Petrology of Passive Margin-Epeiric Sea Sediments: the Garden City Formation, North-central Utah
The Lower Ordovician Garden City Formation is part of the thick sequence of Lower Paleozoic limestones, dolostones, and minor siliciclastic sedimentary rocks of the western United States. The carbonate rocks were formed predominantly by shallow water deposition in tropical, passive-margin epeiric se...
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| Format: | Others |
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DigitalCommons@USU
1988
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| Online Access: | https://digitalcommons.usu.edu/etd/5623 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=6680&context=etd |