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Slaton (b)
Basic information Name: Slaton (b)
     This is an OFFICIAL meteorite name.
Abbreviation: There is no official abbreviation for this meteorite.
Observed fall: No
Year found: 1940s
Country: United States
Mass:help 6 kg
Classification
  history:
Meteoritical Bulletin:  MB 102  (2013)  Iron, IIAB
Recommended:  Iron, IIAB    [explanation]

This is 1 of 137 approved meteorites classified as Iron, IIAB.   [show all]
Search for other: IIAB irons, Iron meteorites, and Metal-rich meteorites
Comments: Approved 30 Dec 2013
Writeuphelp
Writeup from MB 102:

Slaton (b)        33.4336, -101.7498

Lubbock County, Texas, United States

Found: 1940s

Classification: Iron meteorite (IIAB)

History: The meteorite was found at Cade Farm on Union Rd., west of Slaton, Texas, by H.M. Cade reportedly sometime in the 1940s when he was plowing his cotton field. This comes from the same farm and was found by the same person as the L4 chondrite Slaton, which now takes on the synonym Slaton (a). Mr. Cade would always challenge his grandchildren to see if they could pick up this meteorite. It sat on Mr. Cade’s fireplace mantel until his death and was eventually passed down to his grandson. Frank Carroll purchased the meteorite from the grandson in August, 2013.

Physical characteristics: Single iron mass, approximately 20 × 15 × 8 cm, with a centered, large rounded depression, oxidized exterior with some exfoliation; saw cut reveals bright metallic interior with a few small weathering cracks or oxidized grain boundaries.

Petrography: (C. Agee, UNM) This iron meteorite consists primarily of kamacite (~99%) with minor amounts of schreibersite and taenite. Schreibersite frequently occurs as isolated en echelon rhabdites 10-200 μm wide, up to ~1 mm long. Most taenite occurs as isolated skeletal inclusions 10-200 μm wide, up to 1 mm long, within host kamacite. No troilite or silicates observed. Etched surface on 60 × 30 mm slice shows kamacite bands with apparent widths 2-6 mm, abundant Neumann lines.

Geochemistry: (C. Agee, UNM) Bulk composition, ICPMS: Ni 5.7 wt%, Co 0.40 wt%, Cu 88 ppm, W 180 ppm, Ga 370 ppm, Ge 84 ppm, As 12.5 ppm, Ir 21 ppm, Au 1.3 ppm. Kamacite, EMPA, focused beam: Fe 94.3±1.8 wt%, Ni 6.1±0.4 wt%, Co 0.48±0.03 wt%, W 340±170 ppm, Cu <100 ppm, Ga 570±100 ppm, Ge <100 ppm, n=16.

Classification: Iron meteorite (IIAB). Coarsest octahedrite.

Specimens: 24 g on deposit at UNM, Frank Carroll holds the main mass.

Data from:
  MB102
  Table 0
  Line 0:
State/Prov/County:Texas
Date:1940s
Latitude:33.4336
Longitude:-101.7498
Mass (g):6000
Pieces:1
Class:Iron, IIAB
Classifier:C. Agee, UNM
Type spec mass (g):24
Type spec location:UNM
Main mass:Frank Carroll
Comments:Submitted by C. Agee
Institutions
   and collections
UNM: Institute of Meteoritics MSC03 2050 University of New Mexico Albuquerque NM 87131-1126 USA, United States; Website (institutional address; updated 12 Feb 2015)
Catalogs:
References: Published in Meteoritical Bulletin, no. 102, MAPS 50, 1662, September 2015
Find references in NASA ADS:
Find references in Google Scholar:
Photos:
CreditPhotos
Photos uploaded by members of the Encyclopedia of Meteorites.
    (Caution, these are of unknown reliability)
David L. Ribeca   
Frank Carroll         
Geography:

United States
Coordinates:
     Recommended::   (33° 26' 1"N, 101° 44' 59"W)

Statistics:
     This is 1 of 311 approved meteorites from Texas, United States (plus 2 unapproved names) (plus 3 impact craters)
     This is 1 of 1827 approved meteorites from United States (plus 358 unapproved names) (plus 28 impact craters)
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