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Grove Mountains 021512 | |||||||||||||
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Basic information | Name: Grove Mountains 021512 This is an OFFICIAL meteorite name. Abbreviation: GRV 021512 Observed fall: No Year found: 2003 Country: Antarctica [Collected by Chinese Antarctic Research Expedition (CARE)] Mass: ![]() | ||||||||||||
Classification history: |
This is 1 of 627 approved meteorites classified as Ureilite. [show all] Search for other: Achondrites, Ureilites | ||||||||||||
Writeup![]() |
Writeup from MB 89:
Grove Mountains 021512 Antarctica Found 2003 Achondrite (ureilite) The 143.4 g meteorite is hemisphical in shape, and most of the surface is covered with black fusion crust. Classification and Mineralogy (CAS): It consists mainly of subhedral to anhedral olivine (up to 1.0-3.5 mm in size) and a few grains of pigeonite embedded in carbonaceous matrix. Some grains of olivine have 120° triple junctions. Pigeonite (En74.5±0.3Wo8.0±0.2Fs17.5±0.2) and olivine cores (Fo79.6±0.2) are homogeneous. All grains of olivine have FeO-poor rims (Fa as low as 6.4 mol%), which contain abundant fine-grained inclusions of Ni-poor metal and sulfide. The carbonaceous matrix is composed of two distinct assemblages, i.e. most abundant fine-grained mixtures of forsterite, enstatite, Ni-poor metal and sulfides, and less abundant diamond-bearing graphite patches or veins. The presence of diamond was confirmed by Raman spectrum and CL analyses. Limonite veins are common. Shock stage, S2/S3; weathering grade, W3. | ||||||||||||
Data from: MB89 Table 4 Line 35: |
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Institutions and collections |
CAS: Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China (institutional address; updated 16 Oct 2011) |
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Catalogs: |
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References: | Published in Meteoritical Bulletin, no. 89, MAPS 40, A201-A263 (2005)
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Geography:![]() |
Statistics: This is 1 of 43856 approved meteorites from Antarctica (plus 3802 unapproved names) | ||||||||||||
Proximity search: |