Beranek et al. (2024) - American Journal of Science supplementary materials

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.贫岩浆型劳伦大陆东缘形成于多期裂谷作用，其演化以埃迪卡拉纪（Ediacaran）至寒武纪（Cambrian）裂解层序的沉积为顶峰，该层序形成于地壳与地幔破裂事件过程中。本次随附文件为Soukup等人2024年发表于《美国科学杂志》（American Journal of Science）的研究补充材料，包含碎屑锆石（detrital zircon）U-Pb-Hf同位素数据表、SEM-MLA（砂岩矿物学）分析表以及采样点野外照片。