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Boudenib 001 | |||||||||||||||||||||||||||||||||||||
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Basic information | Name: Boudenib 001 This is an OFFICIAL meteorite name. Abbreviation: There is no official abbreviation for this meteorite. Observed fall: No Year found: 2021 Country: Morocco Mass: ![]() | ||||||||||||||||||||||||||||||||||||
Classification history: |
This is 1 of 9 approved meteorites classified as Diogenite-melt breccia. [show all] Search for other: Achondrites, Diogenites, and HED achondrites | ||||||||||||||||||||||||||||||||||||
Comments: | Approved 1 Oct 2022 | ||||||||||||||||||||||||||||||||||||
Writeup![]() |
Writeup from MB 111:
Boudenib 001 31°50.583’N, 3°43.633’W Centre-South, Morocco Find: 2021 Classification: HED achondrite (Diogenite, melt breccia) History: Many stones were found and collected in the desert region close to Boudenib in 2021 by nomads. This material was later purchased by Nbark Boisofa. Physical characteristics: Multiple stones and fragments that are weathered; some of them are partly covered by a dark brown fusion crust. Petrography: (D. Sheikh, Cascadia) This sample is made up of two distinct lithologies; Lithology 1 (host) comprises ~85 vol. % of the analyzed thin section and represents a diogenite melt breccia composed of zoned, tabular low-Ca pyroxene grains (up to ~ 1 mm) set within a melt-textured matrix speckled with Fe-sulfides (primarily pentlandite) and containing accessory calcic plagioclase, olivine, kamacite, chromite, and merrillite. Lithology 2 comprises ~15 vol. % of the analyzed thin section (in the form of a few scattered clasts) and represents a mixed breccia composed of zoned, diogenitic tabular low-Ca pyroxene grains (up to ~1 mm, ~40 vol. %), reversely-zoned, eucritic tabular pigeonite grains (some displaying augite exsolution lamellae, up to ~1 mm, ~25 vol. %), and accessory chromite, merrillite, ilmenite, pentlandite, troilite, kamacite, olivine, and SiO2-rich glass, all of which is sub-ophitically enclosed within a matrix of skeletal and lath-shaped calcic plagioclase (~90 μm, ~35 vol. %). The sample is crosscut by multiple weathering veins containing Fe-hydroxides. Geochemistry: Lithology 1: Diogenite Low-Ca Pyroxene (Fs25.0±2.5Wo1.7±0.4, range Fs22.5-32.4Wo1.1-3.4, Fe/Mn=30±2, n=47), Olivine (Fa33.9±1.6, range Fa32.6-36.8, Fe/Mn=48±3, n=5), Calcic Plagioclase (An87.4±0.8, range An86.6-88.9, n=8); Lithology 2: Diogenite Low-Ca Pyroxene (Fs26.9±4.5Wo2.6±1.4, range Fs19.1-34.8Wo0.9-5.2, Fe/Mn=28±2, n=16), Eucrite Pigeonite (Fs35.8±3.8Wo10.0±4.8, range Fs28.7-41.7Wo5.5-24.2, Fe/Mn=24±2, n=19), Eucrite High-Ca Pyroxene (Fs28.9±9.3Wo31.7±8.9, range Fs22.3-35.5Wo25.4-38.0, Fe/Mn=23±2, n=2), Olivine (Fa48.9±0.2, range Fa48.8-49.1, Fe/Mn=46±1, n=2), Calcic Plagioclase (An87.9±0.6, range An87.3-89.9, n=16). Classification: HED achondrite (Diogenite-melt breccia) due to the fact that the entirety of the host lithology (Lithology 1, occupies ~85 vol. % of section) and ~40% of Lithology 2 (occupies ~15 vol. % of section) is texturally/compositionally representative of a diogenite-melt breccia. Specimens: 20.06 g at Cascadia, main mass with Nbark Boisofa. | ||||||||||||||||||||||||||||||||||||
Data from: MB111 Table 0 Line 0: |
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Institutions and collections |
Cascadia: Cascadia Meteorite Laboratory, Portland State University, Department of Geology, Room 17 Cramer Hall, 1721 SW Broadway, Portland, OR 97201, United States; Website (institutional address; updated 28 Oct 2011) |
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Catalogs: |
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References: | Published in Meteoritical Bulletin, no. 111, in preparation (2022)
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Photos: |
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Geography:![]() |
Statistics: This is 1 of 44 approved meteorites from Centre-South, Morocco (plus 1 unapproved name) (plus 1 impact crater) This is 1 of 2012 approved meteorites from Morocco (plus 35 unapproved names) (plus 1 impact crater) | ||||||||||||||||||||||||||||||||||||
Proximity search: |