Transantarctic Mountains

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21much 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

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Language: English - Date: 2011-05-06 03:37:40
22dently, this clast was once at the base of the east antarctic ice sheet which may be more than 3 kilometers thick, according to the ice-flow model of Whillans and Cassidy (1983), although an extrapolation of the radar so

dently, this clast was once at the base of the east antarctic ice sheet which may be more than 3 kilometers thick, according to the ice-flow model of Whillans and Cassidy (1983), although an extrapolation of the radar so

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Language: English - Date: 2011-05-06 04:08:39
23Study of grounding-line sedimentation processes at the Mackay Glacier tongue using a remotely operated vehicle Observations on the seafloor epibenthic community MICHAEL DAwBER and  Ross D. POwELL, Department of Geology,

Study of grounding-line sedimentation processes at the Mackay Glacier tongue using a remotely operated vehicle Observations on the seafloor epibenthic community MICHAEL DAwBER and Ross D. POwELL, Department of Geology,

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Language: English - Date: 2011-05-06 17:41:00
24Specific targets, especially those related to the sediments that lie immediately above the Kukri erosion surface, were examined in detail. Several areas were found where sedimentary beds in the lower Beacon Group showed

Specific targets, especially those related to the sediments that lie immediately above the Kukri erosion surface, were examined in detail. Several areas were found where sedimentary beds in the lower Beacon Group showed

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Language: English - Date: 2011-05-06 06:13:47
25figure 2 that the core is enriched in the components ferrous oxide (FeO), magnesium oxide (MgO), calcium oxide (CaO), manganese oxide (MnO), potassium oxide (K 20), water (H20) (?), and fluorine (F) relative to the tonal

figure 2 that the core is enriched in the components ferrous oxide (FeO), magnesium oxide (MgO), calcium oxide (CaO), manganese oxide (MnO), potassium oxide (K 20), water (H20) (?), and fluorine (F) relative to the tonal

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Language: English - Date: 2011-05-06 05:40:57
26canic 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
27of this ice in the lower part of ice stream B. The differences in 180 fine structure between the 1976 and 1978 records indicate that the large, and as yet unexplained, 8 180 fluctuations in the 1978 core in this interval

of this ice in the lower part of ice stream B. The differences in 180 fine structure between the 1976 and 1978 records indicate that the large, and as yet unexplained, 8 180 fluctuations in the 1978 core in this interval

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Language: English - Date: 2011-05-06 16:46:05
28valleys and other areas to the east of the Transantarctic Mountains divide may have a source in sedimentary basins in East Antarctica. Correlation of glacial deposits by their constituent microfossils should be approache

valleys and other areas to the east of the Transantarctic Mountains divide may have a source in sedimentary basins in East Antarctica. Correlation of glacial deposits by their constituent microfossils should be approache

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Language: English - Date: 2011-05-06 18:16:29
29phorus also increased along the Onyx as far as Bull Pass, but between the pass and the Vanda Weir, it decreased bya factor of three. We suspect that an active algal community just above Bull Lake may be acting as a phosp

phorus also increased along the Onyx as far as Bull Pass, but between the pass and the Vanda Weir, it decreased bya factor of three. We suspect that an active algal community just above Bull Lake may be acting as a phosp

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Language: English - Date: 2011-05-06 06:14:18
30known. The framework modes and their sources suggest deposition in a foreland basin but do not preclude accumulation in a pull-apart basin. Resolution of basin type is hindered because sequences are fragmentary, folded,

known. The framework modes and their sources suggest deposition in a foreland basin but do not preclude accumulation in a pull-apart basin. Resolution of basin type is hindered because sequences are fragmentary, folded,

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Language: English - Date: 2011-05-06 15:39:04