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Pre-Nectarian

From Wikipedia, the free encyclopedia
Geologic period, 4533 to 3920 million years ago
Pre-Nectarian
4533 – 3920Ma
Chronology
−4500 —
−4000 —
−3500 —
−3000 —
−2500 —
−2000 —
−1500 —
−1000 —
−500 —
0 —
 
 
 
Periods on the Lunar Geologic Timescale. Axis scale: Millions of years ago.
Usage information
Celestial bodyEarth's Moon
Time scale(s) usedLunar Geologic Timescale
Definition
Chronological unitPeriod

Thepre-Nectarian period of thelunar geologic timescale runs from 4.533 billion years ago (the time of the initial formation of theMoon) to 3.920 billion years ago, when theNectaris Basin was formed by a large impact. It is followed by theNectarian period.

Description

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Pre-Nectarian rocks are rare in the lunar sample suite; they are mostly composed of lunar highlands material which have been heavily churned, brecciated, and thermally affected by subsequent impacts, particularly during the Heavy Bombardment Eon[1][2] (HBE; a period of 0.6-1 Gy from the formation of the Moon until at least the formation of the Imbrium Basin ~3.9 Ga, or even later with the formation of Orientale Basin) that marks the approximate beginning of theNectarian period. The primary pre-Nectarian lunar highland material is dominated by the rock typeanorthosite, which suggests that the early stage of lunar crustal formation occurred via mineral crystallization of a globalmagma ocean.

This geologic period has been informally subdivided into theCryptic Era (4.533 - 4.172 Ga ago) and Basin Groups 1-9 (4.172 - 3.92 Ga ago),[3] but these divisions are not used on any geologic maps. Similarly the later period has also been called theAitkenian period.

Millions of years before present


Impact basins

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Lunar impact basins
as categorized by Wilhelmset al. (1987)[4]
Basin nameDiameterAge-
group
(km)(nr.)
Procellarum3,2001
South Pole-Aitken2,500
Tsiolkovskiy-Stark7002
Grissom-White600
Insularum600
Marginis580
Flamsteed-Billy570
Balmer-Kapteyn550
Werner-Airy500
Pingré-Hausen300
Al-Khwarizmi /King590
Fecunditatis9903
Australe880
Tranquillitatis800
Mutus-Vlacq700
Nubium690
Lomonosov-Fleming620
Basin nameDiameterAge-
group
(km)(nr.)
Ingenii6504
Poincaré340
Keeler-Heaviside780
Coulomb-Sarton5305
Smythii840
Lorentz3606
Amundsen-Ganswindt3557
Schiller-Zucchius325
Planck325
Birkhoff330
Freundlich-Sharonov6008
Grimaldi4309
Apollo505
For basins with no article, the two prominent
craters' names are separately linked to their
respective articles.
Names of proposed basins areitalicized.
 

Relationship to Earth's geologic time scale

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Since little or nogeological evidence onEarth exists from the time spanned by the pre-Nectarian period of the Moon, the pre-Nectarian has been used as a guide by at least one notable scientific work[5] to subdivide the unofficial terrestrialHadeaneon. In particular, theHadean eon is subdivided into theCryptic era,Basin Groups 1-9,Nectarian andLower Imbrian, though the first two of these lunar divisions are informal and collectively make up the pre-Nectarian.

See also

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References

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  1. ^Fernandes V. A., Fritz J., Weiss B., Garrick-Bethel and Shuster D. (2013) The bombardment history of the Moon as recorded by 40Ar-39Ar chronology. Meteor. and Planet. Sci. 48, 241–269. DOI: 10.1111/maps.12054.
  2. ^Fritz J., Bitsch B., Kührt E., Morbidelli A., Tornow C., Wünnemann K., Fernandes V.A., Grenfell L.J., Rauer H., Wagner R. andWerner S.C. (2014) Earth-like habitats in planetary systems. Planetary and Space Science 98, 254–267.https://dx.doi.org/ 10.1016/j.pss.2014.03.003i
  3. ^Don Wilhelms (1987).Geologic History of the Moon. U.S. Geological Survey Professional Paper 1348.
  4. ^Wilhelms, Don; McCauley, John; Trask, Newell (1987).The geologic history of the Moon. Professional Paper.US Geological Survey. p. 148.doi:10.3133/pp1348.
  5. ^W. Harland; R. Armstrong; A. Cox; L. Craig; A. Smith; D. Smith (1990).A Geologic time scale 1989. Cambridge University Press.

External links

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