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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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 |
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English |
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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 |
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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 |