Far-Travelled High-Grade Ignimbrites or Widespread Generation of Low-d18O Magma? The Problem of the West Bennett Hills, Snake River Plain, ID (original) (raw)

Abstract

The West Bennett Hills (WBH), on the north side of the Snake River Plain (SRP) of southern Idaho, consist of a sequence of rhyolitic volcanic units known to share similar ages and chemistry with upper units of the Cougar Point Tuff (CPT), a series of high-grade ignimbrites associated with the Bruneau-Jarbidge (BJ) eruptive center 120 km south of WBH. The

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