Nuussuaq spherule bed - Impact Deposit
Alternate Names | N/A |
Coordinates |
70° 34' 48" N; 53° 4' 48" W Notes
|
Country |
Greenland
Related Countries :
|
Region | Greenland |
Date Confirmed | 1991 Notes
|
Age (Ma) | 60.7 ±1.3 Notes :
Method :
|
Impactor Type |
Unknown
Notes
|
Advanced Data Fields
Notes

- This layer was originally thought to be of volcanic origin, however they have certain features which are characteristic of impact ejecta (immiscible melt textures, distinctive Ni-spinel, and high Ir, PGE and siderophile element anomalies) (Jones et al., 2005)
References
(1991) Possible impact ejecta in the Paleocene flood basalt province of West Greenland, Eos Trans. AGU 72, p. 278
(1992) Glass spheres, high iridium and flood basalts in West Greenland: A Paleocene impact site?, Geological Society of America 24, p. 333
(1996) Characteristics and origin of the glass spherules from the Paleocene flood basalt province of western Greenland, Geochimica et Cosmochimica Acta 60(5), p. 815-830, Elsevier Ltd, url, doi:10.1016/0016-7037(95)00433-5
(1998) 40Ar/39Ar geochronology of the West Greenland Tertiary volcanic province, Earth and Planetary Science Letters 160(3-4), p. 569-586, Elsevier, url, doi:10.1016/S0012-821X(98)00112-5
(2005) Are there signs of a large Paleocene impact, preserved around Disko Bay, West Greenland? Nuussuaq spherule beds origin by impact instead of volcanic eruption?, Large Meteorite Impacts III: Special Paper 384, T Kenkmann, F Hörz, A Deutsch (ed.), p. 281-298, Geological Society of America, url
(2012) Distal impact ejecta layers: Spherules and more, Elements 8(1), p. 43-48, GeoScienceWorld, pdf, doi:10.2113/gselements.8.1.43