KREEPy lunar meteorite Dhofar 287A: A new lunar mare basalt

Anand, Mahesh; Taylor, Lawrence A.; Misra, Kula C.; Demidova, Svetlana I. and Nazarov, Mikhail A. (2003). KREEPy lunar meteorite Dhofar 287A: A new lunar mare basalt. Meteoritics and Planetary Science, 38(4) pp. 485–499.



Dhofar 287 (Dho 287) is a new lunar meteorite, found in Oman on January 14, 2001. The
main portion of this meteorite (Dho 287A) consists of a mare basalt, while a smaller portion of breccia
(Dho 287B) is attached on the side. Dho 287A is only the fourth crystalline mare basalt meteorite
found on Earth to date and is the subject of the present study. The basalt consists mainly of
phenocrysts of olivine and pyroxene set in a finer-grained matrix, which is composed of elongated
pyroxene and plagioclase crystals radiating from a common nucleii. The majority of olivine and
pyroxene grains are zoned, from core to rim, in terms of Fe and Mg. Accessory minerals include
ilmenite, chromite, ulvöspinel, troilite, and FeNi metal. Chromite is invariably mantled by ulvöspinel.
This rock is unusually rich in late-stage mesostasis, composed largely of fayalite, Si-K-Ba-rich glass,
fluorapatite, and whitlockite. In texture and mineralogy, Dho 287A is a low-Ti mare basalt, with
similarities to Apollo 12 (A-12) and Apollo 15 (A-15) basalts. However, all plagioclase is now
present as maskelynite, and its composition is atypical for known low-Ti mare basalts. The Fe to Mn
ratios of olivine and pyroxene, the presence of FeNi metal, and the bulk-rock oxygen isotopic ratios,
along with several other petrological features, are evidence for the lunar origin for this meteorite.
Whole-rock composition further confirms the similarity of Dho 287A with A-12 and A-15 samples
but requires possible KREEP assimilation to account for its rare-earth-element (REE) contents.
Cooling-rate estimates, based on Fo zonation in olivine, yield values of 0.2–0.8°C/hr for the lava,
typical for the center of a 10–20 m thick flow. The recalculated major-element concentrations, after
removing 10–15% modal olivine, are comparable to typical A-15 mare basalts. Crystallization modeling
of the recalculated Dho 287A bulk-composition yields a reasonable fit between predicted and
observed mineral abundances and compositions.

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