The Interrelationship Between the Bio- and Sequence Stratigraphy of the Middle Cambrian Spence Shale of Northern Utah and Southern Idaho

The Middle Cambrian Spence Shale Member of the Langston Formation of northern Utah and southern Idaho is a fossil-rich unit that exhibits distinct cyclicity at the parasequence (meter) scale. At least seven discrete, shallowing-upwards parasequences, or cycles, can be found at the Miners Hollow and...

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Bibliographic Details
Main Author: Lyon, Eva
Format: Others
Published: DigitalCommons@USU 2011
Subjects:
Online Access:https://digitalcommons.usu.edu/etd/1117
https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=2120&context=etd