NWA 15170 is a lodranite meteorite of only 89 grams.
The lodranites are a type of meteorites forming a group within the primitive achondrites.
The reference fall is the Lodran meteorite that fell in 1868 in Pakistan..
These rare meteorites are composed for a large part of orthopyroxene (45 to 55 %), of magnesian olivine (40 %), of Fe-Ni alloy, of troilite, of clinopyroxene, of daubreelite, schreibersite, chromite and, accessorily, feldspars plagioclase and orthoclase, alabandite, graphite and apatite.
NWA 15170 is a lodranite meteorite of only 89 grams.
The lodranites are a type of meteorites forming a group within the primitive achondrites.
The reference fall is the Lodran meteorite that fell in 1868 in Pakistan..
These rare meteorites are composed for a large part of orthopyroxene (45 to 55 %), of magnesian olivine (40 %), of Fe-Ni alloy, of troilite, of clinopyroxene, of daubreelite, schreibersite, chromite and, accessorily, feldspars plagioclase and orthoclase, alabandite, graphite and apatite.
NWA 15170 is a lodranite meteorite of only 89 grams.
The lodranites are a type of meteorites forming a group within the primitive achondrites.
The reference fall is the Lodran meteorite that fell in 1868 in Pakistan..
These rare meteorites are composed for a large part of orthopyroxene (45 to 55 %), of magnesian olivine (40 %), of Fe-Ni alloy, of troilite, of clinopyroxene, of daubreelite, schreibersite, chromite and, accessorily, feldspars plagioclase and orthoclase, alabandite, graphite and apatite.
NWA 14809 is a carbonaceous meteorite of type CK5 of only 31 grams.
The reference fall is the Karoonda meteorite that fell in 1930 in Australia.
Writeup from MB 111 :
Northwest Africa 14809 (NWA 14809)
Algeria
Purchased: 2021
Classification: Carbonaceous chondrite (CK5)
History: Found in Algeria. Bought by Jean Redelsperger from Mohamed Elguirah in 2021.
Physical characteristics: Dark fragments.
Petrography: (J. Gattacceca, CEREGE) Chondrule with average apparent diameter about 800 µm set in a recrystallized matrix (grain size 15 µm). Olivine is the dominant mineral. Magnetite and sulfide are abundant in the matrix and chondrules, sometimes as composite spherical grains up to 200 µm.
NWA 14809 is a carbonaceous meteorite of type CK5 of only 31 grams.
The reference fall is the Karoonda meteorite that fell in 1930 in Australia.
Writeup from MB 111 :
Northwest Africa 14809 (NWA 14809)
Algeria
Purchased: 2021
Classification: Carbonaceous chondrite (CK5)
History: Found in Algeria. Bought by Jean Redelsperger from Mohamed Elguirah in 2021.
Physical characteristics: Dark fragments.
Petrography: (J. Gattacceca, CEREGE) Chondrule with average apparent diameter about 800 µm set in a recrystallized matrix (grain size 15 µm). Olivine is the dominant mineral. Magnetite and sulfide are abundant in the matrix and chondrules, sometimes as composite spherical grains up to 200 µm.
NWA 14809 is a carbonaceous meteorite of type CK5 of only 31 grams.
The reference fall is the Karoonda meteorite that fell in 1930 in Australia.
Writeup from MB 111 :
Northwest Africa 14809 (NWA 14809)
Algeria
Purchased: 2021
Classification: Carbonaceous chondrite (CK5)
History: Found in Algeria. Bought by Jean Redelsperger from Mohamed Elguirah in 2021.
Physical characteristics: Dark fragments.
Petrography: (J. Gattacceca, CEREGE) Chondrule with average apparent diameter about 800 µm set in a recrystallized matrix (grain size 15 µm). Olivine is the dominant mineral. Magnetite and sulfide are abundant in the matrix and chondrules, sometimes as composite spherical grains up to 200 µm.
NWA 14809 is a carbonaceous meteorite of type CK5 of only 31 grams.
The reference fall is the Karoonda meteorite that fell in 1930 in Australia.
Writeup from MB 111 :
Northwest Africa 14809 (NWA 14809)
Algeria
Purchased: 2021
Classification: Carbonaceous chondrite (CK5)
History: Found in Algeria. Bought by Jean Redelsperger from Mohamed Elguirah in 2021.
Physical characteristics: Dark fragments.
Petrography: (J. Gattacceca, CEREGE) Chondrule with average apparent diameter about 800 µm set in a recrystallized matrix (grain size 15 µm). Olivine is the dominant mineral. Magnetite and sulfide are abundant in the matrix and chondrules, sometimes as composite spherical grains up to 200 µm.
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