Tectonic model for development of the Byrd Glacier discontinuity and surrounding regions of the Transantarctic Mountains during Neoproterozoic-Early Paleozoic

• Main Authors: Stump, E., Gootee, B., Talarico, F.
• Format: Book Part
• Language: unknown
• Published: 2006
• Subjects: Antarc*; Antarctica; Byrd Glacier; East Antarctica
• Online Access: https://epic.awi.de/id/eprint/17003/; https://epic.awi.de/id/eprint/17003/1/Stu2006d.pdf; https://doi.org/10.1007/3-540-32934-X_22; https://hdl.handle.net/10013/epic.26882; https://hdl.handle.net/10013/epic.26882.d001

The Byrd Glacier discontinuity us a major boundary crossing the Ross Orogen, with crystalline rocks to the north and primarily sedimentary rocks to the south. Most models for the tectonic development of the Ross Orogen in the central Transantarctic Mountains consits of two-dimensional transects acro...