Abstract
The South Mountains of central Arizona are one of the geologically simplest metamorphic core complexes of the N American Cordillera. An early Miocene age of mylonitization is indicated by crosscutting relationships between mylonitic fabroc and a composite pluton dated at 22-25 Ma by Rb-Sr, U-Th-Pb, and K-Ar techniques. The kinematic agreement and close temporal association of mylonitization and detachment faulting support models in which the 2 processes are related to an evolving crustal shear zone that accommodated mid-Tertiary continental extension. -Authors
Original language | English (US) |
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Pages (from-to) | 283-286 |
Number of pages | 4 |
Journal | Geology |
Volume | 14 |
Issue number | 4 |
DOIs | |
State | Published - 1986 |
ASJC Scopus subject areas
- Geology