Showing 901–918 of 1086 results

Zagora 003 Eucrite #4 – 23,9 g

307,96 $

Zagora 003 is a fresh meteorite classified as eucrite of only 135 grams.

It was discovered near Zagora in Morocco by Ahmed Enaji on September 13, 2020.

The eucrites come from the Asteroid Vesta.

Writeup from MB 110:

Zagora 003 30°20’51.94″N, 5°36’41.79″W

Morocco

Find: 2020 Sep 13

Classification: HED achondrite (Eucrite)

History: Found by Ahmed Enaji on September 13, 2020. Bought from Zaid Oualguirah in 2020.

Physical characteristics: Several fusion crusted pieces with grey interior.

Petrography: (J. Gattacceca, CEREGE) Igneous rock with grain size about 500 µm. It contains melt rock areas, and other areas with variolitic texture. Main minerals are pyroxene and plagioclase. Other minerals: metal, troilite, chromite.

Geochemistry: Low-Ca pyroxene Fs34.1±0.8Wo5.7±1.1, FeO/MnO = 28.6±2.4 (n=4). Plagioclase An93.3±0.6Ab6.4±0.6Or0.3±0.1 (n=5). Chromite Cr# = 0.78 (n=1).

Classification: Achondrite (eucrite).

Specimens: Type specimen at CEREGE. Main mass with Jean Redelsperger.

Out of stock

Zagora 003 Eucrite #3 – 11,1 g

153,38 $

Zagora 003 is a fresh meteorite classified as eucrite of only 135 grams.

It was discovered near Zagora in Morocco by Ahmed Enaji on September 13, 2020.

The eucrites come from the Asteroid Vesta.

Writeup from MB 110:

Zagora 003 30°20’51.94″N, 5°36’41.79″W

Morocco

Find: 2020 Sep 13

Classification: HED achondrite (Eucrite)

History: Found by Ahmed Enaji on September 13, 2020. Bought from Zaid Oualguirah in 2020.

Physical characteristics: Several fusion crusted pieces with grey interior.

Petrography: (J. Gattacceca, CEREGE) Igneous rock with grain size about 500 µm. It contains melt rock areas, and other areas with variolitic texture. Main minerals are pyroxene and plagioclase. Other minerals: metal, troilite, chromite.

Geochemistry: Low-Ca pyroxene Fs34.1±0.8Wo5.7±1.1, FeO/MnO = 28.6±2.4 (n=4). Plagioclase An93.3±0.6Ab6.4±0.6Or0.3±0.1 (n=5). Chromite Cr# = 0.78 (n=1).

Classification: Achondrite (eucrite).

Specimens: Type specimen at CEREGE. Main mass with Jean Redelsperger.

Out of stock

Zagora 003 Eucrite #2 – 1,2 g

19,02 $

Zagora 003 is a fresh meteorite classified as eucrite of only 135 grams.

It was discovered near Zagora in Morocco by Ahmed Enaji on September 13, 2020.

The eucrites come from the Asteroid Vesta.

Writeup from MB 110:

Zagora 003 30°20’51.94″N, 5°36’41.79″W

Morocco

Find: 2020 Sep 13

Classification: HED achondrite (Eucrite)

History: Found by Ahmed Enaji on September 13, 2020. Bought from Zaid Oualguirah in 2020.

Physical characteristics: Several fusion crusted pieces with grey interior.

Petrography: (J. Gattacceca, CEREGE) Igneous rock with grain size about 500 µm. It contains melt rock areas, and other areas with variolitic texture. Main minerals are pyroxene and plagioclase. Other minerals: metal, troilite, chromite.

Geochemistry: Low-Ca pyroxene Fs34.1±0.8Wo5.7±1.1, FeO/MnO = 28.6±2.4 (n=4). Plagioclase An93.3±0.6Ab6.4±0.6Or0.3±0.1 (n=5). Chromite Cr# = 0.78 (n=1).

Classification: Achondrite (eucrite).

Specimens: Type specimen at CEREGE. Main mass with Jean Redelsperger.

Zagora 003 Eucrite #1 – 4,5 g

66,59 $

Zagora 003 is a fresh meteorite classified as eucrite of only 135 grams.

It was discovered near Zagora in Morocco by Ahmed Enaji on September 13, 2020.

The eucrites come from the Asteroid Vesta.

Writeup from MB 110:

Zagora 003 30°20’51.94″N, 5°36’41.79″W

Morocco

Find: 2020 Sep 13

Classification: HED achondrite (Eucrite)

History: Found by Ahmed Enaji on September 13, 2020. Bought from Zaid Oualguirah in 2020.

Physical characteristics: Several fusion crusted pieces with grey interior.

Petrography: (J. Gattacceca, CEREGE) Igneous rock with grain size about 500 µm. It contains melt rock areas, and other areas with variolitic texture. Main minerals are pyroxene and plagioclase. Other minerals: metal, troilite, chromite.

Geochemistry: Low-Ca pyroxene Fs34.1±0.8Wo5.7±1.1, FeO/MnO = 28.6±2.4 (n=4). Plagioclase An93.3±0.6Ab6.4±0.6Or0.3±0.1 (n=5). Chromite Cr# = 0.78 (n=1).

Classification: Achondrite (eucrite).

Specimens: Type specimen at CEREGE. Main mass with Jean Redelsperger.

Out of stock

Lahmada 048 #3 Ureilite – 4,7 g

84,42 $

Lahmada 048 is an achondrite ureilite meteorite of only 59 grams discovered in the Western Sahara in a concentration area called Lahmada.

It was discovered on September 23, 2020 by Brahim Elguirah.

Lahmada 048 certainly contains diamonds in view of the difficulties to cut it.

The diamonds, which are rarely larger than a few micrometers in diameter, are probably the result of high-pressure shock waves produced by the collision of the parent body of the ureilites with other asteroids.

Writeup from MB 110:

Lahmada 048 27°24’20.78″N, 9°51’13.07″W

Saguia el Hamra, Western Sahara

Find: 2020 Sep 23

Classification: Ureilite

History: The meteorite was found by Brahim Elguirah. The meteorite was bought by Jean Redelsperger from Zaid Oualguirah in 2020.

Physical characteristics: A single dark brown stone

Petrography: (J. Gattacceca, CEREGE) Aggregate of blocky olivine grains (grain size 800 µm) with reduced margins. Metal, originally present along olivine rims, is almost entirely replaced by terrestrial weathering products. Contains a significant amount of carbon material, likely diamonds in view of the extreme difficulty to saw the rock.

Geochemistry: Olivine Fa21.9±0.4, CaO 0.36±0.02 wt%, CrO3 0.65±0.02, FeO/MnO = 53.4±7.9 (n=4). Olivine rim Fa5.1 (n=1).

Classification: Ureilite

Specimens: Type specimen at CEREGE. Mais mass with Jean Redelsperger.

 

Out of stock

Lahmada 048 #1 Ureilite – 23,3 g

414,97 $

Lahmada 048 is an achondrite ureilite meteorite of only 59 grams discovered in the Western Sahara in a concentration area called Lahmada.

It was discovered on September 23, 2020 by Brahim Elguirah.

Lahmada 048 certainly contains diamonds in view of the difficulties to cut it.

The diamonds, which are rarely larger than a few micrometers in diameter, are probably the result of high-pressure shock waves produced by the collision of the parent body of the ureilites with other asteroids.

Writeup from MB 110:

Lahmada 048 27°24’20.78″N, 9°51’13.07″W

Saguia el Hamra, Western Sahara

Find: 2020 Sep 23

Classification: Ureilite

History: The meteorite was found by Brahim Elguirah. The meteorite was bought by Jean Redelsperger from Zaid Oualguirah in 2020.

Physical characteristics: A single dark brown stone

Petrography: (J. Gattacceca, CEREGE) Aggregate of blocky olivine grains (grain size 800 µm) with reduced margins. Metal, originally present along olivine rims, is almost entirely replaced by terrestrial weathering products. Contains a significant amount of carbon material, likely diamonds in view of the extreme difficulty to saw the rock.

Geochemistry: Olivine Fa21.9±0.4, CaO 0.36±0.02 wt%, CrO3 0.65±0.02, FeO/MnO = 53.4±7.9 (n=4). Olivine rim Fa5.1 (n=1).

Classification: Ureilite

Specimens: Type specimen at CEREGE. Mais mass with Jean Redelsperger.

 

Out of stock

Lahmada 048 #2 Ureilite – 2,5 g

45,18 $

Lahmada 048 is an achondrite ureilite meteorite of only 59 grams discovered in the Western Sahara in a concentration area called Lahmada.

It was discovered on September 23, 2020 by Brahim Elguirah.

Lahmada 048 certainly contains diamonds in view of the difficulties to cut it.

The diamonds, which are rarely larger than a few micrometers in diameter, are probably the result of high-pressure shock waves produced by the collision of the parent body of the ureilites with other asteroids.

Writeup from MB 110:

Lahmada 048 27°24’20.78″N, 9°51’13.07″W

Saguia el Hamra, Western Sahara

Find: 2020 Sep 23

Classification: Ureilite

History: The meteorite was found by Brahim Elguirah. The meteorite was bought by Jean Redelsperger from Zaid Oualguirah in 2020.

Physical characteristics: A single dark brown stone

Petrography: (J. Gattacceca, CEREGE) Aggregate of blocky olivine grains (grain size 800 µm) with reduced margins. Metal, originally present along olivine rims, is almost entirely replaced by terrestrial weathering products. Contains a significant amount of carbon material, likely diamonds in view of the extreme difficulty to saw the rock.

Geochemistry: Olivine Fa21.9±0.4, CaO 0.36±0.02 wt%, CrO3 0.65±0.02, FeO/MnO = 53.4±7.9 (n=4). Olivine rim Fa5.1 (n=1).

Classification: Ureilite

Specimens: Type specimen at CEREGE. Mais mass with Jean Redelsperger.

 

Out of stock

Allende CV3 #9 – 3,4 g

141,49 $

The Allende meteorite fell in Mexico in 1969.

It is often considered as the “Rosetta Stone” of planetologists, because it has improved our knowledge on the origins of our solar system. This meteorite was formed before our planet, in the very first moments of the solar system. It preserves in its heart the traces of the nebula which generated the Sun and its procession of planets.

Out of stock

Allende CV3 #8 – 2,8 g

116,52 $

The Allende meteorite fell in Mexico in 1969.

It is often considered as the “Rosetta Stone” of planetologists, because it has improved our knowledge on the origins of our solar system. This meteorite was formed before our planet, in the very first moments of the solar system. It preserves in its heart the traces of the nebula which generated the Sun and its procession of planets.

Out of stock

Allende CV3 #7 – 1,6 g

68,96 $

The Allende meteorite fell in Mexico in 1969.

It is often considered as the “Rosetta Stone” of planetologists, because it has improved our knowledge on the origins of our solar system. This meteorite was formed before our planet, in the very first moments of the solar system. It preserves in its heart the traces of the nebula which generated the Sun and its procession of planets.

Out of stock

Allende CV3 #6 – 1,8 g

77,29 $

The Allende meteorite fell in Mexico in 1969.

It is often considered as the “Rosetta Stone” of planetologists, because it has improved our knowledge on the origins of our solar system. This meteorite was formed before our planet, in the very first moments of the solar system. It preserves in its heart the traces of the nebula which generated the Sun and its procession of planets.

Out of stock

Allende CV3 #5 – 3,3 g

136,74 $

The Allende meteorite fell in Mexico in 1969.

It is often considered as the “Rosetta Stone” of planetologists, because it has improved our knowledge on the origins of our solar system. This meteorite was formed before our planet, in the very first moments of the solar system. It preserves in its heart the traces of the nebula which generated the Sun and its procession of planets.

Out of stock

Allende CV3 #4 – 3,7g

154,57 $

The Allende meteorite fell in Mexico in 1969.

It is often considered as the “Rosetta Stone” of planetologists, because it has improved our knowledge on the origins of our solar system. This meteorite was formed before our planet, in the very first moments of the solar system. It preserves in its heart the traces of the nebula which generated the Sun and its procession of planets.

Out of stock

Allende CV3 #2 – 4 g

166,46 $

The Allende meteorite fell in Mexico in 1969.

It is often considered as the “Rosetta Stone” of planetologists, because it has improved our knowledge on the origins of our solar system. This meteorite was formed before our planet, in the very first moments of the solar system. It preserves in its heart the traces of the nebula which generated the Sun and its procession of planets.

Out of stock

Allende CV3 #3 – 4,2 g

174,79 $

The Allende meteorite fell in Mexico in 1969.

It is often considered as the “Rosetta Stone” of planetologists, because it has improved our knowledge on the origins of our solar system. This meteorite was formed before our planet, in the very first moments of the solar system. It preserves in its heart the traces of the nebula which generated the Sun and its procession of planets.

Out of stock

Allende CV3 #1 – 8,8 g

366,22 $

The Allende meteorite fell in Mexico in 1969.

It is often considered as the “Rosetta Stone” of planetologists, because it has improved our knowledge on the origins of our solar system. This meteorite was formed before our planet, in the very first moments of the solar system. It preserves in its heart the traces of the nebula which generated the Sun and its procession of planets.

Out of stock

NWA 13487 Mésosidérite #2 – 6,2 g

103,44 $

NWA 13487 is a very nice fresh mesosiderite meteorite of only 58 grams.

Writeup from MB 109:

Northwest Africa 13487 (NWA 13487)

(Northwest Africa)

Purchased: 2019 Jun

Classification: Mesosiderite

History: Bought in Ensisheim in June 2019 from Norddine Azelmat.

Physical characteristics: A dark brown irregular stone.

Petrography: (J. Gattacceca, CEREGE) Brecciated rock with a silicate fraction composed of plagioclase and low-Ca pyroxene (typical size 200 m), and less abundant Ca-pyroxene. Abundant contorted multi-mm sized metal grains (~30 vol%). Other minerals: troilite, merrillite, SiO2.

Geochemistry: Pyroxene Fs31.3±0.1Wo2.2±0.1, FeO/MnO = 24.1 (n=2). Plagioclase An91.6Ab8.2Or0.3 (n=2).

Classification: Mesosiderite.

Specimens: Type specimen at CEREGE. Main mass with Jean Redelsperger.

 

Out of stock

NWA 13487 Mésosidérite #1 – 34,4 g

573,11 $

NWA 13487 is a very nice fresh mesosiderite meteorite of only 58 grams.

Writeup from MB 109:

Northwest Africa 13487 (NWA 13487)

(Northwest Africa)

Purchased: 2019 Jun

Classification: Mesosiderite

History: Bought in Ensisheim in June 2019 from Norddine Azelmat.

Physical characteristics: A dark brown irregular stone.

Petrography: (J. Gattacceca, CEREGE) Brecciated rock with a silicate fraction composed of plagioclase and low-Ca pyroxene (typical size 200 m), and less abundant Ca-pyroxene. Abundant contorted multi-mm sized metal grains (~30 vol%). Other minerals: troilite, merrillite, SiO2.

Geochemistry: Pyroxene Fs31.3±0.1Wo2.2±0.1, FeO/MnO = 24.1 (n=2). Plagioclase An91.6Ab8.2Or0.3 (n=2).

Classification: Mesosiderite.

Specimens: Type specimen at CEREGE. Main mass with Jean Redelsperger.