Abstract:Irregular, branching, white-fragment breccia dikes are restricted to the uppermost flows of the Amulet formation, where they occur within or are parallel to synvolcanic faults. At Buttercup Hill, the breccia dikes bifurcate upward and are continuous with a localized deposit of identical, conformable breccia within the lowermost andesitic flows of the Millenbach andesite formation. The dikes are shallow, poorly sorted intrusive breccias and like the overlying, conformable breccia deposit are characterized by wh… Show more
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