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Geological mapping and geochemical and geochronological analysis of metamorphic basement rocks and the McMurdo volcanics in the Skelton-Glacier and Hoopers Crags area
Entry ID:
K062_1998_1999_NZ_1
Summary
Abstract:
The Ross Orogeny refers to the collision event when East and West Antarctica met, resulting in subduction with associated deformation, crustal thickening, metamorphism and igneous activity. The nature and extent of regional and contact metamorphism during the Ross Orogeny was investigated in the Skelton-Cocks Glacier and Hooper Crags areas. Units of 'high' grade and 'low' grade metamorphism in the ...
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Geographic Coverage
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Spatial coordinates
Temporal Coverage
Start Date:
1998-11-14
Stop Date:
1998-12-18
Paleo Temporal Coverage
Paleo Start Date:
558 Ma
Paleo Stop Date: Present Chrono Unit: Location Keywords
Science Keywords
ISO Topic Category
Platform
Instrument
Ancillary Keywords
Data Set Progress
COMPLETE
Data Center
Personnel
Publications/References
Wynyard, M.J. Geology of the Cocks Glacier area, Antarctica. A study of neo-Proterozoic metamorphism, deformation and magmatism during the Ross Orogeny in south Victoria Land. M.Sc., University of Otago, 2004.
Creation and Review Dates
DIF Creation Date:
2008-10-31
Last DIF Revision Date:
2008-11-10
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