Beranek et al. (2024) - American Journal of Science supplementary materials
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The magma-poor, eastern Laurentian margin resulted from polyphase rifting, which culminated with the deposition of Ediacaran to Cambrian breakup sequences that formed in response to crust and mantle rupture events. The enclosed files are supplements to Soukup et al. (2024) in <i>American Journal of Science</i> and comprise detrital zircon U-Pb-Hf isotope and SEM-MLA (sandstone mineralogy) data tables and field photos of sample sites.
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figshare
创建时间：
2024-01-27
