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Along-strike variations in sediment provenance within the Nanaimo basin reveal mechanisms of forearc basin sediment influx events
2020
Lithosphere
The along-strike variability in sediment provenance within the Nanaimo basin is important for understanding the tectonic evolution of North America's Late Cretaceous Pacific margin, providing context for paleogeographic reconstructions. Here, we provide 35 point-counted sandstone samples and 22 new detrital zircon samples from the Nanaimo basin. These new detrital zircon samples compose a portion of a basin-wide data set (N = 49, n = 10,942) that is leveraged to discern spatio-temporal changes
doi:10.1130/l1138.1
fatcat:m7r2c37hlfdyjmnw5gxjvw5olu