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The distribution and purity of anorthosite across the Orientale basin: New perspectives from Moon Mineralogy Mapper data

Abstract:

The Orientale basin is a multiring impact structure on the western limb of the Moon that provides a clear view of the primary lunar crust exposed during basin formation. Previously, near‐infrared reflectance spectra suggested that Orientale's Inner Rook Ring (IRR) is very poor in mafic minerals and may represent anorthosite excavated from the Moon's upper crust. However, detailed assessment of the mineralogy of these anorthosites was prohibited because the available spectroscopic data sets did not identify the diagnostic plagioclase absorption feature near 1250 nm. Recently, however, this absorption has been identified in several spectroscopic data sets, including the Moon Mineralogy Mapper (M3), enabling the unique identification of a plagioclase‐dominated lithology at Orientale for the first time. Here we present the first in‐depth characterization of the Orientale anorthosites based on direct measurement of their plagioclase component. In addition, detailed geologic context of the exposures is discussed based on analysis of Lunar Reconnaissance Orbiter Narrow Angle Camera images for selected anorthosite identifications. The results confirm that anorthosite is overwhelmingly concentrated in the IRR. Comparison with nonlinear spectral mixing models suggests that the anorthosite is exceedingly pure, containing >95 vol % plagioclase in most areas and commonly ~99–100 vol %. These new data place important constraints on magma ocean crystallization scenarios, which must produce a zone of highly pure anorthosite spanning the entire lateral extent of the 430 km diameter IRR.

Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1002/jgre.20126

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Oxford college:
Exeter College
Role:
Author


Publisher:
American Geophysical Union
Journal:
Journal of Geophysical Research: Planets More from this journal
Volume:
118
Issue:
9
Pages:
1805-1820
Publication date:
2013-08-16
Acceptance date:
2013-08-11
DOI:
ISSN:
2169-9097


Keywords:
Pubs id:
pubs:431433
UUID:
uuid:04dc8496-e116-466d-87ac-ebeccfa2df2d
Local pid:
pubs:431433
Source identifiers:
431433
Deposit date:
2018-04-04

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