Spatio-temporal clustering of post-caldera eruptions at Yellowstone caldera: implications for volcanic hazards and pre-eruptive magma reservoir configuration
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
https://link.springer.com/content/pdf/10.1007/s00445-023-01665-w.pdf
Reference70 articles.
1. Andersen NL, Jicha BR, Singer BS, Hildreth W (2017) Incremental heating of Bishop Tuff sanidine reveals preeruptive radiogenic Ar and rapid remobilization from cold storage. Proc Natl Acad Sci. https://doi.org/10.1073/pnas.1709581114
2. Baag C, Helsley CE, Xu SZ, Lienert BR (1995) Deflection of paleomagnetic directions due to magnetization of the underlying terrain. J Geophys Res Solid Earth 100:10013–10027. https://doi.org/10.1029/95JB00148
3. Befus KS, Zinke RW, Jordan JS et al (2014) Pre-eruptive storage conditions and eruption dynamics of a small rhyolite dome: Douglas Knob, Yellowstone volcanic field, USA. Bull Volcanol 76:1–12. https://doi.org/10.1007/s00445-014-0808-8
4. Befus KS, Gardner JE (2016) Magma storage and evolution of the most recent effusive and explosive eruptions from Yellowstone Caldera. Contrib Mineral Petrol 171:30. https://doi.org/10.1007/s00410-016-1244-x
5. Bindeman IN, Valley JW (2001) Low-delta O-18 rhyolites from Yellowstone: magmatic evolution based on analyses of zircons and individual phenocrysts. J Petrol 42:1491–1517. https://doi.org/10.1093/petrology/42.8.1491
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