Mesosiderite

Class of stony–iron meteorites


title: "Mesosiderite" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public description: "Class of stony–iron meteorites" topic_path: "uncategorized" source: "https://en.wikipedia.org/wiki/Mesosiderite" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0

::summary Class of stony–iron meteorites ::

::data[format=table title="infobox meteorite subdivision"]

FieldValue
SubdivisionClass
NameMesosiderite
ImageVaca muerta mesosiderite.jpg
Image_captionVaca muerta mesosiderite.
TypeStony-iron
Subgroups{{flatlist
CompositionMeteoric iron (kamacite, taenite & tetrataenite); silicates (mostly pyroxene & Ca-rich plagioclase); sulphides (troilite)
Number_of_specimens208
Image2Chinguetti meteorite.jpg
Image2_captionChinguetti mesosiderite
::

|Subdivision = Class |Name = Mesosiderite |Alternative names = |Image = Vaca muerta mesosiderite.jpg |Image_caption = Vaca muerta mesosiderite. |Type = Stony-iron |Class = |Clan = |Subgroups = {{flatlist|

They are a rare type of meteorite; as of November 2014 only 208 are known (of which 56 come from Antarctica) and only 7 of these are observed falls. On the other hand, some mesosiderites are among the largest meteorites known.

At Vaca Muerta in the Atacama Desert in Chile, many fragments with a total mass of 3.8 tons were found in a large strewnfield. They were first discovered in the 19th century by ore prospectors who mistook the shiny metal inclusions for silver and thought they had found an outcrop of a silver ore deposit. Later when an analysis was made and nickel-iron was found, the true nature as a meteorite was established. The meteorite was called Vaca Muerta. The picture at right shows a cut and polished piece of Vaca Muerta.

The most recent fall of a mesosiderite occurred at Dong Ujimqin Qi in China, on September 7, 1995, where three large pieces with a total mass of 129 kg fell. The fall of the Estherville mesosiderite in Iowa, US occurred on May 10, 1879. After a brilliant fireball had been seen, a shower of several large masses and many small fragments fell, totaling 320 kg. The fall at Lowicz in Poland on March 12, 1935, yielded many (more than 50) fragments with a total weight of 59 kg. The other observed mesosiderite falls occurred in 1842 at Barea (Spain), in 1880 at Varamin (Iran), in 1933 at Dyarrl Island (Papua New Guinea), and at Patwar (India) in 1935. The legendary Chinguetti meteorite is also supposed to be a mesosiderite.

The asteroid 16 Psyche is a candidate for the parent body of the mesosiderites. However, a reliable delivery mechanism lacks for Psyche, and spectral analysis indicates the mesosiderites derive from the Maria Asteroid Family

References

References

  1. F. Heide, F. Wlotzka: Meteorites, Messengers from Space. Springer Verlag 1985.
  2. Karl K. Turekian. ''Meteorites, comets, and planets'', [https://books.google.com/books?id=kYtksEUxw0oC&dq=mesosiderite&pg=PA112 Page 112]
  3. H. Pedersen et al., Meteoritics 27 (1992) 126
  4. The Meteoritical Bulletin Database, http://www.lpi.usra.edu/meteor/metbull.php
  5. (1999). "The Missing Psyche Family: Collisionally Eroded or Never Formed?". Icarus.
  6. Fieber-Beyer, S. K., Gaffey, M. J., Kelley, M. S., Reddy, V., Reynolds, C. M., Hicks, T. (2011). The Maria Asteroid Family: Genetic Relationships and a Plausible Source of Mesosiderites near the 3:1 Kirkwood Gap Icarus 213, 524-537 https://doi.org/10.1016/j.icarus.2011.03.009

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