Interior of the Moon: The presence of garnet in the primitive deep lunar mantle
CR Neal - Journal of Geophysical Research: Planets, 2001 - Wiley Online Library
New trace element data have been generated by inductively coupled plasma‐mass
spectrometry (ICP‐MS) for 65 high‐and low‐Ti mare basalts from the Apollo 11, 12, 14, 15 …
spectrometry (ICP‐MS) for 65 high‐and low‐Ti mare basalts from the Apollo 11, 12, 14, 15 …
Compressibility of molten high-Ti mare glass: Evidence for crystal-liquid density inversions in the lunar mantle
S Circone, CB Agee - Geochimica et Cosmochimica Acta, 1996 - Elsevier
Static compression density measurements of molten Apollo 14 black glass have been
performed at liquidus conditions in the pressure range 1.0–11.5 GPa. A range of values for …
performed at liquidus conditions in the pressure range 1.0–11.5 GPa. A range of values for …
Assimilation by lunar mare basalts: Melting of crustal material and dissolution of anorthite
AB Finnila, PC Hess… - Journal of Geophysical …, 1994 - Wiley Online Library
We discuss techniques for calculating the amount of crustal assimilation possible in lunar
magma chambers and dikes based on thermal energy balances, kinetic rates, and simple …
magma chambers and dikes based on thermal energy balances, kinetic rates, and simple …
The role of ilmenite in the source region for mare basalts: Evidence from niobium, zirconium, and cerium in picritic glasses
CK Shearer, JJ Papike, GD Layne - Geochimica et Cosmochimica Acta, 1996 - Elsevier
To investigate models for the generation of lunar high Ti-basalts, we have analyzed lunar
picritic glasses for Zr, Nb, Ce, and Ti at high precision using ion microprobe techniques. The …
picritic glasses for Zr, Nb, Ce, and Ti at high precision using ion microprobe techniques. The …