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Hallingeberg meteorite, Västervik, Småland, Sweden

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Latitude & Longitude (WGS84): 57° 49' 0'' North , 16° 13' 59'' East
Latitude & Longitude (decimal): 57.8166666667, 16.2333333333
Erratic type:Meteorite
Name(s) in local language(s):, Sverige

Ordinary chondrite, unequilibrated (L3.4; S3)
Fall, 1 February 1944; 1456 g

During the afternoon a single stone fell 25 km from Västervik and several fragments were recovered. Average Olivine composition (Fa25) is characteristic of L (low bulk Iron) chondrites, but marked variability of both olivine (Fa0-30) and pyroxene as well as milder Ni-variability in kamacite mark Hallingeberg more specifically as an unequilibrated L-chondrite (L3.4). Distinct chondrules of markedly variabilities and textures are present.

As of early September 2015, 44 meteorites had been classified as 'Unequilibrated Ordinary Chondrites' (UOC) at the Meteoritical Society's Meteoritical Bulletin Database. Of these. 12 meteorites belonged to the L group of ordinary chondrites, but Hallingeberg is the only UOC specifically classified as an L3.4 UOC.

Most of the mass (>1 kg, including the large 685 g fragment) has been held at Lund University.

Mineral List


7 valid minerals.

The above list contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

Mason, B. H. (1963) Olivine composition in chondrites. Geochimica et Cosmochimica Acta 27, 1011-1023.

Fuchs, L.H. (1968) X-ray crystallographic evidence for the meteoritic occurrence of nepheline. Earth and Planetary Science Letters 5: 187-190.

Dodd, R.T. (June 1974) The petrology of chondrules in the Hallingeberg meteorite: Contributions to Mineralogy and Petrology 47 (2): 97-112 (June 1974).

Gooding, J. L., Keil, K., Fukuoka, T., & Schmitt, R. A. (1979) The Metal Components of Chondrules: Meteoritics 14:404-406.

Lux, G., Keil, K. & Taylor, G. J.(1981) Chondrules in H3 chondrites - Textures, compositions and origins: Geochimica et Cosmochimica Acta 45: 675-685. (1981)

Gooding, J. L. & Keil, K. (1981) Relative abundances of chondrule primary textural types in ordinary chondrites and their bearing on conditions of chondrule formation: Meteoritics 16 :17-43. (Mar 1981)

Graham, A. L., Bevan, A. W. R. & Hutchison, B. (1985) Catalogue of Meteorites (4/e). University of Arizona Press: Tucson.

Brearley, A.J. & Jones, R.H. (1998) Chondritic Meteorites. In: Planetary Materials (Papike, JJ - Ed.), Chapter 3: 1-398: Mineralogical Society of America, Washington, DC, USA.

Grady, M.M. (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.

Menzies, O.N., Bland, P.B, Berry F.J. & Cressy, G. (2005) A Mössbauer spectroscopy and X-ray diffraction study of ordinary chondrites: Quantification of modal mineralogy and implications for redox conditions during metamorphism. Meteoritics & Planetary Science 40 (7): 1023-1042. (July 2005).

Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages.

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