Research Paper THEMED ISSUE: Different Personalities of Granites and Rhyolites: Silicic Magmas from the Lower Crust to the Surface GEOSPHERE Feldspar recycling across magma mush bodies during the voluminous Half Dome and Cathedral Peak stages of the Tuolumne GEOSPHERE, v. 17, no. 2 intrusive complex, Yosemite National Park, California, USA https://doi.org/10.1130/GES02286.1 Louis F. Oppenheim1, Valbone Memeti1, Calvin G. Barnes2, Melissa Chambers1, Joachim Krause3, and Rosario Esposito4 13 figures; 3 tables; 1 set of supplemental files 1Department of Geological Sciences, California State University, Fullerton, California 92831, USA 2Department of Geosciences, Texas Tech University, Lubbock, Texas 07409-1053, USA 3 CORRESPONDENCE:
[email protected] Helmholtz-Zentrum Dresden-Rossendorf, Helmholtz Institute Freiberg for Resource Technology, Chemnitzer Straße 40, 09599 Freiberg, Germany 4Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, California 90095-1567, USA CITATION: Oppenheim, L.F., Memeti, V., Barnes, C.G., Chambers, M., Krause, J., and Esposito, R., 2021, Feldspar recycling across magma mush bodies during ABSTRACT ■ INTRODUCTION the voluminous Half Dome and Cathedral Peak stages of the Tuolumne intrusive complex, Yosemite National Park, California, USA: Geosphere, v. 17, no. 2, p. 322– Incremental pluton growth can produce sheeted complexes with no The concept that plutons are incrementally grown and can crystallize over 351, https:// doi.org /10.1130 /GES02286.1. magma-magma interaction or large, dynamic magma bodies communicat- several millions of years is widely accepted (e.g., Miller and Paterson, 2001; ing via crystal and melt exchanges, depending on pulse size and frequency Coleman et al., 2004; Glazner et al., 2004; Matzel et al., 2006; Lipman, 2007; Science Editor: Shanaka de Silva of intrusions.