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Allan Hills A78038 | |||||||||||||||||||||||||||||
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Basic information | Name: Allan Hills A78038 This is an OFFICIAL meteorite name. Abbreviation: ALHA78038 This meteorite may also be called Allan Hills 78038 (ALH 78038) 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 51 approved meteorites classified as L3.4. [show all] Search for other: L chondrites, L chondrites (type 3), Ordinary chondrites, and Ordinary chondrites (type 3) | ||||||||||||||||||||||||||||
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.: ALHA78038 Location: Allan Hills Field No.: 278 weight (gms): 363.0 Meteorite Type: LL3 Chondrite
Physical Description: This angular sample is approximately 12 x 5 x 5 cm. and appears shiny and reddish-brown due to weathering and staining by iron oxidation. Several fractures penetrate deeply into the sample. One small remnant patch of shiny black fusion crust remains on the B surface. During processing the sample fell apart and revealed no unoxidized material.
Petrographic Description: Brian Mason The section shows a close-packed aggregate of chondrules, 0.3 - 2.7 mm in diameter, and a few angular enclaves (some are chondrule fragments) in a minor amount of dark fine-grained matrix. A wide variety of chondrules are present, the commonest being granular olivine and olivine-pyroxene, porphyritic olivine, and fine-grained pyroxene, Most of the pyroxene is polysynthetically twinned. Many of the chondrules have dark rims. Troilite is present in minor amounts in the matrix. Weathering is extensive, the section being rimmed and veined with brown limonite, and little nickel-iron remains. Microprobe analyses show olivine ranging from Fa4 to Fa9, with a mean of Fa22; pyroxene ranges from Fs2 to Fs19 , with a mean of Fs8 and CaO ranging from 0.1 to 1.3 weight percent. The low content of nickel-iron and troilite suggests LL group, and the meteorite is tentatively classified as an LL3 chondrite. | ||||||||||||||||||||||||||||
Data from: MB76 Table 2 Line 281: |
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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 43840 approved meteorites from Antarctica (plus 3802 unapproved names) | ||||||||||||||||||||||||||||
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