Shock-Thermal Decomposition of Minerals as One of the Main Diagnostic Features of Shock Metamorphism

Details Shock-Thermal Decomposition of Minerals as One of the Main Diagnostic Features of Shock Metamorphism Shock-Thermal Decomposition of Minerals as One of the Main Diagnostic Features of Shock Metamorphism

Jan 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001sosyr..35...90f&link_type=abstract

Solar System Research, v. 35, Issue 1, p. 90-94 (2001).

Mathematics

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Scientific paper

The P-T conditions for the formation of polymineral secondary aggregates that arise during the passage of a shock wave through rock are considered on the basis of geological, petrographical, and experimental data. It is shown that these aggregates are formed along the isoentrope and represent a characteristic feature of the impact process. Their mineral composition is given, and the crystallochemical control of the process of their formation is established.

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