Geotechnical analysis on sediment cores from the Antarctic Peninsula

Sedimentological and geotechnical analyses were carried out on two undisturbed large diameter deep sea cores from the Antarctic sector of the Atlantic ocean. One core, from a silled basin within the Bransfield Strait is characterized by fine grained hemipelagic material and turbidite layers. The oth...

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Bibliographic Details
Main Author: Holler, Peter
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1985
Subjects:
KOL
M56
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.887791
https://doi.org/10.1594/PANGAEA.887791
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.887791
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.887791 2024-09-15T17:48:03+00:00 Geotechnical analysis on sediment cores from the Antarctic Peninsula Holler, Peter MEDIAN LATITUDE: -62.256665 * MEDIAN LONGITUDE: -54.960830 * SOUTH-BOUND LATITUDE: -62.275000 * WEST-BOUND LONGITUDE: -57.645000 * NORTH-BOUND LATITUDE: -62.238330 * EAST-BOUND LONGITUDE: -52.276660 * DATE/TIME START: 1981-01-01T00:00:00 * DATE/TIME END: 1981-01-01T00:00:00 1985 application/zip, 3 datasets https://doi.pangaea.de/10.1594/PANGAEA.887791 https://doi.org/10.1594/PANGAEA.887791 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.887791 https://doi.org/10.1594/PANGAEA.887791 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Holler, Peter (1985): Geotechnical properties of Antarctic deep sea sediments. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C39, 23-36, hdl:10013/epic.3ed1dcfe-1a55-418d-b20f-2c3a57fa0f58 FIBEX - First International BIOMASS Experiment ANT I GIK/IfG GIK14875-1 GIK14882-2 Institute for Geosciences Christian Albrechts University Kiel KOL M56 Meteor (1964) Piston corer (Kiel type) Southern Ocean dataset publication series 1985 ftpangaea https://doi.org/10.1594/PANGAEA.887791 2024-07-24T02:31:21Z Sedimentological and geotechnical analyses were carried out on two undisturbed large diameter deep sea cores from the Antarctic sector of the Atlantic ocean. One core, from a silled basin within the Bransfield Strait is characterized by fine grained hemipelagic material and turbidite layers. The other core, from the continental slope of the Weddell Sea represents a typical glacial marine environment. The variations of physical properties as related to both an increasing overburden pressure (or depth below top of core) and/or to lithological changes are discussed. Other/Unknown Material Antarc* Antarctic Antarctic Peninsula Bransfield Strait Southern Ocean Weddell Sea PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-57.645000,-52.276660,-62.238330,-62.275000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic FIBEX - First International BIOMASS Experiment
ANT I
GIK/IfG
GIK14875-1
GIK14882-2
Institute for Geosciences
Christian Albrechts University
Kiel
KOL
M56
Meteor (1964)
Piston corer (Kiel type)
Southern Ocean
spellingShingle FIBEX - First International BIOMASS Experiment
ANT I
GIK/IfG
GIK14875-1
GIK14882-2
Institute for Geosciences
Christian Albrechts University
Kiel
KOL
M56
Meteor (1964)
Piston corer (Kiel type)
Southern Ocean
Holler, Peter
Geotechnical analysis on sediment cores from the Antarctic Peninsula
topic_facet FIBEX - First International BIOMASS Experiment
ANT I
GIK/IfG
GIK14875-1
GIK14882-2
Institute for Geosciences
Christian Albrechts University
Kiel
KOL
M56
Meteor (1964)
Piston corer (Kiel type)
Southern Ocean
description Sedimentological and geotechnical analyses were carried out on two undisturbed large diameter deep sea cores from the Antarctic sector of the Atlantic ocean. One core, from a silled basin within the Bransfield Strait is characterized by fine grained hemipelagic material and turbidite layers. The other core, from the continental slope of the Weddell Sea represents a typical glacial marine environment. The variations of physical properties as related to both an increasing overburden pressure (or depth below top of core) and/or to lithological changes are discussed.
format Other/Unknown Material
author Holler, Peter
author_facet Holler, Peter
author_sort Holler, Peter
title Geotechnical analysis on sediment cores from the Antarctic Peninsula
title_short Geotechnical analysis on sediment cores from the Antarctic Peninsula
title_full Geotechnical analysis on sediment cores from the Antarctic Peninsula
title_fullStr Geotechnical analysis on sediment cores from the Antarctic Peninsula
title_full_unstemmed Geotechnical analysis on sediment cores from the Antarctic Peninsula
title_sort geotechnical analysis on sediment cores from the antarctic peninsula
publisher PANGAEA
publishDate 1985
url https://doi.pangaea.de/10.1594/PANGAEA.887791
https://doi.org/10.1594/PANGAEA.887791
op_coverage MEDIAN LATITUDE: -62.256665 * MEDIAN LONGITUDE: -54.960830 * SOUTH-BOUND LATITUDE: -62.275000 * WEST-BOUND LONGITUDE: -57.645000 * NORTH-BOUND LATITUDE: -62.238330 * EAST-BOUND LONGITUDE: -52.276660 * DATE/TIME START: 1981-01-01T00:00:00 * DATE/TIME END: 1981-01-01T00:00:00
long_lat ENVELOPE(-57.645000,-52.276660,-62.238330,-62.275000)
genre Antarc*
Antarctic
Antarctic Peninsula
Bransfield Strait
Southern Ocean
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Bransfield Strait
Southern Ocean
Weddell Sea
op_source Supplement to: Holler, Peter (1985): Geotechnical properties of Antarctic deep sea sediments. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C39, 23-36, hdl:10013/epic.3ed1dcfe-1a55-418d-b20f-2c3a57fa0f58
op_relation https://doi.pangaea.de/10.1594/PANGAEA.887791
https://doi.org/10.1594/PANGAEA.887791
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.887791
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