GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 032; 037; 052; 2-19-1; 3-17-1; 3-7-1; GC; Glacier; Gravity corer; International Weddell Sea Oceanographic Expeditions; IWSOE68; IWSOE68-032; IWSOE68-037; IWSOE68-052; IWSOE70; IWSOE70-2-19-1; IWSOE70-3-17-1; IWSOE70-3-7-1; PC; Piston corer  (1)
  • 14.2 km at 096° true from Cape Roberts; Cape Roberts Project; Core wireline system; CRP; CRP-2; CRP-2A; CWS; off Cape Roberts, Ross Sea, Antarctica; Sampling/drilling from ice  (1)
Document type
Keywords
Publisher
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Anderson, John B; Andrews, John T (1999): Radiocarbon constrains on ice sheet advance and retreat in the Weddell Sea, Antarctica. Geology, 27(2), 179-182, https://doi.org/10.1130/0091-7613(1999)027%3C0179:RCOISA%3E2.3.CO;2
    Publication Date: 2023-06-27
    Description: We report here the results of a study aimed at providing radiometric age control on glacial events in the Weddell Sea during the late Quaternary. Sediment cores from the eastern continental shelf, where the East Antarctic ice sheet was grounded, have recovered glacial-marine sediments resting on tills and the latter deposits predate the isotope stage 2 last glacial maximum. Sediment cores from the continental slope and rise sampled a prominent ice-rafted debris layer, and radiocarbon ages indicate that this ice-rafting event took place prior to 26 000 yr B.P. Thus, the combined data indicate that significant deglaciation of the Weddell Sea continental shelf took place prior to the last glacial maximum. Our data also suggest that the ice masses that border the Weddell Sea are more extensive than they were during the previous glacial minimum.
    Keywords: 032; 037; 052; 2-19-1; 3-17-1; 3-7-1; GC; Glacier; Gravity corer; International Weddell Sea Oceanographic Expeditions; IWSOE68; IWSOE68-032; IWSOE68-037; IWSOE68-052; IWSOE70; IWSOE70-2-19-1; IWSOE70-3-17-1; IWSOE70-3-7-1; PC; Piston corer
    Type: Dataset
    Format: application/zip, 6 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Barrett, Peter J; Anderson, John B (2000): Grain size analysis of samples from CRP-2/2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(3), 373-378, hdl:10013/epic.28267.d001
    Publication Date: 2023-06-27
    Description: The purpose of this note is to present results of grain size analyses from 118 samples of the CRP-2/2A core using sieve and Sedigraph techniques. The samples were selected to represent the range of facies encountered, and tend to become more widely spaced with depth. Fifteen came from the upper 27 m of Quaternary and Pliocene sediments, 62 from the early Miocene-late Oligocene strata (27 to 307 mbsf), and 41 from the early Oligocene strata beneath (307 to 624 mbsf). The results are intended to provide reference data for lithological descriptions in the core logs (Cape Roberts Science Team, 1999), and to help with facies interpretation. The analytical technique used for determining size frequency of the sand fraction in our samples (sieving) is simple, physical and widely practised for over a century. Thus it provides a useful reference point for analyses produced by other faster and more sophisticated techniques, such as the Malvern laser particle size analysis system (Woolfe et al., 2000), and estimates derived from measurements taken with down-hole logging tools (Bücker, pers. com., 1999).
    Keywords: 14.2 km at 096° true from Cape Roberts; Cape Roberts Project; Core wireline system; CRP; CRP-2; CRP-2A; CWS; off Cape Roberts, Ross Sea, Antarctica; Sampling/drilling from ice
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...