The 80km long NNE-trending Rogerson Graben on the southern margin of the central Snake River Plain, Idaho, USA, hosts a rhyolitic
pyroclastic succession, 200m thick, that records a period of successive, late-Miocene, large-volume explosive eruptions from
the Yellowstone–Snake River Plain volcanic province, and contemporaneous extension. The succession, here termed the Rogerson
Formation,
... [Show full abstract] comprises seven members (defined herein) and records at least eight large explosive eruptions with numerous repose
periods. Five high-grade and extremely high-grade ignimbrites are intercalated with three non-welded ignimbrites and two volcaniclastic
deposits, with numerous repose periods (palaeosols) throughout. Two of the ignimbrites are dominantly rheomorphic and lava-like
but contain subordinate non-welded pyroclastic layers. The ignimbrites are typical Snake River Plain high-silica rhyolites,
with anhydrous crystal assemblages and high inferred magmatic temperatures (≤ 1,025°C). We tentatively infer that the Jackpot
and Rabbit Springs Members may have been emplaced from the Bruneau–Jarbidge eruptive centre on the basis of: (1) flow lineation
trends, (2) crystal assemblage, and (3) radiometric age. We infer that the overlying Brown’s View, Grey’s Landing, and Sand
Springs Members may have been emplaced from the Twin Falls eruptive centre on the basis of: (1) kinematic indicators (from
the east), and (2) crystal assemblage. Furthermore, we have established the contemporaneous evolution of the Rogerson Graben
from the emplacement of the Jackpot Member onwards, and infer that it is similar to younger half-graben along the southern
margin of the Snake River Plain, formed by local reactivation of Basin and Range structures by the northeastwardly migration
of the Yellowstone hot-spot.