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Shinejinst | |||||||||||||||||||||||||||||||||||||
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Basic information | Name: Shinejinst This is an OFFICIAL meteorite name. Abbreviation: There is no official abbreviation for this meteorite. Observed fall: No Year found: 2018 Country: Mongolia Mass: 693 g | ||||||||||||||||||||||||||||||||||||
Classification history: |
This is 1 of 6493 approved meteorites (plus 2 unapproved names) classified as H4. [show all] Search for other: H chondrites, H chondrites (type 4-7), Ordinary chondrites, and Ordinary chondrites (type 4-7) | ||||||||||||||||||||||||||||||||||||
Comments: | Approved 1 Jan 2020 | ||||||||||||||||||||||||||||||||||||
Writeup |
Writeup from MB 109:
Shinejinst 44°37’15.6"N, 99°012’38.1"E Bayankhongor, Mongolia Find: 2018 Aug 30 Classification: Ordinary chondrite (H4) History: Four fragments (156.17, 101.73, 208.17, and 227.35 g) were found on 30 and 31 August 2018 by the UrFU - IAG-MAS meteorite expedition-2018 in Southern Gobi (Pastukhovich A.Yu., Kolunin R.N., Larionov M.Yu., Muraviev L.A., Petrova E.V., Yakovlev G.A., Naasa Ochir) 10 km northwest of Shinejinst, Bayankhongor aimag (province), Mongolia. Petrography: Classification (K. Dugushkina and S. Berzin, RAS-UB). Petrographic observation of a polished section shows a fine-grained inequigranular recrystallized matrix and chondrules (25%). Chondrite consists of olivine 50%, orthopyroxene 15%, clinopyroxene 10%, plagioclase 15%, chromite 3%, troilite 3-4%, Fe-Ni-metal 3-4%. Also chondrite contains accessory apatite and ilmenite. Predominate porphyritic olivine (PO) and porphyritic olivine-pyroxene (POP) chondrules. Chondrules mostly have even boundaries. Petrographic type is 4. Chromite-plagioclase assemblages are found in the recrystallized matrix. The assemblages range in size from 10-350 µm and consist of 0.2-30- µm-size rounded, euhedral, subhedral and anhedral chromite grains surrounded by plagioclase or glass of plagioclase composition. Moderate oxidation of metal, about 20-60% being affected, alteration of mafic silicates is beginning (weathering grade - W2). The samples are transected by dark shock veins. Shock stage is S3/4. Geochemistry: EDX analyses by K. Dugushkina, RAS-UB. The meteorite is composed olivine Fa20±2.1 (N=37), low-Ca pyroxene Fs18±0.4En80±0.4Wo1±0.3 (N=17), plagioclase An24±3.5 (N=9), clinopyroxene En49±3.6Fs10±1.7Wo42±2.8 (N=6), chromite, troilite, kamacite (Ni 5.5-6.8 wt%), taenite (Ni 19.7-36 wt%), apatite and ilmenite. Average composition of chromite (N=9): Cr2O3 55.6±0.9 wt%, FeO 28.4±1.4 wt%, MgO 4.8±1.1 wt%, Al2O3 7.8±0.8 wt%, TiO2 2.2±0.2 wt%, MnO 0.7±0.04 wt%, SiO2 0.5±0.17 wt%, CaO 0.1±0.02 wt%, NiO 0.2±0.01 wt%. Classification: Ordinary chondrite (H4) Specimens: 591 g (3 samples) at IAG-MAS; 96.43 g sample and 5.30 g cut-off and thin section at UrFU. | ||||||||||||||||||||||||||||||||||||
Data from: MB109 Table 0 Line 0: |
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Institutions and collections |
UrFU: Ural Federal University, 620002, 19 Mira street, Ekaterinburg, Russia (institutional address; updated 14 Jan 2015) RAS-UB: Zavaritsky Institute of Geology and Geochemistry Russian Academy of Sciences, Ural Branch 15 Akademika Vonsovskogo str., Ekaterinburg, 620016, Russia (institutional address; updated 19 Apr 2018) IAG-MAS: Institute of Astronomy and Geophysics Mongolian Academy of Sciences P.O.B-152, Ulaanbaatar – 51, 13343, Mongolia (institutional address; updated 30 Nov 2019) |
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Catalogs: |
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References: | Published in Meteoritical Bulletin, no. 109, in preparation (2020)
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Photos: |
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Geography: |
Statistics: This is the only approved meteorite from Bayanhongor, Mongolia This is 1 of 12 approved meteorites from Mongolia (plus 4 unapproved names) (plus 1 impact crater) | ||||||||||||||||||||||||||||||||||||
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Also see: |
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Revision history: |
This lists important revisions made to data for this record.
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