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NWA 15171 Mésosidérite #2 – 6,5 g

30,91 $

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.

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NWA 15171 Mésosidérite #1 – 16,1 g

77,29 $

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.

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Sayh al Uhaymir 001 L5 #4 – 183 g

282,98 $

Sayh al Uhaymir 001 is a meteorite that was discovered in the Sultanate of Oman.

This is a significant fall of over 450 kg.

I was lucky enough to be able to prospect on the place and find some fragments of this meteorite in 2011.

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Sayh al Uhaymir 001 L5 #3 – 279 g

497,02 $

Sayh al Uhaymir 001 is a meteorite that was discovered in the Sultanate of Oman.

This is a significant fall of over 450 kg.

I was lucky enough to be able to prospect on the place and find some fragments of this meteorite in 2011.

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Out of stock

TARDA C2 Ung #26 – 20 g

4.756,13 $

TARDA is a meteorite that fell in Morocco on August 25, 2020.
This meteorite has been classified as C2 ungrouped, a rare type of very primitive carbonaceous.
Tagish lake is a meteorite of the same type and sells for over 1000 euros per gram.
This meteorite is composed of many very small fragments, beautiful pieces with crusts are rare.
Isotopic analyses show that some pieces have values close to CI chondrites, and other pieces have Yamato (CY) values..
An important meteorite at the scientific level in the years to come.

Writeup from MB 109 :

Tarda 31° 49′ 35″N, 4° 40′ 46″W

Morocco

Confirmed fall : 2020

Classification: Carbonaceous chondrite (C2, ungrouped)

Classification : (C. Agee, UNM; K. Ziegler, UNM; A. Irving, UWS; L. Garvie, ASU; D. Sheikh, FSU; P. Carpenter, WUSL; H. Chennaoui Aoudjehane, FSAC; M. Zolensky, JSC; P. Schmitt-Kopplin, HZM) Carbonaceous chondrite (C2-ungrouped). The bulk mineralogy is consistent with a petrologic grade 2, based on the predominance of smectite and serpentine together with the presence of anhydrous mafic silicates, AOA, and chondrules. The oxygen isotopes give a bimodal distribution of the δ18O-values, with one group having values somewhat like those of the CI chondrites, and the other group like values for the Yamato-type (CY) carbonaceous chondrites (King et al., 2019). However, Δ17O values are lower than those for CI and CY chondrites, and plot below the TFL. These isotopic values do not overlap with those of any established carbonaceous chondrite group, hence the ungrouped designation.

Specimens : 18.4 g including one polished thin section and one polished thick section at UWB; 21g and one polished thin section at UNM; 7 g provided by A. Aaronson and 6 g provided by J. Redelsperger at FSAC; 20 g at the Ministry of Energy, Mines and Environment, Rabat, Morocco provided by A. Aaronson; total 628 g with A. Aaronson (including 99 g, 82.4 g and 52.6 g stones); 540 g with M. Farmer and A. Karl, 260 g with J. Poblador; 480 g with D. Dickens; 145 g with M. Oulkouch; 146 g with J. Redelsperger; 31 g with B. Hoefnagels.

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Sudbury Impactite #10 – 5,1 g

15,46 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
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Sudbury Impactite #9 – 3,3 g

14,27 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
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Sudbury Impactite #8 – 8,6 g

33,29 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
Add to cart

Sudbury Impactite #7 – 10,2 g

35,68 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
Add to cart
Out of stock

Sudbury Impactite #6 – 18,9 g

58,26 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
Details

Sudbury Impactite #5 – 20,8 g

63,02 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
Add to cart
Out of stock

Sudbury Impactite #4 – 18,6 g

61,82 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
Details
Out of stock

Sudbury Impactite #3 – 14,7 g

59,45 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
Details

Sudbury Impactite #2 – 48,4 g

108,20 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
Add to cart
Out of stock

Sudbury Impactite #1 – 95 g

197,38 $
The Sudbury Basin is an enormous structure 62 km long, 32 km wide and 15 km deep. This basin was formed after the impact of a meteorite, certainly a comet of about 10 to 15 km in diameter, 1.849 billion years ago.
It is the 2nd largest impact in the world.
The very important mining development in the area is directly related to this event.
Details
Out of stock

NWA 15169 Lunaire #13 – 2,6

255,64 $

NWA 15169 is a lunar meteorite discovered in 2021 in Morocco near Dakhla in the Wad Oum Sfia area by Omar Ben Chaoud and Mouloud Oudinat.

NWA 15169 is a rare lunar meteorite (anorthosite).

This is a very nice and colorful lunar meteorite offered at a very good price.

About fifteen years ago, lunar meteorites were sold for almost 1000 euros per gram !

Writeup from MB 112:

Northwest Africa 15169 (NWA 15169)

Morocco

Purchased: 2021

Classification: Lunar meteorite (anorth)

History: Found by Omar Ben Chaoud and Mouloud Oudinat in the Dakhla, Wad Oum Sfia area. Later bought by Jean Redelsperger from Mohamed Elguirah in 2021.

Physical characteristics: Several stones: a complete 50 g crusted stone, and several gray fragments without fusion crust, the largest one being 52 g.

Petrography: (J. Gattacceca, B. Devouard, CEREGE) Brecciated igneous rock composed primarily of anorthitic plagioclase, and mm-sized poikilitic microgabbroic clasts with plagioclase chadacrysts set in olivine and pyroxene. Accessory minerals: metal, ulvöspinel, chromite. Barite, from terrestrial weathering, is present as veins.

Geochemistry: Plagioclase An93.4±2.7Ab6.3±2.5Or0.2±0.2 (n=4). Olivine (altered) Fo 43.5±5.9, FeO/MnO=143.4, analytical totals 90.9±2.2 (n=9). Orthopyroxene Fs26.0Wo9.0, Fs16.3Wo36.9, FeO/MnO = 50.8 (n=2). Chromite Cr#=0.73 (n=1).

Classification: Lunar (anorthosite). Contains microgabbroic clasts. Olivine, pigeonite and plagioclase are within the ferroan anorthositic suite (FAS) field defined by Warren (1993). Olivine has been altered on Earth, as indicated by the low analytical totals.

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

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NWA 15169 Lunaire #12 – 1,7

167,65 $

NWA 15169 is a lunar meteorite discovered in 2021 in Morocco near Dakhla in the Wad Oum Sfia area by Omar Ben Chaoud and Mouloud Oudinat.

NWA 15169 is a rare lunar meteorite (anorthosite).

This is a very nice and colorful lunar meteorite offered at a very good price.

About fifteen years ago, lunar meteorites were sold for almost 1000 euros per gram !

Writeup from MB 112:

Northwest Africa 15169 (NWA 15169)

Morocco

Purchased: 2021

Classification: Lunar meteorite (anorth)

History: Found by Omar Ben Chaoud and Mouloud Oudinat in the Dakhla, Wad Oum Sfia area. Later bought by Jean Redelsperger from Mohamed Elguirah in 2021.

Physical characteristics: Several stones: a complete 50 g crusted stone, and several gray fragments without fusion crust, the largest one being 52 g.

Petrography: (J. Gattacceca, B. Devouard, CEREGE) Brecciated igneous rock composed primarily of anorthitic plagioclase, and mm-sized poikilitic microgabbroic clasts with plagioclase chadacrysts set in olivine and pyroxene. Accessory minerals: metal, ulvöspinel, chromite. Barite, from terrestrial weathering, is present as veins.

Geochemistry: Plagioclase An93.4±2.7Ab6.3±2.5Or0.2±0.2 (n=4). Olivine (altered) Fo 43.5±5.9, FeO/MnO=143.4, analytical totals 90.9±2.2 (n=9). Orthopyroxene Fs26.0Wo9.0, Fs16.3Wo36.9, FeO/MnO = 50.8 (n=2). Chromite Cr#=0.73 (n=1).

Classification: Lunar (anorthosite). Contains microgabbroic clasts. Olivine, pigeonite and plagioclase are within the ferroan anorthositic suite (FAS) field defined by Warren (1993). Olivine has been altered on Earth, as indicated by the low analytical totals.

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

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NWA 15169 Lunaire #11 – 3 g

296,06 $

NWA 15169 is a lunar meteorite discovered in 2021 in Morocco near Dakhla in the Wad Oum Sfia area by Omar Ben Chaoud and Mouloud Oudinat.

NWA 15169 is a rare lunar meteorite (anorthosite).

This is a very nice and colorful lunar meteorite offered at a very good price.

About fifteen years ago, lunar meteorites were sold for almost 1000 euros per gram !

Writeup from MB 112:

Northwest Africa 15169 (NWA 15169)

Morocco

Purchased: 2021

Classification: Lunar meteorite (anorth)

History: Found by Omar Ben Chaoud and Mouloud Oudinat in the Dakhla, Wad Oum Sfia area. Later bought by Jean Redelsperger from Mohamed Elguirah in 2021.

Physical characteristics: Several stones: a complete 50 g crusted stone, and several gray fragments without fusion crust, the largest one being 52 g.

Petrography: (J. Gattacceca, B. Devouard, CEREGE) Brecciated igneous rock composed primarily of anorthitic plagioclase, and mm-sized poikilitic microgabbroic clasts with plagioclase chadacrysts set in olivine and pyroxene. Accessory minerals: metal, ulvöspinel, chromite. Barite, from terrestrial weathering, is present as veins.

Geochemistry: Plagioclase An93.4±2.7Ab6.3±2.5Or0.2±0.2 (n=4). Olivine (altered) Fo 43.5±5.9, FeO/MnO=143.4, analytical totals 90.9±2.2 (n=9). Orthopyroxene Fs26.0Wo9.0, Fs16.3Wo36.9, FeO/MnO = 50.8 (n=2). Chromite Cr#=0.73 (n=1).

Classification: Lunar (anorthosite). Contains microgabbroic clasts. Olivine, pigeonite and plagioclase are within the ferroan anorthositic suite (FAS) field defined by Warren (1993). Olivine has been altered on Earth, as indicated by the low analytical totals.

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

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