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Allan Hills A78103 | |||||||||||||||||||||||||
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Basic information | Name: Allan Hills A78103 This is an OFFICIAL meteorite name. Abbreviation: ALHA78103 This meteorite may also be called Allan Hills 78103 (ALH 78103) in publications. Observed fall: No Year found: 1978 Country: Antarctica [Collected jointly by ANSMET (US) and NIPR (Japan)] Mass: ![]() | ||||||||||||||||||||||||
Classification history: |
This is 1 of 12331 approved meteorites (plus 8 unapproved names) classified as L6. [show all] Search for other: L chondrites, L chondrites (type 4-7), Ordinary chondrites, and Ordinary chondrites (type 4-7) | ||||||||||||||||||||||||
Writeup![]() |
Writeup from AMN 3(1):
This text was reprinted from AMN 3(1) in AMN 4(1). In some cases, it may be an updated version from the original. Sample No.: ALHA78103 Location: Allan Hills Field No.: 243 Weight (gms): 589.7 Meteorite Type: L6 Chondrite
Physical Description: The rounded specimen is approximately 11 x 7 x 4 cm.. The entire sample, with possible exception of a small patch of remnant fusion crust on the E surface, is weathered and stained by iron-oxidation. The B surface is the less severely weathered of all the surfaces, and several chondrules, 3-5 mm in diameter, are apparent. The matrix of the sample is greenish-gray. Several fractures are present on the T surface. The sample broke along at fracture during processing of the meteorite. Some oxidation halos, and some metallic flakes are visible in the greenish gray matrix of the sample, The sample appears to have a weathering rind, ~3 mm. in depth, along the T surface. The sample cannot be magnetically orientated.
Petrographic Description: Brian Mason Chondrules are sparse and have diffuse margins which tend to merge with the granular matrix, which consists of olivine and pyroxene with minor subequal amounts of nickel-iron and troilite, some plagioclase,- and accessory chromite. Minor limonitic staining is present around nickel-iron grains. Well-preserved fusion crust, 0.5 mm thick, is present along one edge. Microprobe analyses give the following compositions: olivine, Fa24; pyroxene, Fs20; plagioclase, An 10. The meteorite is an L6 chondrite. ALHA78103 is an L6 chondrite similar to ALHA78104 in all respects. | ||||||||||||||||||||||||
Data from: MB76 Table 2 Line 327: |
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Catalogs: |
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References: | Published in Antarctic Meteorite Newsletter 3(1) (1980), JSC, Houston Published in Meteoritical Bulletin, no. 76, Meteoritics 29, 100-143 (1994)
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Geography:![]() |
Statistics: This is 1 of 43856 approved meteorites from Antarctica (plus 3802 unapproved names) | ||||||||||||||||||||||||
Proximity search: |