Newsletter |
38,2 |
Location |
Larkman Nunatak |
Field Number |
23131 |
Dimensions (cm) |
3.1 x 2.7 x 1.2 |
Weight (g) |
20.07 |
Original Classification |
LL3.8 Chondrite |
Fayalite (mol%): 4-27;Ferrosilite (mol%): 19 |
B/C |
A/B |
The exterior is covered with 80% black fusion crust. Some areas are weathered brown with visible chondrules. The interior is heavily weathered with some dark gray to black matrix visible. The visible chondrules/inclusions are weathered. |
The section exhibits numerous well-defined chondrules (up to 1 mm) in a matrix of fine-grained silicates, metal and troilite. Polysynthetically twinned pyroxene is abundant. The meteorite is modestly stained with hydrated iron oxides of terrestrial origin. Silicates are unequilibrated; olivines range from Fa4-27 and a pyroxene is Fs19. The meteorite is an LL3 chondrite (estimated subtype 3.8). |