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Wolfkop | |||||||||||||||||||||||||||||||||||||||
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Basic information | Name: Wolfkop This is an OFFICIAL meteorite name. Abbreviation: There is no official abbreviation for this meteorite. Observed fall: No Year found: 2021 Country: South Africa Mass: ![]() | ||||||||||||||||||||||||||||||||||||||
Classification history: |
This is 1 of 8831 approved meteorites (plus 4 unapproved names) classified as L5. [show all] Search for other: L chondrites, L chondrites (type 4-7), Ordinary chondrites, and Ordinary chondrites (type 4-7) | ||||||||||||||||||||||||||||||||||||||
Comments: | Approved 30 Jul 2023 | ||||||||||||||||||||||||||||||||||||||
Writeup![]() |
Writeup from MB 112:
Wolfkop 29°42.546’S, 19°37.912’E Northern Cape, South Africa Find: 2021 Aug 27 Classification: Ordinary chondrite (L5) History: A single stone discovered by G.F. Lombaard while farming. Brought to attention of R. Gibson via G. Goncalves (USP). Physical characteristics: A 90.26 g weakly magnetic stone with flattened tetrahedral shape, 7x4.5x2 cm. Upper surfaces are covered by thin (<< 1 mm) brownish black fusion crust that has been chipped away in several shallow pits that expose dark brown oxidized interior; faces intersect in obtuse angles and edges are rounded. Basal surface lacks fusion crust and is formed by an irregular fracture at an acute angle to other faces; it exposes oxidized mid/dark brown granular-textured interior with sub-mm shiny metal flakes and a few <1 mm chondrules. Petrography: (R.L. Gibson and L.D. Ashwal, Wits) Chondrules are mostly poorly defined, with only a few, large (1.0-2.3 mm) pyroxene-rich (RP, POP) types visible; mostly slightly flattened shapes, but with a few spherical examples present. Irregular metal and troilite grains are up to 0.3 mm in size, with metal showing variable Ni content. Mineralogy: high-Ca Pyx (5%) - low-Ca Pyx (7%) - Ol (70%) - Fsp (6%) - metal (9%) - troilite (3%) and trace chromite, phosphate. The matrix grain size of ~ 50 μm and elongate-polygonal grain shapes indicate significant metamorphic recrystallization. Planar fractures dominate over irregular fractures in Ol and Pyx; Ol shows mosaicism. Fsp shows undulose extinction, PDF and possible maskelynite. Displacements of ~0.1 mm occur along an irregular network of planar to curved fractures that host dark shock veins up to 1 mm wide. Geochemistry: Mineral compositions and geochemistry: (R.L. Gibson and L.D. Ashwal, Wits) Ol: Fa25.1±0.6 (24.1-26.5; N=12); low-Ca Pyx: Fs21.1±0.2 (20.7-21.6; N=14), Wo1.5±0.2 (1.1-1.8; N=14); high-Ca Pyx: Fs8.1±0.4 (7.2-8.8; N=10), Wo46.7±0.4 (44.7-47.2; N=10). Relatively homogeneous Ol and low-Ca Pyx indicate substantial reequilibration. Classification: Ordinary chondrite (L5), shock stage S4, weathering W2 Specimens: Type specimen (Wits) 82.54 g; cut surface exposes metal flakes up to 2 mm in length in variably weathered (light to dark brown) matrix; remaining surfaces largely intact fusion crust, except for several shallow cm-wide chips. Polished thin section and 1.73 g offcut. | ||||||||||||||||||||||||||||||||||||||
Data from: MB112 Table 0 Line 0: |
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Institutions and collections |
Wits: Curator of Fossil and Rock Collections
c/o Evolutionary Studies Institute
University of the Witwatersrand
Private Bag 3
WITS 2050
Johannesburg
South Africa, South Africa (institutional address; updated 3 May 2019) USP: Museu de Geociências - USP Rua do Lago, 562 CEP: 05508-080 Butantã - SP Brazil, Brazil; Website (institutional address; updated 22 Oct 2022) |
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Catalogs: |
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References: | Published in Meteoritical Bulletin, no. 112, in preparation (2023)
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Geography:![]() |
Statistics: This is 1 of 11 approved meteorites from Northern Cape, South Africa (plus 1 unapproved name) This is 1 of 49 approved meteorites from South Africa (plus 2 unapproved names) (plus 4 impact craters) | ||||||||||||||||||||||||||||||||||||||
Proximity search: |