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Long Valley Caldera
Geolocalization of Large‐Scale DAS Channels Using a GPS‐Tracked Moving Vehicle
A low-aluminum clinopyroxene-liquid geothermometer for high-silica magmatic systems
Seismic evidence for significant melt beneath the Long Valley Caldera, California, USA
Seismically anisotropic magma reservoirs underlying silicic calderas
Ascent rates of rhyolitic magma at the onset of three caldera-forming eruptions
Graphite in the Bishop Tuff and its effect on postcaldera oxygen fugacity
Evenly spaced columns in the Bishop Tuff (California, USA) as relicts of hydrothermal cooling
On the Use of Data Noise as a Site‐Specific Weight Parameter in a Hierarchical Bayesian Moment Tensor Inversion: The Case Study of The Geysers and Long Valley Caldera Earthquakes
PERSPECTIVE
Northern California Seismic Attenuation: 3D Q P and Q S Models
Co-Evolution of Volcanic and Lacustrine Systems In Pleistocene Long Valley Caldera, California, U.S.A.
Zircon saturation and Zr diffusion in rhyolitic melts, and zircon growth geospeedometer
The Life and Times of Silicic Volcanic Systems
In defense of magnetite-ilmenite thermometry in the Bishop Tuff and its implication for gradients in silicic magma reservoirs
Long Valley Caldera and the UCERF Depiction of Sierra Nevada Range-Front Faults
Timescales of crustal magma reservoir processes: insights from U-series crystal ages
Abstract The dynamic processes operating within crustal magma reservoirs control many aspects of the chemical composition of erupted magmas, and crystals in volcanic rocks provide a temporally constrained archive of these changing environments. In this review, I compile 238 U– 230 Th ages of accessory phases and 238 U– 230 Th– 226 Ra ages of bulk mineral separates of major phases. These data document that crystals in individual samples can have ages spanning most of the history of a volcanic centre. Age populations for accessory phases show protracted pre-eruptive crystal residence times but few crystals predate magmatic activity at a given centre. These data have been interpreted in the context of residence times of the host magmas or timescales of the storage of crystals within a largely crystalline portion of the reservoir system. In contrast, less than half of the bulk separate 238 U– 230 Th– 226 Ra ages for major phases are more than 10 kyr older than the eruption. Many of these apparently conflicting observations of ages of major and accessory phases can be reconciled within the context of a model where a crystal mush was remobilized during processes leading to eruption. Overall, the compiled data show that crystals contain rich archives of magmatic processes in crustal reservoirs, especially when combined with other crystal-scale geochemical data. Supplementary material: Compilation of U–Th–Pb ages of accessory phases and associated references are available at www.geolsoc.org.uk/SUP18820