Global silicate mineralogy of the Moon from the Diviner lunar radiometer.

We obtained direct global measurements of the lunar surface using multispectral thermal emission mapping with the Lunar Reconnaissance Orbiter Diviner Lunar Radiometer Experiment. Most lunar terrains have spectral signatures that are consistent with known lunar anorthosite and basalt compositions. H...

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Main Authors: Greenhagen, B, Lucey, P, Wyatt, M, Glotch, T, Allen, C, Arnold, J, Bandfield, J, Bowles, N, Donaldson Hanna, K, Hayne, P, Song, E, Thomas, I, Paige, D
Format: Journal article
Language:English
Published: 2010
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author Greenhagen, B
Lucey, P
Wyatt, M
Glotch, T
Allen, C
Arnold, J
Bandfield, J
Bowles, N
Donaldson Hanna, K
Hayne, P
Song, E
Thomas, I
Paige, D
author_facet Greenhagen, B
Lucey, P
Wyatt, M
Glotch, T
Allen, C
Arnold, J
Bandfield, J
Bowles, N
Donaldson Hanna, K
Hayne, P
Song, E
Thomas, I
Paige, D
author_sort Greenhagen, B
collection OXFORD
description We obtained direct global measurements of the lunar surface using multispectral thermal emission mapping with the Lunar Reconnaissance Orbiter Diviner Lunar Radiometer Experiment. Most lunar terrains have spectral signatures that are consistent with known lunar anorthosite and basalt compositions. However, the data have also revealed the presence of highly evolved, silica-rich lunar soils in kilometer-scale and larger exposures, expanded the compositional range of the anorthosites that dominate the lunar crust, and shown that pristine lunar mantle is not exposed at the lunar surface at the kilometer scale. Together, these observations provide compelling evidence that the Moon is a complex body that has experienced a diverse set of igneous processes.
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spelling oxford-uuid:979c8b30-c807-42af-8cbf-b4403cc9832e2022-03-27T00:01:11ZGlobal silicate mineralogy of the Moon from the Diviner lunar radiometer.Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:979c8b30-c807-42af-8cbf-b4403cc9832eEnglishSymplectic Elements at Oxford2010Greenhagen, BLucey, PWyatt, MGlotch, TAllen, CArnold, JBandfield, JBowles, NDonaldson Hanna, KHayne, PSong, EThomas, IPaige, DWe obtained direct global measurements of the lunar surface using multispectral thermal emission mapping with the Lunar Reconnaissance Orbiter Diviner Lunar Radiometer Experiment. Most lunar terrains have spectral signatures that are consistent with known lunar anorthosite and basalt compositions. However, the data have also revealed the presence of highly evolved, silica-rich lunar soils in kilometer-scale and larger exposures, expanded the compositional range of the anorthosites that dominate the lunar crust, and shown that pristine lunar mantle is not exposed at the lunar surface at the kilometer scale. Together, these observations provide compelling evidence that the Moon is a complex body that has experienced a diverse set of igneous processes.
spellingShingle Greenhagen, B
Lucey, P
Wyatt, M
Glotch, T
Allen, C
Arnold, J
Bandfield, J
Bowles, N
Donaldson Hanna, K
Hayne, P
Song, E
Thomas, I
Paige, D
Global silicate mineralogy of the Moon from the Diviner lunar radiometer.
title Global silicate mineralogy of the Moon from the Diviner lunar radiometer.
title_full Global silicate mineralogy of the Moon from the Diviner lunar radiometer.
title_fullStr Global silicate mineralogy of the Moon from the Diviner lunar radiometer.
title_full_unstemmed Global silicate mineralogy of the Moon from the Diviner lunar radiometer.
title_short Global silicate mineralogy of the Moon from the Diviner lunar radiometer.
title_sort global silicate mineralogy of the moon from the diviner lunar radiometer
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