A major work by the author describing this regions" identified agate inclusions and their proposed geochemistry of formation.
Also includes additional study of the clays in the agates.
Key Features:
This book proposes and presents the data to support the model view that the Lake Superior agates formed in metamorphosed basalts in lava flow tops that were highly vesicular, around Cretaceous. At that time, substantial ash deposits of the Midwest from Western volcanism released silica that filled these voids (amygdules). Earlier clay deposits of illite dominant in the midwestern rock strata from Ordovician was also released by this local tectonic activity, introduced as inclusions of various types in the amygdules and in some vein agates. The geochemistry behind these and other inclusion reactions, and their correlation to regional geologic systems is described.
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