Sobral Formation

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1to resolve the field relations between the various sedimentary units exposed there. Sobral Formation sandstones exposed along the shore at the east end of Cross Valley appear to belong to a facies different from any reco

to resolve the field relations between the various sedimentary units exposed there. Sobral Formation sandstones exposed along the shore at the east end of Cross Valley appear to belong to a facies different from any reco

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Language: English - Date: 2011-05-06 18:56:11
2within the Sobral Formation) may be related to global changes in sea level. The plant record reflects a gradual climatic change from cooltemperate in the Late Cretaceous to somewhat cooler temperatures in the Tertiary, a

within the Sobral Formation) may be related to global changes in sea level. The plant record reflects a gradual climatic change from cooltemperate in the Late Cretaceous to somewhat cooler temperatures in the Tertiary, a

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Language: English - Date: 2011-05-06 07:06:58
3Tertiary boundary. Over much of this section it was possible to collect at 1.5-meter intervals; for most of the remainder, we could collect at 3-meter intervals. Cretaceous strata (Lopez de Bertodano Formation) cropping

Tertiary boundary. Over much of this section it was possible to collect at 1.5-meter intervals; for most of the remainder, we could collect at 3-meter intervals. Cretaceous strata (Lopez de Bertodano Formation) cropping

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Language: English - Date: 2011-05-06 05:46:01
4Early geologic history of Lyreidus in Antarctica RODNEY Cape Wiman

Early geologic history of Lyreidus in Antarctica RODNEY Cape Wiman

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Language: English - Date: 2011-05-06 19:44:28
5Bookman Old Style Negreta cursiva

Bookman Old Style Negreta cursiva

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Language: English - Date: 2011-05-06 05:45:41
6Changes in the macrofossil faunas at the end of the cretaceous on Seymour Island, Antarctic Peninsula I

Changes in the macrofossil faunas at the end of the cretaceous on Seymour Island, Antarctic Peninsula I

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Language: English - Date: 2011-05-06 05:14:24
7include bivalves, gastropods, echinoderm spines, and abundant wood. This work was supported by National Science Foundation grant DPPReferences Andersson, J. Con the geology of Graham Land. Bulletin of

include bivalves, gastropods, echinoderm spines, and abundant wood. This work was supported by National Science Foundation grant DPPReferences Andersson, J. Con the geology of Graham Land. Bulletin of

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Language: English - Date: 2011-05-06 05:45:54
8Geologic studies on Seymour Island DAVID H. ELLIOT and STEVEN M. HOFFMAN  Byrd Polar Research Center

Geologic studies on Seymour Island DAVID H. ELLIOT and STEVEN M. HOFFMAN Byrd Polar Research Center

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Language: English - Date: 2011-05-06 16:41:26
9____  Figure 2. Cockburn Island, Antarctic Peninsula. Seymour Island in background. View to the southeast.  sequence exposed along one of the small gullies at the south end

____ Figure 2. Cockburn Island, Antarctic Peninsula. Seymour Island in background. View to the southeast. sequence exposed along one of the small gullies at the south end

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Language: English - Date: 2011-05-06 15:40:53
10References  but also to move pebbles and, perhaps, tamp the walls of a burrow. The description of this new genus and species of decapod not only enhances our understanding of the fossil fauna of the

References but also to move pebbles and, perhaps, tamp the walls of a burrow. The description of this new genus and species of decapod not only enhances our understanding of the fossil fauna of the

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Language: English - Date: 2011-05-06 18:56:05