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Tin-Essako 001 | |||||||||||||||||||||||||||||||||
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Basic information | Name: Tin-Essako 001 This is an OFFICIAL meteorite name. Abbreviation: TE 001 Observed fall: No Year found: 2021 Country: Mali Mass: 4.3 kg | ||||||||||||||||||||||||||||||||
Classification history: |
This is 1 of 160 approved meteorites classified as Achondrite-ung. [show all] Search for other: Achondrites, Ungrouped achondrites | ||||||||||||||||||||||||||||||||
Comments: | Approved 4 Dec 2021 | ||||||||||||||||||||||||||||||||
Writeup |
Writeup from MB 110:
Tin-Essako 001 (TE 001) 18.280242, 2.094914 Gao, Mali Find: 2020 Classification: Ungrouped achondrite History: Purchased by Jay Piatek in 2021 from meteorite dealers Hassan Ounir and Ali Benamar. Found in 2020 by a nomad in Mali approximately 120 km east of the town of Kidal. Physical characteristics: Oriented single stone, irregular surface, dark colored exterior patina with some reddish-brown oxidation patches. Saw cuts reveal a stony-iron appearing interior with a heterogenous distribution of metal and silicate grains and domains. Cut metal surfaces appear fresh with only minor oxidation. Silicates are very dark brown in color. Petrography: (C. Agee, M. Spilde, UNM) This meteorite consists of approximately 50% silicates and 50% metal. The dominant silicate mineral is olivine; metal consists of kamacite. Backscatter electron imaging gives the approximate modal silicate abundances: 85-90% olivine, 10% plagioclase, and minor chromite, and quench melt pockets. Small (<100 μm) carbon rich phases (possibly graphite) at olivine-metal grain boundaries and as inclusions in metal were found. No pyroxenes, sulfides, or diamonds were detected in the microprobe mount. Geochemistry: (C. Agee, M. Spilde, UNM) Olivine Fa25.0±0.1, Fe/Mn=51±2, Cr2O3=0.27±0.02 wt%, CaO=0.24±0.01 wt%, n=8; plagioclase An54.0±1.5Or0.2±0.1Ab45.8±1.5, n=7; melt pocket SiO2=76.0±5.5, Al2O3=16.2±3.6, CaO=2.2±0.2, FeO=1.0±0.1, Na2O=5.1±1.3, all wt%, n=2; kamacite Fe=93.2±1.1, Ni=4.9±0.2, Co=0.46±0.02 (wt%), n=5. Oxygen isotopes (K. Ziegler, UNM): 3 acid-washed fragments analyzed by laser fluorination gave δ18O= 7.374, 8.164, 9.305; δ17O= 3.203, 3.663, 4.288; Δ17O= -0.690, -0.647, -0.625 (linearized, all per mil, TFL slope=0.528). Classification: Ungrouped achondrite, metal-rich. The oxygen isotope values of this meteorite plot at the high end of the ureilite trend, and it possesses olivine with Fa, Fe/Mn, Cr2O3, and CaO within the range of ureilites, suggesting ureilite affinity, however it lacks both pigeonite and low-Ca pyroxene. Specimens: 20 g including a probe mount on deposit at UNM, Jay Piatek holds the main mass. | ||||||||||||||||||||||||||||||||
Data from: MB110 Table 0 Line 0: |
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Plots: | O isotopes: | ||||||||||||||||||||||||||||||||
Institutions and collections |
UNM: Institute of Meteoritics
MSC03 2050
University of New Mexico
Albuquerque NM 87131-1126
USA, United States; Website (institutional address; updated 12 Feb 2015) |
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Catalogs: |
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References: | Published in Gattacceca J., McCubbin F.M., Grossman J., Bouvier A., Chabot N.L., D'Orazio M., Goodrich C., Greshake A., Gross J., Komatsu M., Miao B., and Schrader D. (2022) The Meteoritical Bulletin, No. 110. Meteorit. Planet. Sci. 1-4
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Geography: |
Statistics: This is 1 of 36 approved meteorites from Gao, Mali (plus 1 unapproved name) This is 1 of 128 approved meteorites from Mali (plus 2 unapproved names) | ||||||||||||||||||||||||||||||||
Proximity search: |