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Chwichiya 004 LL7 #8 – 3,9 g

41,62 $

This meteorite was discovered in the mythical Chwichiya concentration area in the Western Sahara.

Chwichiya 004 27°23’42.89 “N, 11°42’12.82 “W

Saguia el Hamra, Sahara occidental

Discovery date : April 24, 2019

Classification : Ordinary chondrite (LL7)

History : found by Hammo Oualguirah on April 24, 2019. Purchased from Mohamed Elguirah by Jean Redelsperger.

Physical characteristics : Several grayish stones, without fusion crust.

Petrography : (J. Gattacceca, CEREGE) Recrystallized chondrite. No relict chondrules observed. Olivine (up to 200 µm) has lobed contours. Plagioclase of typical size 100 µm.

Geochemistry: Olivine Fa30.0 (n=2). Low Ca pyroxene Fs24.8±0.0Wo3.2±0.2 (n=3).

Classification : Ordinary chondrite (LL7). Type 7 based on texture and Wo content of low-Ca pyroxene.

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

 

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Chwichiya 004 LL7 #7 – 3 g

32,10 $

This meteorite was discovered in the mythical Chwichiya concentration area in the Western Sahara.

Chwichiya 004 27°23’42.89 “N, 11°42’12.82 “W

Saguia el Hamra, Sahara occidental

Discovery date : April 24, 2019

Classification : Ordinary chondrite (LL7)

History : found by Hammo Oualguirah on April 24, 2019. Purchased from Mohamed Elguirah by Jean Redelsperger.

Physical characteristics : Several grayish stones, without fusion crust.

Petrography : (J. Gattacceca, CEREGE) Recrystallized chondrite. No relict chondrules observed. Olivine (up to 200 µm) has lobed contours. Plagioclase of typical size 100 µm.

Geochemistry: Olivine Fa30.0 (n=2). Low Ca pyroxene Fs24.8±0.0Wo3.2±0.2 (n=3).

Classification : Ordinary chondrite (LL7). Type 7 based on texture and Wo content of low-Ca pyroxene.

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

 

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Chwichiya 004 LL7 #6 – 2,6 g

27,35 $

This meteorite was discovered in the mythical Chwichiya concentration area in the Western Sahara.

Chwichiya 004 27°23’42.89 “N, 11°42’12.82 “W

Saguia el Hamra, Sahara occidental

Discovery date : April 24, 2019

Classification : Ordinary chondrite (LL7)

History : found by Hammo Oualguirah on April 24, 2019. Purchased from Mohamed Elguirah by Jean Redelsperger.

Physical characteristics : Several grayish stones, without fusion crust.

Petrography : (J. Gattacceca, CEREGE) Recrystallized chondrite. No relict chondrules observed. Olivine (up to 200 µm) has lobed contours. Plagioclase of typical size 100 µm.

Geochemistry: Olivine Fa30.0 (n=2). Low Ca pyroxene Fs24.8±0.0Wo3.2±0.2 (n=3).

Classification : Ordinary chondrite (LL7). Type 7 based on texture and Wo content of low-Ca pyroxene.

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

 

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Chwichiya 004 LL7 #5 – 4 g

42,80 $

This meteorite was discovered in the mythical Chwichiya concentration area in the Western Sahara.

Chwichiya 004 27°23’42.89 “N, 11°42’12.82 “W

Saguia el Hamra, Sahara occidental

Discovery date : April 24, 2019

Classification : Ordinary chondrite (LL7)

History : found by Hammo Oualguirah on April 24, 2019. Purchased from Mohamed Elguirah by Jean Redelsperger.

Physical characteristics : Several grayish stones, without fusion crust.

Petrography : (J. Gattacceca, CEREGE) Recrystallized chondrite. No relict chondrules observed. Olivine (up to 200 µm) has lobed contours. Plagioclase of typical size 100 µm.

Geochemistry: Olivine Fa30.0 (n=2). Low Ca pyroxene Fs24.8±0.0Wo3.2±0.2 (n=3).

Classification : Ordinary chondrite (LL7). Type 7 based on texture and Wo content of low-Ca pyroxene.

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

 

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Chwichiya 004 LL7 #4 – 7 g

74,90 $

This meteorite was discovered in the mythical Chwichiya concentration area in the Western Sahara.

Chwichiya 004 27°23’42.89 “N, 11°42’12.82 “W

Saguia el Hamra, Sahara occidental

Discovery date : April 24, 2019

Classification : Ordinary chondrite (LL7)

History : found by Hammo Oualguirah on April 24, 2019. Purchased from Mohamed Elguirah by Jean Redelsperger.

Physical characteristics : Several grayish stones, without fusion crust.

Petrography : (J. Gattacceca, CEREGE) Recrystallized chondrite. No relict chondrules observed. Olivine (up to 200 µm) has lobed contours. Plagioclase of typical size 100 µm.

Geochemistry: Olivine Fa30.0 (n=2). Low Ca pyroxene Fs24.8±0.0Wo3.2±0.2 (n=3).

Classification : Ordinary chondrite (LL7). Type 7 based on texture and Wo content of low-Ca pyroxene.

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

 

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Chwichiya 004 LL7 #3 – 2,9 g

30,91 $

This meteorite was discovered in the mythical Chwichiya concentration area in the Western Sahara.

Chwichiya 004 27°23’42.89 “N, 11°42’12.82 “W

Saguia el Hamra, Sahara occidental

Discovery date : April 24, 2019

Classification : Ordinary chondrite (LL7)

History : found by Hammo Oualguirah on April 24, 2019. Purchased from Mohamed Elguirah by Jean Redelsperger.

Physical characteristics : Several grayish stones, without fusion crust.

Petrography : (J. Gattacceca, CEREGE) Recrystallized chondrite. No relict chondrules observed. Olivine (up to 200 µm) has lobed contours. Plagioclase of typical size 100 µm.

Geochemistry: Olivine Fa30.0 (n=2). Low Ca pyroxene Fs24.8±0.0Wo3.2±0.2 (n=3).

Classification : Ordinary chondrite (LL7). Type 7 based on texture and Wo content of low-Ca pyroxene.

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

 

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Chwichiya 004 LL7 #2 – 6,2 g

66,59 $

This meteorite was discovered in the mythical Chwichiya concentration area in the Western Sahara.

Chwichiya 004 27°23’42.89 “N, 11°42’12.82 “W

Saguia el Hamra, Sahara occidental

Discovery date : April 24, 2019

Classification : Ordinary chondrite (LL7)

History : found by Hammo Oualguirah on April 24, 2019. Purchased from Mohamed Elguirah by Jean Redelsperger.

Physical characteristics : Several grayish stones, without fusion crust.

Petrography : (J. Gattacceca, CEREGE) Recrystallized chondrite. No relict chondrules observed. Olivine (up to 200 µm) has lobed contours. Plagioclase of typical size 100 µm.

Geochemistry: Olivine Fa30.0 (n=2). Low Ca pyroxene Fs24.8±0.0Wo3.2±0.2 (n=3).

Classification : Ordinary chondrite (LL7). Type 7 based on texture and Wo content of low-Ca pyroxene.

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

 

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NWA 14820 L6 #3 – 11 g

26,16 $

NWA 14820 is a meteorite of 1260 grams discovered in Mauritania in 2021.

This meteorite has been classified chondrite type L6 by Jérôme Gattacceca scientist at Cerege in Aix-en-Provence.

It’s a piece with a nice patina.

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NWA 14820 L6 #2 – 41 g

83,23 $

NWA 14820 is a meteorite of 1260 grams discovered in Mauritania in 2021.

This meteorite has been classified chondrite type L6 by Jérôme Gattacceca scientist at Cerege in Aix-en-Provence.

It’s a piece with a nice patina.

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TARDA C2 Ung #26 – 0,13 g

59,45 $

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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TARDA C2 Ung #25 – 0,28 g

116,52 $

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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TARDA C2 Ung #24 – 0,5 g

214,02 $

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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TARDA C2 Ung #23 – 0,5 g

208,08 $

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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TARDA C2 Ung #22 – 1,6 g

582,62 $

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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Zagora 003 Eucrite #13 – 1,3 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.

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Zagora 003 Eucrite #12 – 3,1 g

45,18 $

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.

Details
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Zagora 003 Eucrite #11 – 2,8 g

40,43 $

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.

Details

Zagora 003 Eucrite #10 – 5,2 g

76,09 $

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.

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