Description of lithofacies associations and their interpreted settings from sequences of sediment core CRP-1 (Table 2) ...
Cape Roberts Project drillcore 1 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 147 m long with the upper 43.15 metres below the sea floor (revised figure) being dated as Quarternar...
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ftdatacite:10.1594/pangaea.433089 2024-09-15T17:46:33+00:00 Description of lithofacies associations and their interpreted settings from sequences of sediment core CRP-1 (Table 2) ... Powell, Ross Hambrey, Mike J Krissek, Lawrence A 1998 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.433089 https://doi.pangaea.de/10.1594/PANGAEA.433089 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Depth, top/min Depth, bottom/max Facies name/code Lithology/composition/facies Environment Core wireline system CRP-1 Sampling/drilling ice Cape Roberts Project CRP dataset Supplementary Dataset Dataset 1998 ftdatacite https://doi.org/10.1594/pangaea.433089 2024-08-01T11:00:37Z Cape Roberts Project drillcore 1 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 147 m long with the upper 43.15 metres below the sea floor (revised figure) being dated as Quarternary and the older part of the sequence being Miocene. The core includes nine facies: sandy diamict, muddy diamict, gravel/conglomerate, mud(stone), clay(stone) and carbonate. These facies occure in associations that are repeated in particulare sequences throughout the core, and are interpreted as representing different depositional environments through time. Seven lithofacies associations are interpreted as representing offshore shelf, ice protected/below wave-base; prodeltaic/offshore shelf; delta front/sandy shelf; ice system; subglacial till/rainout diamict/debris flow diamicts singly or in combination; and a carbonate-rich shelf bank. The facies associations are used to infer that the Quaternary section ... : Supplement to: Powell, Ross; Hambrey, Mike J; Krissek, Lawrence A (1998): Quaternary and Miocene glacial and climatic history of the Cape Roberts drillsite region, Antarctica. Terra Antartica, 5(3), 341-351 ... Dataset Antarc* Antarctica antartic* McMurdo Sound DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Facies name/code Lithology/composition/facies Environment Core wireline system CRP-1 Sampling/drilling ice Cape Roberts Project CRP |
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DEPTH, sediment/rock Depth, top/min Depth, bottom/max Facies name/code Lithology/composition/facies Environment Core wireline system CRP-1 Sampling/drilling ice Cape Roberts Project CRP Powell, Ross Hambrey, Mike J Krissek, Lawrence A Description of lithofacies associations and their interpreted settings from sequences of sediment core CRP-1 (Table 2) ... |
topic_facet |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Facies name/code Lithology/composition/facies Environment Core wireline system CRP-1 Sampling/drilling ice Cape Roberts Project CRP |
description |
Cape Roberts Project drillcore 1 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 147 m long with the upper 43.15 metres below the sea floor (revised figure) being dated as Quarternary and the older part of the sequence being Miocene. The core includes nine facies: sandy diamict, muddy diamict, gravel/conglomerate, mud(stone), clay(stone) and carbonate. These facies occure in associations that are repeated in particulare sequences throughout the core, and are interpreted as representing different depositional environments through time. Seven lithofacies associations are interpreted as representing offshore shelf, ice protected/below wave-base; prodeltaic/offshore shelf; delta front/sandy shelf; ice system; subglacial till/rainout diamict/debris flow diamicts singly or in combination; and a carbonate-rich shelf bank. The facies associations are used to infer that the Quaternary section ... : Supplement to: Powell, Ross; Hambrey, Mike J; Krissek, Lawrence A (1998): Quaternary and Miocene glacial and climatic history of the Cape Roberts drillsite region, Antarctica. Terra Antartica, 5(3), 341-351 ... |
format |
Dataset |
author |
Powell, Ross Hambrey, Mike J Krissek, Lawrence A |
author_facet |
Powell, Ross Hambrey, Mike J Krissek, Lawrence A |
author_sort |
Powell, Ross |
title |
Description of lithofacies associations and their interpreted settings from sequences of sediment core CRP-1 (Table 2) ... |
title_short |
Description of lithofacies associations and their interpreted settings from sequences of sediment core CRP-1 (Table 2) ... |
title_full |
Description of lithofacies associations and their interpreted settings from sequences of sediment core CRP-1 (Table 2) ... |
title_fullStr |
Description of lithofacies associations and their interpreted settings from sequences of sediment core CRP-1 (Table 2) ... |
title_full_unstemmed |
Description of lithofacies associations and their interpreted settings from sequences of sediment core CRP-1 (Table 2) ... |
title_sort |
description of lithofacies associations and their interpreted settings from sequences of sediment core crp-1 (table 2) ... |
publisher |
PANGAEA |
publishDate |
1998 |
url |
https://dx.doi.org/10.1594/pangaea.433089 https://doi.pangaea.de/10.1594/PANGAEA.433089 |
genre |
Antarc* Antarctica antartic* McMurdo Sound |
genre_facet |
Antarc* Antarctica antartic* McMurdo Sound |
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.433089 |
_version_ |
1810494785102807040 |