Journal
EARTH AND PLANETARY SCIENCE LETTERS
Volume 175, Issue 3-4, Pages 289-296Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/S0012-821X(99)00299-X
Keywords
plagioclase; shock metamorphism; mobilization; shergottite; experimental studies
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Shock recovery experiments of plagioclase feldspar in contact with pyroxene, shock-loaded at 36-53 GPa, showed that monomineralic glass of plagioclase was mixed with brecciated pyroxenes with virtual absence of mixed-mineral melts. This amorphous phase of plagioclase produced at 36-42 GPa displays enormously high ductility although the amorphous phase is less likely to be a quenched high-pressure melt because both shock and post-shock bulk temperature cannot exceed the melting point. The results suggest that alkaline components in feldspar can be extensively mobilized even in a very short duration of shock, which can never be achieved by normal diffusion in the same time scale. Since feldspar is a major carrier phase of alkaline volatiles. shock mobilization mechanism may explain shock disturbance of Rb-Sr and Ar-39-Ar-40 ages of basaltic shergottites. (C) 2000 Elsevier Science B.V. All rights reserved.
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