Clinoenstatite in alpe arami peridotite: additional evidence of very high pressure

Abstract

Observations by transmission electron microscopy show that lamellae of clinoenstatite are present in diopside grains of the Alpe Arami garnet lherzolite of the Swiss Alps. The simplest interpretation of the orientation, crystallography, and microstructures of the lamellae and the phase relationships in this system is that the lamellae originally exsolved as… (More)

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Cite this paper

@article{Bozhilov1999ClinoenstatiteIA, title={Clinoenstatite in alpe arami peridotite: additional evidence of very high pressure }, author={Bozhilov and K R Green and Dobrzhinetskaya}, journal={Science}, year={1999}, volume={284 5411}, pages={128-32} }