Abstract
The Mairan domes are four features located in northern Oceanus Procellarum at ∼312.3E, 41.4N on the Moon. High resolution visible imagery, visible-to-mid-IR spectra, and Lunar Prospector Th abundance data all indicate that these four domes have a composition that is consistent with derivation from a Si-rich, highly evolved magma.
| Original language | English |
|---|---|
| Article number | L21204 |
| Journal | Geophysical Research Letters |
| Volume | 38 |
| Issue number | 21 |
| DOIs | |
| State | Published - Nov 1 2011 |