[Parameters: Topic='SOLID EARTH', Term='ROCKS/MINERALS', Variable_Level_1='MINERALS/CRYSTALS']
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Geochemistry, paleomagnetism and intrusive history of the Ferrar Dolerites, Antarctica
Entry ID:
K061_2004_2007_NZ_1
Summary
Abstract:
A suite of geological samples were collected in the Transanatarctic Mountains for paleomagnetic and geochemical analysis. Combined with field observations, these samples will help determine magma flow directions at upper crustal depths during emplacement of the Ferrar Large Igneous Province at c. 180 Ma. Paleomagnetic samples are oriented; rock samples average 1 kg. About 300 kg of rock was sampled per season overall. Samples are housed at the Department of Geology, University of Otago, Dunedin, New Zealand.
Related URL
Geographic Coverage
(Click for Interactive Map)
Spatial coordinates
Paleo Temporal Coverage
Paleo Start Date:
180 Ma
Paleo Stop Date: 180 Ma Chrono Unit: Location Keywords
Science Keywords
ISO Topic Category
Project
Access Constraints
see http://data.scarmarbin.be/duaForm
Use Constraints
see http://data.scarmarbin.be/duaForm
Ancillary Keywords
Data Set Progress
COMPLETE
Originating Center
Data Center
Distribution
Distribution Format:
www
Fees:
free
Personnel
Publications/References
Glover, A.G., Smith, C.R., Mincks, S.L., Sumida, P.Y., Thurber, A., 2008. Macrofaunal abundance and composition on theWest Antarctic Peninsula continental shelf: evidence for a sediment ‘food bank’ and similarities to deep-sea habitats. Deep-Sea Research II, 55 (2491–2501)
Creation and Review Dates
DIF Creation Date:
2010-11-08
Last DIF Revision Date:
2010-11-08
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