Here we go again - Bencubbin time once more :-)

Best regards,

Bernd


MASON B. (1962) Meteorites (John Wiley and Sons, Inc., p. 128):

A few mesosiderites (e.g., Bencubbin, Patwar) have almost
pure MgSiO3 as the pyroxene; in these meteorites nickel-iron
is predominant, and they should probably be classed as irons
with silicate inclusions.

GEHRELS T. (1979) Asteroids (UoA Press,
Part VI, Origin of Iron Meteorites, p. 918):

There are other metal-rich meteorites with well-analyzed metal.
Bencubbin, Weatherford and Mt. Egerton have chondritic levels
of Ir (2-3 �g/g) (Kallemeyn et al. 1978; Scott and Wasson 1976).
Bencubbin has been identified as an impact-produced breccia.
Its metal has low concentrations of volatile siderophiles like Ga
and Ge which show a correlation between abundance and
condensation temperature. The only known meteorites containing
silicate and appreciable metal with non-chondritic levels of Ir are
those in iron group IB.

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