Abstract

La Virgen tephra is the product of the youngest and most voluminous explosive eruption of Las Tres Vírgenes volcano (Baja California). Combined U–Th and (U–Th)/He zircon dating allows accurate correction for uranium-series disequilibrium, and yields an eruption age for La Virgen tephra of 30.7 − 1.4 + 1.8 ka (2 σ). No difference in eruption ages was found between samples from proximal and distal La Virgen tephra. A previously undated tephra south of Las Tres Vírgenes volcano yielded U–Th and (U–Th)/He zircon ages overlapping those of La Virgen tephra, which suggests that both units are identical. 3He surface exposure ages ( T 3) of overlying mafic lavas are 25.5 ± 4.4 and 22.0 ± 2.5 ka, and agree within uncertainties with 21Ne exposure ages ( T 21). T 3 and T 21 ages for dome lava south of La Virgen are slightly older ( T 3 = 42.5 ± 3.8 ka). (U–Th)/He and surface exposure ages are stratigraphically consistent, whereas a published Holocene 14C charcoal age from the distal site could not be confirmed. Instead, abundant zircon crystals with (U–Th)/He ages between ∼1 and 22 Ma are interpreted as undegassed detrital grains, suggesting reworking of pumice at the distal location. The results presented here underscore the potential of combined U–Th and (U–Th)/He zircon dating for Quaternary tephrochronology.

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