(Table 2) Apatite fission track results from sediment core CRP-3 ...

The Cape Roberts drillhole 3 (CRP-3) on the western edge of the Victoria Land Basin, Antarctica cored through a highly altered igneous intrusion intruded into Paleozoic sedimentary basement. This intrusion was regarded as highly enigmatic as its origin could represent volcanism associated with early...

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Bibliographic Details
Main Author: Fitzgerald, Paul G
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.484981
https://doi.pangaea.de/10.1594/PANGAEA.484981
id ftdatacite:10.1594/pangaea.484981
record_format openpolar
spelling ftdatacite:10.1594/pangaea.484981 2024-09-15T17:43:01+00:00 (Table 2) Apatite fission track results from sediment core CRP-3 ... Fitzgerald, Paul G 2001 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.484981 https://doi.pangaea.de/10.1594/PANGAEA.484981 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 Lithology/composition/facies Grains, counted/analyzed Sample comment Probability, chi-square test Error, relative Age, dated Age, dated standard deviation Length Standard deviation Core wireline system CRP-3 Sampling/drilling from ice Cape Roberts Project CRP dataset Supplementary Dataset Dataset 2001 ftdatacite https://doi.org/10.1594/pangaea.484981 2024-08-01T11:00:37Z The Cape Roberts drillhole 3 (CRP-3) on the western edge of the Victoria Land Basin, Antarctica cored through a highly altered igneous intrusion intruded into Paleozoic sedimentary basement. This intrusion was regarded as highly enigmatic as its origin could represent volcanism associated with early rifling of the Victoria Land Basin, later renewed rifting within the Terror rift, or Jurassic tholeiitic magmatism. Direct methods to date the intrusion by U-Pb dating of zircon or fission track analysis failed due to insufficient quantities of these minerals. Apatite fission track (AFT) analysis on the adjacent sedimentary basement, the Devonian Beacon Supergroup sandstone, yielded an age of 101 ± 6 Ma and a mean track length of 12.3 µm with a 1.9 µm standard deviation. The fission tracks were not annealed in the Cenozoic and thus the intrusion must be older than this. This observation, plus race element chemistry of the intrusion suggest it is most likely the same age and original composition as the middle ... : Supplement to: Fitzgerald, Paul G (2001): Apatite fission track ages associated with the altered igneous intrusive in beacon sandstone near the base of CRP-3, Victoria Land Basin, Antarctica. Terra Antartica, 8(4), 585-592 ... Dataset Antarc* Antarctica antartic* Victoria Land DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Lithology/composition/facies
Grains, counted/analyzed
Sample comment
Probability, chi-square test
Error, relative
Age, dated
Age, dated standard deviation
Length
Standard deviation
Core wireline system
CRP-3
Sampling/drilling from ice
Cape Roberts Project CRP
spellingShingle DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Lithology/composition/facies
Grains, counted/analyzed
Sample comment
Probability, chi-square test
Error, relative
Age, dated
Age, dated standard deviation
Length
Standard deviation
Core wireline system
CRP-3
Sampling/drilling from ice
Cape Roberts Project CRP
Fitzgerald, Paul G
(Table 2) Apatite fission track results from sediment core CRP-3 ...
topic_facet DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Lithology/composition/facies
Grains, counted/analyzed
Sample comment
Probability, chi-square test
Error, relative
Age, dated
Age, dated standard deviation
Length
Standard deviation
Core wireline system
CRP-3
Sampling/drilling from ice
Cape Roberts Project CRP
description The Cape Roberts drillhole 3 (CRP-3) on the western edge of the Victoria Land Basin, Antarctica cored through a highly altered igneous intrusion intruded into Paleozoic sedimentary basement. This intrusion was regarded as highly enigmatic as its origin could represent volcanism associated with early rifling of the Victoria Land Basin, later renewed rifting within the Terror rift, or Jurassic tholeiitic magmatism. Direct methods to date the intrusion by U-Pb dating of zircon or fission track analysis failed due to insufficient quantities of these minerals. Apatite fission track (AFT) analysis on the adjacent sedimentary basement, the Devonian Beacon Supergroup sandstone, yielded an age of 101 ± 6 Ma and a mean track length of 12.3 µm with a 1.9 µm standard deviation. The fission tracks were not annealed in the Cenozoic and thus the intrusion must be older than this. This observation, plus race element chemistry of the intrusion suggest it is most likely the same age and original composition as the middle ... : Supplement to: Fitzgerald, Paul G (2001): Apatite fission track ages associated with the altered igneous intrusive in beacon sandstone near the base of CRP-3, Victoria Land Basin, Antarctica. Terra Antartica, 8(4), 585-592 ...
format Dataset
author Fitzgerald, Paul G
author_facet Fitzgerald, Paul G
author_sort Fitzgerald, Paul G
title (Table 2) Apatite fission track results from sediment core CRP-3 ...
title_short (Table 2) Apatite fission track results from sediment core CRP-3 ...
title_full (Table 2) Apatite fission track results from sediment core CRP-3 ...
title_fullStr (Table 2) Apatite fission track results from sediment core CRP-3 ...
title_full_unstemmed (Table 2) Apatite fission track results from sediment core CRP-3 ...
title_sort (table 2) apatite fission track results from sediment core crp-3 ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.484981
https://doi.pangaea.de/10.1594/PANGAEA.484981
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.484981
_version_ 1810489848758272000