This work was supported in part by National Science Foundation grant DPPReferences Cook, E.R., and L.A. Kairiukstis (EdsMethods of dendrochronology. Dordrecht: Kluwer Academic Publications. Creber,

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Date: 2011-05-06 20:37:31 Gould Coast Transantarctic Mountains Horlick West Antarctica Reedy Glacier Nimrod Glacier Ohio Range Scott Glacier Marie Byrd Land Geography of Antarctica Queen Maud Mountains Amundsen Coast		This work was supported in part by National Science Foundation grant DPPReferences Cook, E.R., and L.A. Kairiukstis (EdsMethods of dendrochronology. Dordrecht: Kluwer Academic Publications. Creber, Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 2,92 MB Share Document on Facebook

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	the equilibrium solubility behavior of the hydrates of sodium borate (Bassett 1976; Nies and Hulbert 1967), we consider the most probable origin for this material to have been crystallization from a sub-glacial, alkaline DocID: 15a6b - View Document
	Granitic rocks were systematically collected on the traverse down Scott Glacier for later chemical analysis. In the Gothic Mountains a roof pendant of porphyry similar to the Wyatt Formation was visited and the granitic DocID: 15a3B - View Document
	Figure 1. Exposure of Unit Rg, showing meter-thick black glass layers interleaved with crystalline rhyolite. Lighter colored rock bordering the black glass is composed of devitrified glass. Figure 2. Cliff face exposure DocID: 159QM - View Document
	much lower levels than the outcrops along Touchdown Glacier. As the survey was extended south of the head of Byrd Glacier into the area of the Sefton and Zeller glaciers, a complex series of low-grade metamorphic rocks w DocID: 159vb - View Document