Nr. 92217587

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Rumuruti (R3) Meteorit, Tni-Haia 001. Ingen reservepris. - 17.19 g
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Rumuruti (R3) Meteorit, Tni-Haia 001. Ingen reservepris. - 17.19 g

Tni-Haia 001 24°52’48.45"N, 0°58’1.85"W Adrar, Algeria Find: 2022 Jan 5 Classification: Rumuruti chondrite (R3) History: The meteorite was found by meteorite hunters on January 5 and 6, 2022, in the southwestern part of the Algerian desert and subsequently purchased by the main mass holder on May 6, 2023, from a meteorite dealer in Agadir, Morocco. Physical characteristics: Many dark grayish to black fragments some of which partly covered with fusion crust. Petrography: The meteorite shows a dark grayish to black interior and is composed of well-defined, mostly rounded separated chondrules (apparent mean diameter about 350 µm) and mineral fragments set in abundant matrix dominated by Fe-rich olivine. Sodic plagioclase is present as small isolated grains dispersed throughout the matrix. Opaque phases are troilite, pentlandite, and Ti-bearing chromite; no metal has been detected. Geochemistry: olivine: Fa23.6±15.3 (Fa0.5-40.7, n=16); low-Ca pyroxene: Fs13.7±5.9Wo0.5±0.3 (Fs2.6-21.8Wo0.2-1.1, n=12) Shock stage: S2. Weathering grade: low. Classifier: A. Greshake, MNB This lot comes with certificate of authenticity. Thanks for your interest.

Nr. 92217587

Solgt
Rumuruti (R3) Meteorit, Tni-Haia 001. Ingen reservepris. - 17.19 g

Rumuruti (R3) Meteorit, Tni-Haia 001. Ingen reservepris. - 17.19 g

Tni-Haia 001 24°52’48.45"N, 0°58’1.85"W
Adrar, Algeria
Find: 2022 Jan 5

Classification: Rumuruti chondrite (R3)

History: The meteorite was found by meteorite hunters on January 5 and 6, 2022, in the southwestern part of the Algerian desert and subsequently purchased by the main mass holder on May 6, 2023, from a meteorite dealer in Agadir, Morocco.

Physical characteristics: Many dark grayish to black fragments some of which partly covered with fusion crust.

Petrography: The meteorite shows a dark grayish to black interior and is composed of well-defined, mostly rounded separated chondrules (apparent mean diameter about 350 µm) and mineral fragments set in abundant matrix dominated by Fe-rich olivine. Sodic plagioclase is present as small isolated grains dispersed throughout the matrix. Opaque phases are troilite, pentlandite, and Ti-bearing chromite; no metal has been detected.

Geochemistry: olivine: Fa23.6±15.3 (Fa0.5-40.7, n=16); low-Ca pyroxene: Fs13.7±5.9Wo0.5±0.3 (Fs2.6-21.8Wo0.2-1.1, n=12)

Shock stage: S2.
Weathering grade: low.
Classifier: A. Greshake, MNB
This lot comes with certificate of authenticity.
Thanks for your interest.

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