Like many other Martian basalts in the world’s meteorite collections, it probably formed as a basalt flow at or near the surface of Mars. The unusual “poikilitic” texture of this rock is marked by large crystals of pyroxene (a magnesium-iron silicate) enclosing small crystals of olivine (a magnesium-iron silicate) and chromite (an iron-chromium oxide). The texture most likely formed by rapid cooling of the rock from magmatic temperatures. The feldspar mineral grains (a calcium-aluminum silicate) have been transformed into glass, a mark of the intense shock pressure experienced by the rock when it was blasted off the surface of Mars by an enormously energetic impact event.
Generally in very good condition with very light scratches and marks from cutting process not effecting overall appearance. Please note that weights and dimensions are approximate only and that the appearance and surfaces of meteorites can change with atmospheric conditions. Specifically moisture can be lightly corrosive and accelerate the natural patination of the surface.
預計金額計算機
拍品 12拍賣 10887
DISCOVERED IN SMARA, MOROCCO, 2012A Complete Meteorite from the Planet Mars (NWA 7397)估價: USD 35,000 - 55,000