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Yamato 74037 meteorite, Queen Fabiola Mts, Queen Maud Land, Eastern Antarctica, Antarcticai
Regional Level Types
Yamato 74037 meteoriteMeteorite Fall Location
Queen Fabiola MtsMountain Range
Queen Maud LandRegion
Eastern AntarcticaRegion
AntarcticaContinent

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Latitude & Longitude (WGS84):
71° 30' South , 35° 40' East
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Other/historical names associated with this locality:
Y-74037


Official name: Yamato 74037
Synonym: Y-74037
Observed fall: no
Found: 1974
Coordinates: 71°30'S, 35°40'E (Catalogue of Meteorites)
Approx. recovered weight: 592 g
Diogenite


Yamato 74037, as well as Y-74013 and Y-6902 meteorites, is a diogenite with granoblastic texture and composed almost entirely of equigranualr grains of orthopyroxene. Many other fragments with almost the same appearance were also collected in the same area. However, diogenite is comparatively rare type among meteorites and especially the granoblastic texture is thought to be rather unique in contrast with brecciated structure of usual diogenites. It seems to be very probable that each of these diogenites were once located at the different positions in the identical parent body. The distance from the surface of the preatmospheric mass were studied by means of cosmic-ray particle tracks (Yabuki, 1978). The tracks recorded in bronzite in diogenites are expected to be mostly due to cosmic-ray heavy primaries, because of their extremely low uranium contents. Assuming that the cosmic-ray exposure age, 31 Myr, of Yamato 6902 is also applicable to other diogenites, the distance from the preatmospheric surface to the test crystals is estimated to be 17 cm for Yamato 74037.

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Standard Detailed Gallery Strunz Chemical Elements

Mineral List


1 valid mineral.

Meteorite/Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

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Alphabetical List Tree Diagram

Detailed Mineral List:

Enstatite
Formula: Mg2Si2O6
Reference: Yabuki, H. (1978) Charged-particle tracks in Yamato-74 meteorites. Journal of the Faculty of Science, Hokkaido University, Series 4, Geology and mineralogy, 18, 1-2 (February 1978), 85-104.
Enstatite var. Bronzite
Formula: (Mg,Fe2+)2[SiO3]2
Reference: Yabuki, H. (1978) Charged-particle tracks in Yamato-74 meteorites. Journal of the Faculty of Science, Hokkaido University, Series 4, Geology and mineralogy, 18, 1-2 (February 1978), 85-104.
'Fayalite-Forsterite Series'
Reference: Yabuki, H. (1978) Charged-particle tracks in Yamato-74 meteorites. Journal of the Faculty of Science, Hokkaido University, Series 4, Geology and mineralogy, 18, 1-2 (February 1978), 85-104.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 9 - Silicates
Enstatite9.DA.05Mg2Si2O6
var. Bronzite9.DA.05(Mg,Fe2+)2[SiO3]2
Unclassified Minerals, Rocks, etc.
'Fayalite-Forsterite Series'-

List of minerals for each chemical element

OOxygen
O Enstatite var. Bronzite(Mg,Fe2+)2[SiO3]2
O EnstatiteMg2Si2O6
MgMagnesium
Mg Enstatite var. Bronzite(Mg,Fe2+)2[SiO3]2
Mg EnstatiteMg2Si2O6
SiSilicon
Si Enstatite var. Bronzite(Mg,Fe2+)2[SiO3]2
Si EnstatiteMg2Si2O6
FeIron
Fe Enstatite var. Bronzite(Mg,Fe2+)2[SiO3]2

References

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Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Yabuki, H. (1978) Charged-particle tracks in Yamato-74 meteorites. Journal of the Faculty of Science, Hokkaido University, Series 4, Geology and mineralogy, 18, 1-2 (February 1978), 85-104.

External Links


Other Regions, Features and Areas containing this locality

Antarctic MeteoritesGroup of Meteorite Fall Locations
Antarctic PlateTectonic Plate

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