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Mairan

Lunar Orbiter 4 image
Coordinates	41°36′N 43°24′W / 41.6°N 43.4°W / 41.6; -43.4
Diameter	40 km
Depth	3.4 km
Colongitude	44° at sunrise
Eponym	Jean J. d'Ortous de Mairan

Mairan is a lunar impact crater that is located on a highland peninsula between Oceanus Procellarum to the west and Mare Imbrium to the east. To the north-northeast is the comparably sized crater Sharp. Northwest of Mairan is the heavily eroded Louville.

The outer rim of Mairan has not been significantly eroded or impacted, and retains a sharp edge. The surface around Mairan is rough and irregular, with a multitude of many tiny craters, particularly to the south and west. The inner walls display some terracing, and flow down to a relatively flat interior floor.

Mairan is a crater of Upper (Late) Imbrian age.

Mairan domes

The volcanic complex, known as Mairan Hills or Mairan Domes, is composed of Mairan T together with three satellite domes (Mairan Northwest, Mairan Middle, and Mairan South). It was formed by two volcanic episodes 3.75±0.1 and 3.35±0.2 billion years ago, extruding a viscous silicic lava simultaneously with basalt eruptions in nearby mare. Most of volcanic complex, except for dome summits, is now buried under mare surface.

In the mare, due west of Mairan, is a small lunar dome designated Mairan T with 3.8 km wide depression at the summit (in official IAU nomenclature "Mairan T" name refers only to the depression), believed to be a caldera The width of hill is about 7 km, and height is about 800 m. It is one of four unusually steep (with slopes reaching 22-27 degrees) and bright domes in area which are thought to be formed by very viscous, high-Si lava.

The composition of domes is changing from the north to south, with Mairan Northwest composed of pyroxenes with 30% quartz admixture, while Mairan South dome composed of nearly pure quartz, with extremely high thorium concentration of 83±19 ppm.

Rima Mairan

There is a sinuous rille along the southwest edge of the highland peninsula containing Mairan. It is designated Rima Mairan, and follows a north–south course for a length of about 100 kilometers.

Satellite craters

By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Mairan.

• Lunar dome Mairan T
• Mairan T from Apollo 15

References

1. The geologic history of the Moon. USGS Professional Paper 1348. By Don E. Wilhelms, John F. McCauley, and Newell J. Trask. U.S. Government Printing Office, Washington: 1987. Table 11.2.
2. Geology of Mairan middle dome: Its implication to silicic volcanism on the Moon
3. "Mairan". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
4. Tran, T.; Robinson, M. S.; Lawrence, S. J.; Braden, S. E.; Plescia, J.; Hawke, B. R.; et al. (March 2011). "Morphometry of Lunar Volcanic Domes from LROC" (PDF). 42nd Lunar and Planetary Science Conference, Held March 7–11, 2011 at the Woodlands, Texas. LPI Contribution (1608 p.2228): 2228. Bibcode:2011LPI....42.2228T.
5. Lena R.; Wöhler C.; Phillips J.; Chiocchetta M. T. (2013). Lunar Domes: Properties and Formation Processes. Springer Science & Business Media. pp. vii, 5–13, 35, 42. Bibcode:2013ldpf.book.....L. doi:10.1007/978-88-470-2637-7. ISBN 9788847026377.
6. The Mairan domes: Silicic volcanic constructs on the Moon

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• LQ04 quadrangle
• Impact craters on the Moon