Abstract
Partial syntectonic recrystallization has been produced in an experimentally deformed plagioclase (peristerite An4.5). The recrystallized grains are scattered through the strongly deformed matrix and appear to have developed by a nucleation and growth mechanism.
Original language | English |
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Pages (from-to) | 49-54 |
Number of pages | 6 |
Journal | Contributions to Mineralogy and Petrology |
Volume | 57 |
Issue number | 1 |
DOIs | |
Publication status | Published - Mar 1976 |