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Yarle Lakes 004 | |||||||||||||||||||||||||||||||||||
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Basic information | Name: Yarle Lakes 004 This is an OFFICIAL meteorite name. Abbreviation: There is no official abbreviation for this meteorite. Observed fall: No Year found: 2009 Country: Australia Mass: ![]() | ||||||||||||||||||||||||||||||||||
Classification history: |
This is 1 of 121 approved meteorites classified as CK4. [show all] Search for other: Carbonaceous chondrites, Carbonaceous chondrites (equilibrated), CK chondrites, CK chondrites (type 4-6), and CV-CK clan chondrites | ||||||||||||||||||||||||||||||||||
Comments: | Approved 18 Jan 2011 | ||||||||||||||||||||||||||||||||||
Writeup![]() |
Writeup from MB 99:
Yarle Lakes 004 30°30’S, 131°28’E South Australia, Australia Found: 11 May 2009 Classification: Carbonaceous chondrite (CK4) History: D. Bradley found a single piece lying on the Nullarbor Plain. Physical characteristics: The meteorite weighs 4.6 g and measures 2.2 cm x 1.6 cm x 0.7 cm. The surface is dark maroon to black and has no obvious fusion crust. The freshly cut surface reveals a dark rusted brown interior with several paler chondrules scattered throughout. Petrography: (Kim Lai N. Bell, Monash) Large PO chondrules within a dark stained, fine-grained matrix and are difficult to discern due to the staining. Chondrules have a size range of 0.3-1 mm, with an average diameter of 0.6 mm. Mineralogy differs from an ordinary chondrite in that it contains no obvious metals or sulfides. Mineralogy dominated by olivine, plagioclase, pyroxenes and magnetite. Olivine and pyroxene grains have straight to undulose extinctions and occur within chondrules or as fragments in the matrix. Plagioclase tends to occur as small grains (≤50 μm) within both the matrix and chondrules. The silicates are stained a rusty brown, with up to 75% staining affecting them. Magnetite (4%) grains are irregular shaped, <0.1 mm in size and can be found rimming chondrules and within the matrix. Geochemistry: EMPA (wt%) Olivine: SiO2 = 36.85, TiO2 = 0.02, Al2O3 = 0.02, FeO = 28.87, MnO = 0.26, MgO = 34.49, CaO = 0.02, Na2O = 0.01, K2O = 0.00, (Fa31.95±0.13, n = 6). Plagioclase: SiO2 = 55.73, TiO2 = 0.01, Al2O3 = 26.27, FeO = 0.52, MnO = 0.01, MgO = 0.22, CaO = 9.71, Na2O = 5.83, K2O = 0.65 (An47.26±18.59, n = 5). Pentlandite: Fe = 27.96, Ni = 30.66, Cr = 1.26, Mg = 0.71. Magnetite: Fe = 61.25, Cr = 3.27, Al = 1.33, Ti = 0.74, Mg = 0.34, Ni = 0.19. Classification: Carbonaceous chondrite (CK4, S2, W1-4). Specimens: Sample and one thin section held by A. Tomkins at Monash. | ||||||||||||||||||||||||||||||||||
Data from: MB99 Table 0 Line 0: |
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Institutions and collections |
Monash: Building 28
School of Geosciences
Monash University
Victoria 3800
Australia, Australia (institutional address; updated 12 Dec 2012) |
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Catalogs: |
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References: | Published in Meteoritical Bulletin, No. 99, April 2012, MAPS 47, E1-E52 (2012) [published online only]
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Geography:![]() |
Statistics: This is 1 of 240 approved meteorites from South Australia, Australia (plus 3 unapproved names) (plus 4 impact craters) This is 1 of 718 approved meteorites from Australia (plus 46 unapproved names) (plus 27 impact craters) | ||||||||||||||||||||||||||||||||||
Proximity search: |