Magnesian Suite (MS) Unit, the Alkali Suite (AS...

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Published in:Scientific Reports
Main Authors: Wang, Xianmin, Pedrycz, Witold
Format: Text
Language:English
Published: Nature Publishing Group 2015
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4661461/
http://www.ncbi.nlm.nih.gov/pubmed/26611148
https://doi.org/10.1038/srep17075
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spelling ftpubmed:oai:pubmedcentral.nih.gov:4661461 2023-05-15T18:22:42+02:00 Petrologic Characteristics of the Lunar Surface Wang, Xianmin Pedrycz, Witold 2015-11-27 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4661461/ http://www.ncbi.nlm.nih.gov/pubmed/26611148 https://doi.org/10.1038/srep17075 en eng Nature Publishing Group http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4661461/ http://www.ncbi.nlm.nih.gov/pubmed/26611148 http://dx.doi.org/10.1038/srep17075 Copyright © 2015, Macmillan Publishers Limited http://creativecommons.org/licenses/by/4.0/ This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ CC-BY Article Text 2015 ftpubmed https://doi.org/10.1038/srep17075 2015-12-06T01:49:47Z Petrologic analysis of the lunar surface is critical for determining lunar formation and evolution. Here, we report the first global petrologic map that includes the five most important lunar lithological units: the Ferroan Anorthositic (FAN) Unit, the Magnesian Suite (MS) Unit, the Alkali Suite (AS) Unit, the KREEP Basalt (KB) Unit and the Mare Basalt (MB) Unit. Based on the petrologic map and focusing on four long-debated and important issues related to lunar formation and evolution, we draw the following conclusions from the new insights into the global distribution of the five petrologic units: (1) there may be no petrogenetic relationship between MS rocks and KB; (2) there may be no petrogenetic link between MS and AS rocks; (3) the exposure of the KREEP component on the lunar surface is likely not a result of MB volcanism but is instead mainly associated with the combined action of plutonic intrusion, KREEP volcanism and celestial collision; (4) the impact size of the South Pole-Aitken basin is constrained, i.e., the basin has been excavated through the whole crust to exhume a vast majority of lower-crustal material and a very limited mantle components to the lunar surface. Text South pole PubMed Central (PMC) Aitken ENVELOPE(-44.516,-44.516,-60.733,-60.733) South Pole Scientific Reports 5 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Wang, Xianmin
Pedrycz, Witold
Petrologic Characteristics of the Lunar Surface
topic_facet Article
description Petrologic analysis of the lunar surface is critical for determining lunar formation and evolution. Here, we report the first global petrologic map that includes the five most important lunar lithological units: the Ferroan Anorthositic (FAN) Unit, the Magnesian Suite (MS) Unit, the Alkali Suite (AS) Unit, the KREEP Basalt (KB) Unit and the Mare Basalt (MB) Unit. Based on the petrologic map and focusing on four long-debated and important issues related to lunar formation and evolution, we draw the following conclusions from the new insights into the global distribution of the five petrologic units: (1) there may be no petrogenetic relationship between MS rocks and KB; (2) there may be no petrogenetic link between MS and AS rocks; (3) the exposure of the KREEP component on the lunar surface is likely not a result of MB volcanism but is instead mainly associated with the combined action of plutonic intrusion, KREEP volcanism and celestial collision; (4) the impact size of the South Pole-Aitken basin is constrained, i.e., the basin has been excavated through the whole crust to exhume a vast majority of lower-crustal material and a very limited mantle components to the lunar surface.
format Text
author Wang, Xianmin
Pedrycz, Witold
author_facet Wang, Xianmin
Pedrycz, Witold
author_sort Wang, Xianmin
title Petrologic Characteristics of the Lunar Surface
title_short Petrologic Characteristics of the Lunar Surface
title_full Petrologic Characteristics of the Lunar Surface
title_fullStr Petrologic Characteristics of the Lunar Surface
title_full_unstemmed Petrologic Characteristics of the Lunar Surface
title_sort petrologic characteristics of the lunar surface
publisher Nature Publishing Group
publishDate 2015
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4661461/
http://www.ncbi.nlm.nih.gov/pubmed/26611148
https://doi.org/10.1038/srep17075
long_lat ENVELOPE(-44.516,-44.516,-60.733,-60.733)
geographic Aitken
South Pole
geographic_facet Aitken
South Pole
genre South pole
genre_facet South pole
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4661461/
http://www.ncbi.nlm.nih.gov/pubmed/26611148
http://dx.doi.org/10.1038/srep17075
op_rights Copyright © 2015, Macmillan Publishers Limited
http://creativecommons.org/licenses/by/4.0/
This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.1038/srep17075
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