Forsberg, Carl F. et al. (2001): Glacial development in the Prydz Bay region as witnessed by geotechnical and mineralogical properties of Leg 188 sites 1166 and 1167

Leg/Site/Hole:
ODP 188
ODP 188 1166
ODP 188 1167
Identifier:
2004-019654
georefid

Creator:
Forsberg, Carl F.
Norwegian Polar Institute Polarmiljosenteret, Tromso, Norway
author

Solheim, Anders
Norwegian Geotechnical Institute, Norway
author

Gruetzner, Jens
Universitaet Bremen, Federal Republic of Germany
author

Taylor, Brian
Jacques Whitford & Associates, Canada
author

Strand, Kari
University of Oulu, Finland
author

Identification:
Glacial development in the Prydz Bay region as witnessed by geotechnical and mineralogical properties of Leg 188 sites 1166 and 1167
2001
In: Florindo, Fabio (editor), Cooper, Alan K. (editor), Extended abstracts for the International ANTOSTRAT symposium on The geologic record of the Antarctic ice sheet from drilling, coring and seismic studies
Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
16
71-72
ODP sites 1166 and 1167, Antarctic continental margin in the Prydz Bay sector of the Southern Ocean, provide evidence for studying the glacial growth on Antarctica during the Eocene-Oligocene transition. Site 1167 provides good evidence of sedimentation associated with movement of the Antarctic ice sheet. This study looks at the mineralogical and geotechnical properties that control the lithostratigraphy as a way to understand the glacial evolution of the Prydz Bay region. (MTE)
English
Coverage:Geographic coordinates:
North:-66.2400
West:72.1700East: 74.4800
South:-67.4200

Stratigraphy; Antarctica; Cenozoic; clay minerals; continental margin; Eocene; glacial environment; glaciation; glaciomarine environment; grain size; Leg 188; lithofacies; marine environment; mechanical properties; mineral composition; Ocean Drilling Program; ODP Site 1166; ODP Site 1167; Oligocene; Paleogene; Prydz Bay; resistivity; sheet silicates; silicates; size distribution; Southern Ocean; Tertiary;

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