East Antarctic craton

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1ated surfaces suggest deposition from wet-based terrestrial glaciers. Black shales of the overlying Mackellar Formation are in sharp contact with diamictite and sandstone of the Pagoda Formation. Lonestones are extremely

ated surfaces suggest deposition from wet-based terrestrial glaciers. Black shales of the overlying Mackellar Formation are in sharp contact with diamictite and sandstone of the Pagoda Formation. Lonestones are extremely

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 17:37:20
2Late 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

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Language: English - Date: 2011-05-06 05:15:51
3Polarforschung 67 (3): [removed], 1997 (erschienen[removed]Geologie Signifieanee of Regional Magnetie Anomalies

Polarforschung 67 (3): [removed], 1997 (erschienen[removed]Geologie Signifieanee of Regional Magnetie Anomalies

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Source URL: epic.awi.de

Language: English - Date: 2011-09-28 13:38:57