1![](https://www.pdfsearch.io/img/af9c67f543a9a06a9c1a6c0c7d0b787d.jpg) | Add to Reading ListSource URL: antarcticanz.govt.nzLanguage: English - Date: 2013-08-06 00:53:12
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2![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 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](https://www.pdfsearch.io/img/da2d5dccb738e3285552460ba98ba06a.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 16:44:07
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3![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 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](https://www.pdfsearch.io/img/c815e6ba81f3b59e3ee1d8e715d40376.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 06:15:19
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4![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 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](https://www.pdfsearch.io/img/e17acd27f6aba6da2e3153d64c197d55.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 06:15:09
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5![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 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](https://www.pdfsearch.io/img/0948874ca7da73d9c7fc99ed8a67c21a.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 03:37:40
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6![high ice hummocks. Although the ice appears to be moving rapidly in this region, the crevassing does not indicate a preferential direction of movement. Bulk ice samples were collected by chipping at locations near statio high ice hummocks. Although the ice appears to be moving rapidly in this region, the crevassing does not indicate a preferential direction of movement. Bulk ice samples were collected by chipping at locations near statio](https://www.pdfsearch.io/img/9a4234d0807a085956772e92784c5175.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 03:40:53
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7![Bookman Old Style Cursiva Bookman Old Style Cursiva](https://www.pdfsearch.io/img/7929d3fe872ba70bc942118379256bee.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 16:34:24
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8![Permian and Triassic fossil forests from the central Transantarctic Mountains EDITH L. TAYLOR, RUBEN CUNEO, and THOMAS N. TAYLOR Permian and Triassic fossil forests from the central Transantarctic Mountains EDITH L. TAYLOR, RUBEN CUNEO, and THOMAS N. TAYLOR](https://www.pdfsearch.io/img/1ffceb2083745988ecc2ad93f1ba7c2c.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 20:36:55
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9![Late Neogene and older Cenozoic microfossils in high elevation deposits of the Transantarctic Mountains: Evidence for marine sedimentation and ice volume variation on the east antarctic craton Late Neogene and older Cenozoic microfossils in high elevation deposits of the Transantarctic Mountains: Evidence for marine sedimentation and ice volume variation on the east antarctic craton](https://www.pdfsearch.io/img/ba7fe8a5074cd082b668e221f8a2d1be.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 05:15:51
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10![Depositional setting of the (Permian) Mackellar Formation, Beardmore Glacier area M.F. MILLER and R.S. FRISCH Department of Geology Vanderbilt University Depositional setting of the (Permian) Mackellar Formation, Beardmore Glacier area M.F. MILLER and R.S. FRISCH Department of Geology Vanderbilt University](https://www.pdfsearch.io/img/c7fb5514633e9c59d3698705a34b23d0.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 18:12:51
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