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The Formation of Chondrules: Petrologic Tests of the Shock Wave Model

The Formation of Chondrules: Petrologic Tests of the Shock Wave Model

Connolly, H. C. Jr.; Love, S. G.
URI: http://hdl.handle.net/2014/18995
Date: 1998-01
Citation: Science
USA

Abstract:

Chondrules are mm-sized spheroidal igneous components of chondritic meteorites. They consist of olivine and orthopyroxene set in a glassy mesostasis with varying minor amounts of metals, sulfieds, oxides and carbon phases.

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