Gair Mesa

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1present. 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

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

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Language: English - Date: 2011-05-06 05:33:40
2

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Language: English - Date: 2011-05-06 05:32:46
3Mesozoic conchostracan fossils from Gair Mesa and Agate Peak, northern Victoria Land, Antarctica P. TASCH

Mesozoic conchostracan fossils from Gair Mesa and Agate Peak, northern Victoria Land, Antarctica P. TASCH

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Language: English - Date: 2011-05-06 18:07:01
4The Kirkpatrick Basalt, Mesa Range, northern Victoria Land D. H. ELLIoT, M. SIDERS, C. FAURE, and K. S. TAYLOR Institute of Polar Studies

The Kirkpatrick Basalt, Mesa Range, northern Victoria Land D. H. ELLIoT, M. SIDERS, C. FAURE, and K. S. TAYLOR Institute of Polar Studies

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Language: English - Date: 2011-05-06 05:37:24
5Mesozoic conchostracan fossils from Gair Mesa and Agate Peak, northern Victoria Land, Antarctica P. TASCH

Mesozoic conchostracan fossils from Gair Mesa and Agate Peak, northern Victoria Land, Antarctica P. TASCH

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Language: English - Date: 2011-05-06 18:06:30
6Maximum ground temperatures measured in warm ground areas inafter Lyon and Giggenbachand 1983 Warm ground area 2

Maximum ground temperatures measured in warm ground areas inafter Lyon and Giggenbachand 1983 Warm ground area 2

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Language: English - Date: 2011-05-06 05:00:47