Fig. 3: Sediment-accumulation rates and subsidence-uplift histories of the Coastal Range.
From: Extremely rapid up-and-down motions of island arc crust during arc-continent collision
a Stratigraphic age models for the Coastal Range. b, c Geohistory curves of the northern and southern Coastal Range. Symbols and color-fill style follow Fig. 3a. Asterisk in each curve is the reconstructed depth using youngest sediment eroded from top of section. Error bars represent one standard error of the mean. See details of data and calculation results in Supplementary Data 4.
