Antarctic Meteorite Newsletter, Volume 30, No. 2 - August 2007
Volume 31, No. 1 - February 2008
Petrographic Descriptions   (Select a sample)
 
CMS 04032
GRA 06158
GRO 06050
GRO 06054
GRO 06059
GRO 06068
LAP 04720
LAP 04721
LAP 04754
LAR 06317
LAR 06318
LAR 06867
LAR 06868
LAR 06869
LAR 06871
LAR 06872
LAR 06873
LAR 06874
RBT 04133
SCO 06012
SCO 06013
SCO 06014
SCO 06042
SCO 06043
 



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Antarctic Meteorite Newsletter 31,1 - Petrographic Descriptions

Sample No.: LAR 06869
Location: Larkman Nunatak
Field No.: 19740
Dimensions (cm):   3.0 x 2.5 x 1.5
Weight (g): 18.258
Meteorite Type:

CK6 Chondrite

Pairing: LAR 06869, LAR 06872, LAR 06873


Macroscopic Description: Kathleen McBride
The exteriors of these meteorites range from rough brown/black fusion crust to smooth black exterior. The interiors have dark gray to black matrix with evaporites, some are rusty and very hard and have small light colored inclusions.

 

Thin Section (,2) Description: Tim McCoy, Linda Welzenbach and Cari Corrigan
The sections exhibit a mixture of fine-grained mixture of olivine, calcic pyroxene and plagioclase with individual grains reaching a few hundred microns, but most grains of apparently finer grain size, perhaps owing to shock. Shock veins cross cut the sections forming a network. Vesicular, melted fusion crust was only present on one of the sections examined. Oxides and sulfide are relatively common to abundant.  Olivine is Fa34, pyroxene is an Al-bearing (2-4 wt.% Al2O3) augite of Fs12Wo50, and a small number of plagioclase analyses suggest considerable heterogeneity An43-88Or0-8. Iron oxide is abundant and appears to be magnetite with significant Fe3+ present (based on low totals), as well as 5 wt.% Cr2O3 and 2 wt.% Al2O3.   Sulfide is an Fe,Ni sulfide, likely pentlandite. The meteorites are strongly shocked and metamorphosed chondrites, probably CK6.


Oxygen Isotopic Analysis: D. Rumble, Geophysical Laboratory, Carnegie Institution of Washington
Magnetic fractions (magnetite) were analyzed (after ultrasonication in dilute HCl), which is important because an analysis of silicates will almost certainly give heavier small delta values.

Oxygen isotopic analyses of two small (2-5 mg) pieces of LAR 06872 yielded the following results:

δ17O = -5.87, δ18O = -2.44, Δ17O = -4.587
δ17O = -5.98, δ18O = -2.46, Δ17O = -4.692
[where Δ17O = δ17O – 0.526 x δ18O]


Thin Section Images

Plane-Polarized
Light LAR 06869
Reflective
Light LAR 06869
Cross-Polarized
Light LAR 06869
LAR 06869 - Plane-Polarized
LAR 06869 - Reflective
LAR 06869 - Cross-Polarized



Lab Images

North View
LAR 06869
LAR 06869 - North View