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NWA 15171 Mésosidérite #24 - 1,7 g

NWA 15171 Mésosidérite #24 – 1,7 g

11,70 $

NWA 15171 is a rare mesosiderite meteorite.

Mesosiderites are brecciated rocks containing silicate and metallic components, the silicates are mainly fragments of igneous rocks.

Writeup from MB 112:

Northwest Africa 15171 (NWA 15171)

Adrar, Algeria

Purchased: 2022

Classification: Mesosiderite

History: Bought by Jean Redelsperger from Mohamed Elguirah in 2022.

Physical characteristics: Many brown ireggular stones without fusion crust.

Petrography: (J. Gattacceca, CEREGE) The rock contains similar abundances of silicate minerals (pyroxene, and plagioclase), and metal and its weathering products. Silicate grain size is about 200 µm. Plagioclase and low-Ca pyroene dominate over Ca-pyroxene. Fe,Ni metal and troilite have been mostly replaced by terrestrial weathering products.

Geochemistry: Low-Ca pyroxene Fs31.4±2.0Wo3.8±0.2, range Fs29.5-35.9, FeO/MnO = 26.4±4.9 (n=7). Plagioclase An92.5±2.1Ab7.4±2.0Or0.1±0.1 (n=4).

Classification: Achondrite (mesosiderite)

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

NWA 15171 Mésosidérite #23 - 1,8 g

NWA 15171 Mésosidérite #23 – 1,8 g

12,88 $

NWA 15171 is a rare mesosiderite meteorite.

Mesosiderites are brecciated rocks containing silicate and metallic components, the silicates are mainly fragments of igneous rocks.

Writeup from MB 112:

Northwest Africa 15171 (NWA 15171)

Adrar, Algeria

Purchased: 2022

Classification: Mesosiderite

History: Bought by Jean Redelsperger from Mohamed Elguirah in 2022.

Physical characteristics: Many brown ireggular stones without fusion crust.

Petrography: (J. Gattacceca, CEREGE) The rock contains similar abundances of silicate minerals (pyroxene, and plagioclase), and metal and its weathering products. Silicate grain size is about 200 µm. Plagioclase and low-Ca pyroene dominate over Ca-pyroxene. Fe,Ni metal and troilite have been mostly replaced by terrestrial weathering products.

Geochemistry: Low-Ca pyroxene Fs31.4±2.0Wo3.8±0.2, range Fs29.5-35.9, FeO/MnO = 26.4±4.9 (n=7). Plagioclase An92.5±2.1Ab7.4±2.0Or0.1±0.1 (n=4).

Classification: Achondrite (mesosiderite)

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

TURPAN 003 #31 Fer - 2,6 g

TURPAN 003 #31 Fer – 2,6 g

49,14 $
Turpan 003 is an iron meteorite.
It was discovered in 2022 in China’s Xinjiang Province.
What makes this meteorite unique in the world is its natural structure, which is unusual for an iron meteorite.
In fact, the structure of metallic meteorites is usually revealed by acid.
Another unique feature is the green, bubbly silicate inclusions it contains.
Further studies are currently underway.

 

TURPAN 003 #30 Fer - 1,3 gOut of stock

TURPAN 003 #30 Fer – 1,3 g

30,42 $
Turpan 003 is an iron meteorite.
It was discovered in 2022 in China’s Xinjiang Province.
What makes this meteorite unique in the world is its natural structure, which is unusual for an iron meteorite.
In fact, the structure of metallic meteorites is usually revealed by acid.
Another unique feature is the green, bubbly silicate inclusions it contains.
Further studies are currently underway.

 

Trinitite #58 - 1 gOut of stock

Trinitite #58 – 1 g

51,48 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitite had taken the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #57 - 1,8 gOut of stock

Trinitite #57 – 1,8 g

92,42 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitite had taken the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #56 - 0,8 gOut of stock

Trinitite #56 – 0,8 g

40,96 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitite had taken the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #55 - 1,1 g

Trinitite #55 – 1,1 g

56,16 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitite had taken the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #54 - 0,5 gOut of stock

Trinitite #54 – 0,5 g

25,74 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitite had taken the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #53 - 1 g

Trinitite #53 – 1 g

51,48 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitite had taken the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

NWA 15971 Pallasite #32 - 2,4 g

NWA 15971 Pallasite #32 – 2,4 g

56,16 $

NWA 15971 is a pallasite meteorite.

Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.

Pallasites are among the most visually striking meteorites.

 

 

NWA 15971 Pallasite #31 - 2,3 gOut of stock

NWA 15971 Pallasite #31 – 2,3 g

53,82 $

NWA 15971 is a pallasite meteorite.

Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.

Pallasites are among the most visually striking meteorites.

 

 

NWA 15971 Pallasite #30 - 1,6 gOut of stock

NWA 15971 Pallasite #30 – 1,6 g

37,44 $

NWA 15971 is a pallasite meteorite.

Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.

Pallasites are among the most visually striking meteorites.

 

 

NWA 15971 Pallasite #29 - 3,3 g

NWA 15971 Pallasite #29 – 3,3 g

77,22 $

NWA 15971 is a pallasite meteorite.

Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.

Pallasites are among the most visually striking meteorites.

 

 

NWA 15971 Pallasite #28 - 1,6 g

NWA 15971 Pallasite #28 – 1,6 g

37,44 $

NWA 15971 is a pallasite meteorite.

Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.

Pallasites are among the most visually striking meteorites.

 

 

NWA 15971 Pallasite #27 - 3,3 g

NWA 15971 Pallasite #27 – 3,3 g

77,22 $

NWA 15971 is a pallasite meteorite.

Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.

Pallasites are among the most visually striking meteorites.

 

 

NWA 15971 Pallasite #26 - 2,8 g

NWA 15971 Pallasite #26 – 2,8 g

65,52 $

NWA 15971 is a pallasite meteorite.

Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.

Pallasites are among the most visually striking meteorites.

 

 

TURPAN 003 #29 Fer - 2,4 g

TURPAN 003 #29 Fer – 2,4 g

56,16 $
Turpan 003 is an iron meteorite.
It was discovered in 2022 in China’s Xinjiang Province.
What makes this meteorite unique in the world is its natural structure, which is unusual for an iron meteorite.
In fact, the structure of metallic meteorites is usually revealed by acid.
Another unique feature is the green, bubbly silicate inclusions it contains.
Further studies are currently underway.