On the rise: using reentrants to extract magma ascent rates in the Bandelier Tuff caldera complex, New Mexico, USA

Author:

Saalfeld Megan A.,Myers M. L.,deGraffenried R.,Shea T.,Waelkens C. M.

Funder

national science foundation

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference70 articles.

1. Aldrich M Jr (1986) Tectonics of the Jemez lineament in the Jemez Mountains and Rio Grande rift. J Geophys Res Solid Earth 91:1753–1762

2. Audétat A (2013) Origin of Ti-rich rims in quartz phenocrysts from the Upper Bandelier Tuff and the Tunnel Spring Tuff, southwestern USA. Chem Geol 360:99–104

3. Boehnke P, Watson EB, Trail D, Harrison TM, Schmitt AK (2013) Zircon saturation re-revisited. Chem Geol 351:324–334

4. Boro JR (2019) Recharge and mobilization of crystal mush to produce and erupt a zoned magma chamber–the Tshirege Member of the Bandelier Tuff. Valles Caldera, New Mexico

5. Boro JR, Wolff JA, Neill OK (2020) Anatomy of a recharge magma: Hornblende Dacite Pumice from the rhyolitic Tshirege Member of the Bandelier Tuff. Valles Caldera, New Mexico, USA: Contributions to Mineralogy and Petrology 175:1–26

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