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Stratigraphy Dufek Coast Fremouw Formation Lystrosaurus American Museum of Natural History Transantarctic Mountains Antarctica Glossopteris Beacon sandstone Geology Physical geography Geologic formations		Add to Reading List Source URL: digitallibrary.amnh.org Download Document from Source Website Share Document on Facebook

	Cooper, R. A., J . B. Jago, A. J . Rowell, and P. Braddock. In press. Age and correlation of the Cambrian—Ordovician Bowers Supergroup, northern Victoria Land. In R. L. Oliver, J. B. Jago, and P. R. James (Eds.), Antar DocID: 159YE - View Document
	floodplain deposits laterally suggests a scenario in which a forested, swampy island was undercut and destroyed during flooding. Once buried, the fossil peat was quickly silicified before compression could take place, pr DocID: 159VH - View Document
	present. Orientations of abundant striations on fault surfaces (slickensides) and other features clearly indicate normal or reverse faulting with little or no strike-slip movement (figure 3). The last of these appears re DocID: 1586N - View Document
	Carbon isotope composition of Permian and Triassic plants in silicified peat, Transantarctic Mountains GUNTER FAURE and TERESA M. MENSING DocID: 14yKk - View Document
	Chemical index of alterationa values for Permian samples from the central Transantarctic Mountains Number of Standard Formation Area samples Mean deviation DocID: 14lCw - View Document