Fig. 8From: Natural and experimental high-pressure, shock-produced terrestrial and extraterrestrial materialsBF-TEM image of akimotoite (Aki) in the Tenham L6 ordinary chondrite. The akimotoite grains formed in a solid-state transformation from low-Ca pyroxene (clinoenstatite: Cen) with (100) twin lamellae in the host rock entrapped into a shock-melt veinBack to article page