[meteorite-list] Olivine with Spinel Structure in Meteorites
From: Sara Russell <sarr_at_meteoritecentral.com>
Date: Thu Apr 22 09:46:22 2004 Message-ID: <E14wkO4-0001M4-00_at_pat.nhm.ac.uk> Dear Elton and list Although ringwoodite requires high pressures to form, its presence does not necessarily indicate it came from a big parent body. On Earth, it is predicted to exist because of the high pressures caused by the large mass of Earth. However in meteorites, ringwoodite forms by a different mechanism- it is always associated with shock features, and so it is thought to form in the high pressures experienced by a collision between two asteroids- a big parent body is not required, only very high collisional velocities. Also, while perovskite is often associated with high pressure mineralogy in many terrestrial samples, in meteorites perovskite is most abundant in calcium-aluminium-rich inclusions, and is thought to form at very high temperatures, but low pressures, in the solar nebula. Its formation is not linked to ringwoodite. hope this helps Sara ************************************* Dr Sara Russell, Department of Mineralogy, The Natural History Museum, Cromwell Road, London, SW7 5BD, U.K. Tel: +44 (0) 20 7942 5074 Fax: +44 (0) 20 7942 5537 Received on Mon 07 May 2001 08:45:16 AM PDT |
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