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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Moscoviense Basin
3D gravity inversion based on mixed-norm regularization in spherical coordinates with application to the lunar Moscoviense Basin Available to Purchase
(a) Free-air and (b) Bouguer gravity anomalies of the Moscoviense Basin. Al... Available to Purchase
Topography map of the Moscoviense Basin. Its location is represented as a w... Available to Purchase
Spinel-rich lithologies in the lunar highland crust: Linking lunar samples with crystallization experiments and remote sensing Available to Purchase
Reflectance spectra of the AT-65785 experimental run products (1500 to 1150... Available to Purchase
Example M 3 spectra for three of the rock types exposed along the inner ri... Available to Purchase
Distribution of Mg-spinel across the Moon displayed with oversized symbols.... Available to Purchase
The distribution of Mg-spinel across the Moon and constraints on crustal origin Available to Purchase
Lunar mare volcanism: lateral heterogeneities in volcanic activity and relationship with crustal structure Available to Purchase
Abstract Lunar mare basalts are spatially unevenly distributed, and their abundances differ between the nearside and farside of the Moon. Although mare asymmetry has been attributed to thickness variations in the low-density anorthositic crust, the eruptive mechanism of lunar magma remains unknown. In this study, we investigate the relationship between mare distribution and crustal thickness using geological and geophysical data obtained by the SELENE (Kaguya) and the Gravity Recovery and Interior Laboratory spacecraft, and quantitatively re-evaluate the influence of the anorthositic crust on magma eruption. We identify a lateral heterogeneity in the upper limit of crustal thickness that allows magma extrusion to the surface. In the Procellarum KREEP Terrane, where the surface abundances of heat-producing elements are extremely high, magmas can erupt in regions of crustal thickness below about 30 km. In contrast, magma eruptions are limited to regions of crustal thickness below about 20 km in other nearside regions, around 10 km in the South Pole–Aitken Basin and approximately 5 km in the farside Felspathic Highland Terrane. Such heterogeneity may result from lateral variations in magma production in the lunar mantle and/or crustal density.