Gruetzner, Jens et al. (2001): Evidence for palaeoclimatic variability at the East Antarctic continental rise (ODP Site 1165) inferred from spectral analysis of high-resolution core logging data

Leg/Site/Hole:
ODP 188
ODP 188 1165
Identifier:
2004-019659
georefid

Creator:
Gruetzner, Jens
Universitaet Bremen, Fachbereich Geowissenschaften, Bremen, Federal Republic of Germany
author

Rebesco, Michele
Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Italy
author

Forsberg, Carl F.
Norwegian Polar Institute, Norway
author

Cooper, Alan K.
Stanford University, United States
author

Identification:
Evidence for palaeoclimatic variability at the East Antarctic continental rise (ODP Site 1165) inferred from spectral analysis of high-resolution core logging data
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
81-82
ODP Site 1165, Prydz Bay, Southern Ocean provides data to study paleoclimate changes of the upper Miocene-lower Pliocene. Spectral analysis of high-resolution core logging data allows characterization of sedimentary cycles and ice advances of the Lambert Glacier system into Prydz Bay, sea ice extent, and variations in ocean circulation. (MTE)
English
Coverage:Geographic coordinates:
North:-64.2200
West:67.1300East: 67.1400
South:-64.2300

Stratigraphy; Antarctica; bulk density; Cenozoic; climate change; continental rise; cores; East Antarctica; glacial environment; high-resolution methods; interglacial environment; Leg 188; lithofacies; magnetic properties; magnetic susceptibility; marine environment; Miocene; Neogene; Ocean Drilling Program; ocean floors; ODP Site 1165; paleo-oceanography; paleocirculation; paleoclimatology; paleomagnetism; Pliocene; Prydz Bay; Southern Ocean; Tertiary;

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