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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| Format: | Others |
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DigitalCommons@USU
2011
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| Online Access: | https://digitalcommons.usu.edu/etd/1117 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=2120&context=etd |