Science Keywords>SOLID EARTH>GEOMORPHOLOGY
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The Heimdall and Kukri Erosion surfaces
Entry ID:
K051_2007_2008_NZ_1
Summary
Abstract:
The Heimdall Erosion Surface was followed southwards from the Olympus Range through the Asgard Range and onward to the mountains south of the Taylor-Ferrar Glaciers where it is said to die out or become unrecognizable. Wherever possible, the base of the Taylor Group and its relationship to the basement was investigated. At each site a reconnaissance was conducted to determine the best sections to ...
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Spatial coordinates
Temporal Coverage
Start Date:
2008-01-08
Stop Date:
2008-02-05
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Quality
All remaining samples and thin sections of all the analysed rocks are kept in the University of Canterbury geological rock collection. For more information, please contact the investigator or the department.
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Data Set Progress
COMPLETE
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Publications/References
O'Toole, T, MSc thesis in progress
O'Toole, T, Gilmer, G., Bradshaw, M. A, Bradshaw, J.D. and Bassett, K.N. Soft sediment deforrmation in Devonian Beacon Group, southern Victoria Land: Aeolian or Submarine slumping? Abstract, Annual Antarctic conference 2008, Dunedin Gilmer, G., O'Toole, T, Bradshaw, M. A, Bradshaw, J.D. and Bassett, K.N. Paleoenvironmental interpretation of the New Mountain Sandstone, Taylor Group, southern Victoria Land. Abstract, Annual Antarctic conference 2008, Dunedin. Bradshaw, J.D., Bradshaw, M. A, Gilmer, G. and O'Toole, T. The topography of the Kukri Erosion Srface: Tectonics of Taylor Group Sedimentary Basin initiation. Abstract, Annual Antarctic conference 2008, Dunedin Creation and Review Dates
DIF Creation Date:
2005-09-22
Last DIF Revision Date:
2009-06-06
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