Beacon sandstone

Results: 10



#Item
1Cooper, 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

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

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Language: English - Date: 2011-05-06 05:05:54
2The wood impressions, the occurrence of fossilized logs up to 40 centimeters in diameter, and the presence of tree stumps caught up in the flows (Barrett, Elliot, and Lindsay 1986), all point to a climate suitable for th

The wood impressions, the occurrence of fossilized logs up to 40 centimeters in diameter, and the presence of tree stumps caught up in the flows (Barrett, Elliot, and Lindsay 1986), all point to a climate suitable for th

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Language: English - Date: 2011-05-06 07:03:36
3Orthoquartzite (Farnell, West Beacon, and Brawhm Sandstones), Arena Sandstone, Altar Mountain Formation (including Ashtray Sandstone Member), New Mountain Sandstone (Terra Cotta Siltstone and Windy Gully Sandstone member

Orthoquartzite (Farnell, West Beacon, and Brawhm Sandstones), Arena Sandstone, Altar Mountain Formation (including Ashtray Sandstone Member), New Mountain Sandstone (Terra Cotta Siltstone and Windy Gully Sandstone member

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Language: English - Date: 2011-05-06 06:14:48
4canic detritus, derived from a caic-alkaline arc along the paleoPacific margin, became the principal component in sandstone. This change from cratonic to orogenic provenance was the result of a shift in the basin axis to

canic detritus, derived from a caic-alkaline arc along the paleoPacific margin, became the principal component in sandstone. This change from cratonic to orogenic provenance was the result of a shift in the basin axis to

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Language: English - Date: 2011-05-06 07:07:21
5present. 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
6Chemical index of alterationa values for Permian samples from the central Transantarctic Mountains Number of	 Standard Formation	Area	samples	Mean	deviation

Chemical index of alterationa values for Permian samples from the central Transantarctic Mountains Number of Standard Formation Area samples Mean deviation

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Language: English - Date: 2011-05-06 07:04:56
7Depositional 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

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Language: English - Date: 2011-05-06 18:12:51
8Permian and Triassic paleosols from the Beardmore Glacier region, Antarctica WLG

Permian and Triassic paleosols from the Beardmore Glacier region, Antarctica WLG

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Language: English - Date: 2011-05-06 20:44:54
9

PDF Document

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Source URL: pubs.usgs.gov

Language: English - Date: 2007-08-08 22:50:43
10

PDF Document

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Source URL: digitallibrary.amnh.org

Language: English