Zuñi sequence
A Jurassic-Cretaceous cratonic sequence / From Wikipedia, the free encyclopedia
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The Zuñi sequence was the major cratonic sequence after the Absaroka sequence that began in the latest Jurassic, peaked in the late Cretaceous, and ended by the start of the following Paleocene.[1] Though it was not the final major transgression, it was the last complete sequence to cover the North American craton; the following Tejas sequence was much less extensive.