[meteorite-list] iron meteorite cooling rates and Meteorite Men
From: Alan Rubin <aerubin_at_meteoritecentral.com>
Date: Wed, 15 Dec 2010 09:54:14 -0800 Message-ID: <D606A5ED835C49E18CC75DE451806AA9_at_igpp.ucla.edu> On last night's Meteorite Men show, the narrator was attempting to explain that the Widmanstatten pattern is caused by kamacite and taenite cooling at different rates. This is incorrect. How could two intergrown metal grains buried deep inside a core cool at different rates? The Widmanstatten pattern forms in the following manner: (1) At high temperatures (but below the solidus), metallic Fe-Ni exists as a single phase -- taenite. (2) As the metal cools, it eventually reaches the two-phase field (or solvus) on the phase diagram. For metal containing 90% iron and 10% nickel, it reaches this boundary when temperatures cool to about 700?C. (3) At this point, small kamacite grains nucleate inside the taenite. With continued cooling, the kamacite grains grow larger at the expense of taenite, but both phases become richer in nickel. This is possible because the low-Ni phase (kamacite) is becoming increasingly abundant. (4) At low temperatures, say <400?C or so, diffusion becomes so sluggish that the reaction essentially stops. These meteorites are called octohedrites because solids have three-dimensional structures and the kamacite planes are oriented with respect to each other in the same way as the faces of a regular octahedron. Alan Rubin Institute of Geophysics and Planetary Physics University of California 3845 Slichter Hall 603 Charles Young Dr. E Los Angeles, CA 90095-1567 phone: 310-825-3202 e-mail: aerubin at ucla.edu website: http://cosmochemists.igpp.ucla.edu/Rubin.html Received on Wed 15 Dec 2010 12:54:14 PM PST |
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