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Elephant Moraine 82613 | |||||||||||||||||||||
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Basic information | Name: Elephant Moraine 82613 This is an OFFICIAL meteorite name. Abbreviation: EET 82613 Observed fall: No Year found: 1982 Country: Antarctica [Collected by US Antarctic Search for Meteorites program (ANSMET)] Mass: 4.2 g | ||||||||||||||||||||
Classification history: |
This is 1 of 2062 approved meteorites (plus 5 unapproved names) classified as L4. [show all] Search for other: L chondrites, L chondrites (type 4-7), Ordinary chondrites, and Ordinary chondrites (type 4-7) | ||||||||||||||||||||
Writeup |
Writeup from AMN 7(2):
Sample No.: EET82613 Location: Elephant Moraine Field No.: 2977 Weight (gms): 4.2 Meteorite Type: L4 Chondrite
Physical Description: Carol Schwarz, This angular fragment is shaped like the corner of a larger piece. The interior is yellowish with some less weathered gray matrix visible. The fusion crust is black and dull and approximately 1 mm thick. Dimensions: 1.5 x 1.5 x 1.5 cm
Petrographic Description: Brian Mason Chondrules are abundant and well-developed, ranging up to 1.5 mm in diameter; a variety of types are present, the commonest being granular and porphyritic olivine and olivine-pyroxene (much of the pyroxene is polysynthetically twinned clinobronzite). The chondrules are set in a ground-mass consisting largely of fine-grained olivine and pyroxene, with minor amounts of coarser-grained nickel-iron and troilite. A moderate degree of weathering is indicated by brown limonitic staining concentrated around metal grains. Microprobe analyses give the following compositions: olivine, Fa24; pyroxene, Fs20. The meteorite is an L4 chondrite. | ||||||||||||||||||||
Data from: MB76 Table 2 Line 1461: |
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Catalogs: |
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References: | Published in Antarctic Meteorite Newsletter 7(2) (1984), 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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