Environmental analysis on sediment core CRP-2 from the Ross Sea, Antarctica ...

Cape Roberts Project drill core 2/2A was obtained from Roberts Ridge, a sea-floor high located at 77° S, 16 km offshore from Cape Roberts in western McMurdo Sound, Antarctica. The recovered core is about 624 m long and includes strata dated as being Quaternary, Pliocene, Miocene and Oligocene in age...

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Main Authors: Powell, Ross, Krissek, Lawrence A, van der Meer, Jaap
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2000
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.510752
https://doi.pangaea.de/10.1594/PANGAEA.510752
id ftdatacite:10.1594/pangaea.510752
record_format openpolar
spelling ftdatacite:10.1594/pangaea.510752 2024-09-15T17:45:55+00:00 Environmental analysis on sediment core CRP-2 from the Ross Sea, Antarctica ... Powell, Ross Krissek, Lawrence A van der Meer, Jaap 2000 application/zip https://dx.doi.org/10.1594/pangaea.510752 https://doi.pangaea.de/10.1594/PANGAEA.510752 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Core wireline system CRP-2 Sampling/drilling from ice Cape Roberts Project CRP article Collection Supplementary Publication Series of Datasets 2000 ftdatacite https://doi.org/10.1594/pangaea.510752 2024-08-01T10:54:59Z Cape Roberts Project drill core 2/2A was obtained from Roberts Ridge, a sea-floor high located at 77° S, 16 km offshore from Cape Roberts in western McMurdo Sound, Antarctica. The recovered core is about 624 m long and includes strata dated as being Quaternary, Pliocene, Miocene and Oligocene in age. The core includes twelve facies commonly occurring in associations that are repeated in particular sequences throughout the core and which are interpreted as representing different depositional environments through time. Depositional systems inferred to be represented in the succession include: outer shelf with minor iceberg influence, outer shelf-inner shelf-nearshore to shoreface under iceberg influence, deltaic and/or grounding-line fan, and ice proximal-ice marginal-subglacial (mass flow/rainout diamictite/subglacial till) singly or in combination. Changes in palaeoenvironmental interpretations up the core are used to estimate relative glacial proximity to the site through time. These inferred glacial ... : Supplement to: Powell, Ross; Krissek, Lawrence A; van der Meer, Jaap (2000): Preliminary depositional environmental analysis of CRP-2/2A, Victoria Land Basin, Antarctica: palaeoglaciological and palaeoclimatic inferences. Terra Antartica, 7(3), 313-322 ... Article in Journal/Newspaper Antarc* Antarctica antartic* McMurdo Sound Ross Sea Victoria Land DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Core wireline system
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
spellingShingle Core wireline system
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
Powell, Ross
Krissek, Lawrence A
van der Meer, Jaap
Environmental analysis on sediment core CRP-2 from the Ross Sea, Antarctica ...
topic_facet Core wireline system
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
description Cape Roberts Project drill core 2/2A was obtained from Roberts Ridge, a sea-floor high located at 77° S, 16 km offshore from Cape Roberts in western McMurdo Sound, Antarctica. The recovered core is about 624 m long and includes strata dated as being Quaternary, Pliocene, Miocene and Oligocene in age. The core includes twelve facies commonly occurring in associations that are repeated in particular sequences throughout the core and which are interpreted as representing different depositional environments through time. Depositional systems inferred to be represented in the succession include: outer shelf with minor iceberg influence, outer shelf-inner shelf-nearshore to shoreface under iceberg influence, deltaic and/or grounding-line fan, and ice proximal-ice marginal-subglacial (mass flow/rainout diamictite/subglacial till) singly or in combination. Changes in palaeoenvironmental interpretations up the core are used to estimate relative glacial proximity to the site through time. These inferred glacial ... : Supplement to: Powell, Ross; Krissek, Lawrence A; van der Meer, Jaap (2000): Preliminary depositional environmental analysis of CRP-2/2A, Victoria Land Basin, Antarctica: palaeoglaciological and palaeoclimatic inferences. Terra Antartica, 7(3), 313-322 ...
format Article in Journal/Newspaper
author Powell, Ross
Krissek, Lawrence A
van der Meer, Jaap
author_facet Powell, Ross
Krissek, Lawrence A
van der Meer, Jaap
author_sort Powell, Ross
title Environmental analysis on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_short Environmental analysis on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_full Environmental analysis on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_fullStr Environmental analysis on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_full_unstemmed Environmental analysis on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_sort environmental analysis on sediment core crp-2 from the ross sea, antarctica ...
publisher PANGAEA
publishDate 2000
url https://dx.doi.org/10.1594/pangaea.510752
https://doi.pangaea.de/10.1594/PANGAEA.510752
genre Antarc*
Antarctica
antartic*
McMurdo Sound
Ross Sea
Victoria Land
genre_facet Antarc*
Antarctica
antartic*
McMurdo Sound
Ross Sea
Victoria Land
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.510752
_version_ 1810493861178376192