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Condensation Experiments of Mg-Silicate Minerals
Published online by Cambridge University Press: 12 April 2016
Abstract
Condensation experiments were performed in the simple but most fundamental system Mg-Si-O-H with forsterite vaporization source. At temperatures above about 1000°C, euhedral crystals of forsterite (Mg2SiO4) of a few μm were formed. These crystals are similar to olivines in Allende matrix. At temperatures below about 1000°C, whiskers of forsterite and enstatite (MgSiO3) were formed by vapor-liquid-solid growth mechanism. These whiskers are different from enstatite whiskers in interplanetary dust, which were probably formed at small super coolings.
- Type
- Interplanetary Dust: Physical and Chemical Analysis
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- Copyright © Kluwer 1991