Re-Os Systematics and HSE Distribution in Tieschitz (H3.6): Two Isochrons for One Meteorite

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Scientific paper

We present new Re-Os and HSE data for mineral separates of Tieschitz
(H3). While metal and several types of chondrules form well-defined
isochron with pristine age (4.59 Ga), the samples of white matrix and
bleached chondrules give apparent age of 2.0 Ga.

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