Summary of 40Ar/39Ar results from sediment core CRP-2A (Table 1) ...

40Ar/39Ar analyses of tephra and clasts of volcanic rock provide age constraints for upper parts of the CRP-2A core. Single-crystal laser-fusion analyses of anorthoclase phenocrysts from three tephra-bearing layers yielded the most precise age constraints for CRP-2A. The dated tephra layers are: 1)...

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Bibliographic Details
Main Author: McIntosh, W C
Format: Dataset
Language:English
Published: PANGAEA 2004
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.194709
https://doi.pangaea.de/10.1594/PANGAEA.194709
id ftdatacite:10.1594/pangaea.194709
record_format openpolar
spelling ftdatacite:10.1594/pangaea.194709 2024-09-15T17:45:47+00:00 Summary of 40Ar/39Ar results from sediment core CRP-2A (Table 1) ... McIntosh, W C 2004 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.194709 https://doi.pangaea.de/10.1594/PANGAEA.194709 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Sample ID Sample comment Comment Age, dated material Sample method Number Argon-39 Calcium/Potassium ratio Age, dated Age, error Core wireline system Isotope ratio mass spectrometry see comment CRP-2 Sampling/drilling from ice Cape Roberts Project CRP dataset Supplementary Dataset Dataset 2004 ftdatacite https://doi.org/10.1594/pangaea.194709 2024-08-01T11:02:40Z 40Ar/39Ar analyses of tephra and clasts of volcanic rock provide age constraints for upper parts of the CRP-2A core. Single-crystal laser-fusion analyses of anorthoclase phenocrysts from three tephra-bearing layers yielded the most precise age constraints for CRP-2A. The dated tephra layers are: 1) a 2.7-m-thick interval of pumice and ash layers between 111.5 and 114.2 meters below sea floor (mbsf) (weighted mean age = 21.44 ± 0.05 Ma, +2.2); 2) a concentration of pumice near 193.4 mbsf (23.98 ± 0.13 Ma): and 3) a concentration of pumice near 280 mbsf (24,22 ± 0.03 Ma) (all ages are calibrated relative to Fish Canyon Tuff sanidine at 27.84 Ma). The 111 to 114 mbsf tephra is almost entirely non-reworked, and the 193 mbsf and 280 mbsf tephra concentrations are interpreted as being reworked and redeposited soon after eruption. All three of the tephra ages are therefore considered to be equivalent to depositional ages. The variation in precision of these three age determinations is largely a function of ... : Supplement to: McIntosh, W C (2000): 40Ar/39Ar geochronology of tephra and volcanic clasts in CRP-2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(4), 621-630 ... Dataset Antarc* Antarctica antartic* Victoria Land DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Sample ID
Sample comment
Comment
Age, dated material
Sample method
Number
Argon-39
Calcium/Potassium ratio
Age, dated
Age, error
Core wireline system
Isotope ratio mass spectrometry
see comment
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
spellingShingle DEPTH, sediment/rock
Sample ID
Sample comment
Comment
Age, dated material
Sample method
Number
Argon-39
Calcium/Potassium ratio
Age, dated
Age, error
Core wireline system
Isotope ratio mass spectrometry
see comment
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
McIntosh, W C
Summary of 40Ar/39Ar results from sediment core CRP-2A (Table 1) ...
topic_facet DEPTH, sediment/rock
Sample ID
Sample comment
Comment
Age, dated material
Sample method
Number
Argon-39
Calcium/Potassium ratio
Age, dated
Age, error
Core wireline system
Isotope ratio mass spectrometry
see comment
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
description 40Ar/39Ar analyses of tephra and clasts of volcanic rock provide age constraints for upper parts of the CRP-2A core. Single-crystal laser-fusion analyses of anorthoclase phenocrysts from three tephra-bearing layers yielded the most precise age constraints for CRP-2A. The dated tephra layers are: 1) a 2.7-m-thick interval of pumice and ash layers between 111.5 and 114.2 meters below sea floor (mbsf) (weighted mean age = 21.44 ± 0.05 Ma, +2.2); 2) a concentration of pumice near 193.4 mbsf (23.98 ± 0.13 Ma): and 3) a concentration of pumice near 280 mbsf (24,22 ± 0.03 Ma) (all ages are calibrated relative to Fish Canyon Tuff sanidine at 27.84 Ma). The 111 to 114 mbsf tephra is almost entirely non-reworked, and the 193 mbsf and 280 mbsf tephra concentrations are interpreted as being reworked and redeposited soon after eruption. All three of the tephra ages are therefore considered to be equivalent to depositional ages. The variation in precision of these three age determinations is largely a function of ... : Supplement to: McIntosh, W C (2000): 40Ar/39Ar geochronology of tephra and volcanic clasts in CRP-2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(4), 621-630 ...
format Dataset
author McIntosh, W C
author_facet McIntosh, W C
author_sort McIntosh, W C
title Summary of 40Ar/39Ar results from sediment core CRP-2A (Table 1) ...
title_short Summary of 40Ar/39Ar results from sediment core CRP-2A (Table 1) ...
title_full Summary of 40Ar/39Ar results from sediment core CRP-2A (Table 1) ...
title_fullStr Summary of 40Ar/39Ar results from sediment core CRP-2A (Table 1) ...
title_full_unstemmed Summary of 40Ar/39Ar results from sediment core CRP-2A (Table 1) ...
title_sort summary of 40ar/39ar results from sediment core crp-2a (table 1) ...
publisher PANGAEA
publishDate 2004
url https://dx.doi.org/10.1594/pangaea.194709
https://doi.pangaea.de/10.1594/PANGAEA.194709
genre Antarc*
Antarctica
antartic*
Victoria Land
genre_facet Antarc*
Antarctica
antartic*
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.194709
_version_ 1810493694052139008