First evidence of a “Barrovian”-type metamorphic regime in the Ross orogen of the Byrd Glacier area, central Transantarctic Mountains von Talarico, F.M., Stump, E., Gootee, B.F., Foland, K.A., Palmeri, R., Van Schmus, W.R., Brand, P.K., Ricci, C.A.

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Correlation of Byrd and Selborne Groups, with implications for the Byrd Glacier discontinuity, central Transantarctic Mountains, Antarctica von Stump, E., Gootee, B. F., Talarico, F., Van Schmus, W. R., Brand, P. K., Foland, K. A., Fanning, C. M.

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Evidence for the overflow origin of the Grand Canyon von Douglass, John C., Gootee, Brian F., Dallegge, Todd, Jeong, A., Seong, Y.B., Yu, B.Y.

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Tectonic Model for Development of the Byrd Glacier Discontinuity and Surrounding Regions of the Transantarctic Mountains during the Neoproterozoic — Early Paleozoic von Stump, Edmund, Gootee, Brian, Talarico, Franco

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Depositional Environments of the Byrd Group, Byrd Glacier Area: A Cambrian Record of Sedimentation, Tectonism, and Magmatism von Gootee, Brian, Stump, Edmund

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