GLORIA

GEOMAR Library Ocean Research Information Access

X
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
  • 138-845; 138-846; 138-847; 138-848; 138-849; 138-850; 138-851; 138-852; 138-853; 138-854; 34-319_Site; 67-495; 85-572_Site; 9-84; Accumulation rate, calcium carbonate; AGE; Calcium carbonate; Calculated; COMPCORE; Composite Core; Density, wet bulk; DRILL; Drilling/drill rig; Elevation of event; Event label; Glomar Challenger; Joides Resolution; Latitude of event; Leg138; Leg34; Leg67; Leg85; Leg9; Longitude of event; North Pacific; North Pacific/TRENCH; North Pacific Ocean; Ocean Drilling Program; ODP; Paleoelevation; Paleolatitude; Paleolongitude; Porosity; Sedimentation rate; South Pacific/BASIN; South Pacific Ocean  (1)
  • 1995-1999  (1)
Document type
Keywords
Publisher
Years
  • 1995-1999  (1)
Year
  • 1
    facet.materialart.
    Unknown
    (Table 3) Carbonate accumulation and paleobathymetry of eastern Pacific DSDP and ODP sites (1995)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 138-845; 138-846; 138-847; 138-848; 138-849; 138-850; 138-851; 138-852; 138-853; 138-854; 34-319_Site; 67-495; 85-572_Site; 9-84; Accumulation rate, calcium carbonate; AGE; Calcium carbonate; Calculated; COMPCORE; Composite Core; Density, wet bulk; DRILL; Drilling/drill rig; Elevation of event; Event label; Glomar Challenger; Joides Resolution; Latitude of event; Leg138; Leg34; Leg67; Leg85; Leg9; Longitude of event; North Pacific; North Pacific/TRENCH; North Pacific Ocean; Ocean Drilling Program; ODP; Paleoelevation; Paleolatitude; Paleolongitude; Porosity; Sedimentation rate; South Pacific/BASIN; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 1444 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...