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Allan Hills A78126 | |||||||||||||||||||||||||
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Basic information | Name: Allan Hills A78126 This is an OFFICIAL meteorite name. Abbreviation: ALHA78126 This meteorite may also be called Allan Hills 78126 (ALH 78126) in publications. Observed fall: No Year found: 1978 Country: Antarctica [Collected jointly by ANSMET (US) and NIPR (Japan)] Mass: 607 g | ||||||||||||||||||||||||
Classification history: |
This is 1 of 12780 approved meteorites (plus 11 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(2):
This text was reprinted from AMN 3(2) in AMN 4(1). In some cases, it may be an updated version from the original. Sample No.: ALHA78126 Location: Allan Hills Field No.: 383 Weight (gms): 606.9 Meteorite Type: L6 Chondrite
Physical Description: The NE corner of this sample (~12 x 8 x 5 cm) has been removed. A thin, ~1 mm, black fusion crust that is polygonally fractured in the B surface, and is weathering to a brown in some areas, covers the remainder of the specimen. Some areas of the fusion crust have weathered away, revealing a partially weathered, yellowish-gray matrix material. Some metallic looking particles are apparent on the broken surface. A deep fracture extends along the T and S faces. During processing of the sample, it became apparent that weathering penetrated the sample as much as 0.5 cm. below the fusion crust. The matrix material exposed during processing is greenish-gray, with several veins of what appears to be darker matrix material penetrating it. Small metallic locking particles were also apparent in this friable sample.
Petrographic Description: Brian Mason Chondrules are sparse and poorly defined, their borders tending to merge with the granular groundmass, which consists largely of olivine and pyroxene with minor subequal amounts of nickel-iron and troilite, plagioclase, and accessory chromite. A moderate amount of brown limonitic staining is present around the nickel-iron grains. Microprobe analyses give the following compositions: olivine, Fa25; pyroxene, Fs21; plagioclase, An10. The meteorite is an L6 chondrite. ALHA78130, 78131 are L6 chondrites similar in all respects to ALHA78126. | ||||||||||||||||||||||||
Data from: MB76 Table 2 Line 349: |
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Catalogs: |
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References: | Published in Antarctic Meteorite Newsletter 3(2) (1980), JSC, Houston Published in Meteoritical Bulletin, no. 76, Meteoritics 29, 100-143 (1994)
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Geography: |
Statistics: This is 1 of 44547 approved meteorites from Antarctica (plus 3802 unapproved names) | ||||||||||||||||||||||||
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Revision history: |
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