Sand geochemistry on sediment core CRP-3 from the Ross Sea, Antarctica ...

A total of 167 samples distubuted throughout the CRP-3 drillhole from 5.77 to 787.68 mbsf and representing fine to coarse sandstones have been analysed by X-ray fluorescence spectrometry (XRF) Bulk sample geochemistry (major and trace elements) indicates a dominant provenance of detritus from the Fe...

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Main Authors: Sprovieri, Mario, Bellanca, Adriana, Neri, Rodolfo
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.510771
https://doi.pangaea.de/10.1594/PANGAEA.510771
id ftdatacite:10.1594/pangaea.510771
record_format openpolar
spelling ftdatacite:10.1594/pangaea.510771 2024-09-15T17:44:05+00:00 Sand geochemistry on sediment core CRP-3 from the Ross Sea, Antarctica ... Sprovieri, Mario Bellanca, Adriana Neri, Rodolfo 2001 application/zip https://dx.doi.org/10.1594/pangaea.510771 https://doi.pangaea.de/10.1594/PANGAEA.510771 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-3 Sampling/drilling from ice Cape Roberts Project CRP article Collection Supplementary Publication Series of Datasets 2001 ftdatacite https://doi.org/10.1594/pangaea.510771 2024-08-01T11:01:17Z A total of 167 samples distubuted throughout the CRP-3 drillhole from 5.77 to 787.68 mbsf and representing fine to coarse sandstones have been analysed by X-ray fluorescence spectrometry (XRF) Bulk sample geochemistry (major and trace elements) indicates a dominant provenance of detritus from the Ferrar Supergroup in the uppermost 200 mbsf of the core. A markedly increased contribution from the Beacon sandstones is recognized below 200 mbsf and down to 600 mbsf. In the lower part of CRP-3, down to 787.68 mbsf, geochemical evidence for influxes of Ferrar materials is again recorded. On the basis of preliminary magnetostratigraphic data reported for the lower 447 mbsf of the drillhole, we tentatively evaluated the main periodicities modulating the geochemical records. Our results identify a possible influence of the precession, obliquity and long-eccentricity astronomical components (21, 41, and 400 ky frequency bands) on the deposition mechanisms of the studied glaciomarine sediments. ... : Supplement to: Sprovieri, Mario; Bellanca, Adriana; Neri, Rodolfo (2001): Bulk geochemistry of the sand fraction from CRP-3 (Victoria Land Basin, Antarctica): Evidence of provenance and Milankovitch climaric fluctuations. Terra Antartica, 8(4), 551-560 ... Article in Journal/Newspaper Antarc* Antarctica antartic* Ross Sea Victoria Land DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Core wireline system
CRP-3
Sampling/drilling from ice
Cape Roberts Project CRP
spellingShingle Core wireline system
CRP-3
Sampling/drilling from ice
Cape Roberts Project CRP
Sprovieri, Mario
Bellanca, Adriana
Neri, Rodolfo
Sand geochemistry on sediment core CRP-3 from the Ross Sea, Antarctica ...
topic_facet Core wireline system
CRP-3
Sampling/drilling from ice
Cape Roberts Project CRP
description A total of 167 samples distubuted throughout the CRP-3 drillhole from 5.77 to 787.68 mbsf and representing fine to coarse sandstones have been analysed by X-ray fluorescence spectrometry (XRF) Bulk sample geochemistry (major and trace elements) indicates a dominant provenance of detritus from the Ferrar Supergroup in the uppermost 200 mbsf of the core. A markedly increased contribution from the Beacon sandstones is recognized below 200 mbsf and down to 600 mbsf. In the lower part of CRP-3, down to 787.68 mbsf, geochemical evidence for influxes of Ferrar materials is again recorded. On the basis of preliminary magnetostratigraphic data reported for the lower 447 mbsf of the drillhole, we tentatively evaluated the main periodicities modulating the geochemical records. Our results identify a possible influence of the precession, obliquity and long-eccentricity astronomical components (21, 41, and 400 ky frequency bands) on the deposition mechanisms of the studied glaciomarine sediments. ... : Supplement to: Sprovieri, Mario; Bellanca, Adriana; Neri, Rodolfo (2001): Bulk geochemistry of the sand fraction from CRP-3 (Victoria Land Basin, Antarctica): Evidence of provenance and Milankovitch climaric fluctuations. Terra Antartica, 8(4), 551-560 ...
format Article in Journal/Newspaper
author Sprovieri, Mario
Bellanca, Adriana
Neri, Rodolfo
author_facet Sprovieri, Mario
Bellanca, Adriana
Neri, Rodolfo
author_sort Sprovieri, Mario
title Sand geochemistry on sediment core CRP-3 from the Ross Sea, Antarctica ...
title_short Sand geochemistry on sediment core CRP-3 from the Ross Sea, Antarctica ...
title_full Sand geochemistry on sediment core CRP-3 from the Ross Sea, Antarctica ...
title_fullStr Sand geochemistry on sediment core CRP-3 from the Ross Sea, Antarctica ...
title_full_unstemmed Sand geochemistry on sediment core CRP-3 from the Ross Sea, Antarctica ...
title_sort sand geochemistry on sediment core crp-3 from the ross sea, antarctica ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.510771
https://doi.pangaea.de/10.1594/PANGAEA.510771
genre Antarc*
Antarctica
antartic*
Ross Sea
Victoria Land
genre_facet Antarc*
Antarctica
antartic*
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.510771
_version_ 1810491417427968000