Figure 2 was originally published with an error in the lower positioning of the boundary line between “Transitional Arc” and “Undissected Arc” in the paper that appeared in the Journal of Sedimentary Research, v. 81, no. 9, September 2011, on pages 702–707. It is reproduced here with the correct configuration.

In the “Chart Description” of page 703, the 3rd sentence of that paragraph is rewritten here to better represent the nomenclatures that were used in this paper for constructing provenance diagrams based on Dickinson (1985).

The program utilizes major sandstone framework grains, including monocrystalline quartz (Qm), polycrystalline quartz (Qp) and...

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