K-Ar data for whole-rock basalts at ODP Hole 105-647A (Table 1)
Alteration of basalt samples in the basement rocks of Site 647 produced a range of K-Ar ages from 35 to 71 Ma. Microprobe data indicate that an alteration phase contributes nearly 50% of the potassium in the samples. Thus, a component with uncertain argon-retention characteristics is considered resp...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.745269 2024-09-15T18:23:16+00:00 K-Ar data for whole-rock basalts at ODP Hole 105-647A (Table 1) Roddick, J C LATITUDE: 53.331300 * LONGITUDE: -45.262000 * DATE/TIME START: 1985-10-15T04:10:00 * DATE/TIME END: 1985-10-23T18:15:00 * MINIMUM DEPTH, sediment/rock: 704 m * MAXIMUM DEPTH, sediment/rock: 736 m 1989 text/tab-separated-values, 56 data points https://doi.pangaea.de/10.1594/PANGAEA.745269 https://doi.org/10.1594/PANGAEA.745269 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.745269 https://doi.org/10.1594/PANGAEA.745269 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Roddick, J C (1989): K-Ar dating of basalts from Site 647, Ocean Drilling Program Leg 105. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 885-887, https://doi.org/10.2973/odp.proc.sr.105.176.1989 105-647A Age dated dated standard deviation Argon-40 DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg105 North Atlantic Ocean Ocean Drilling Program ODP Potassium standard deviation Sample code/label Sample code/label 2 dataset 1989 ftpangaea https://doi.org/10.1594/PANGAEA.74526910.2973/odp.proc.sr.105.176.1989 2024-08-21T00:02:26Z Alteration of basalt samples in the basement rocks of Site 647 produced a range of K-Ar ages from 35 to 71 Ma. Microprobe data indicate that an alteration phase contributes nearly 50% of the potassium in the samples. Thus, a component with uncertain argon-retention characteristics is considered responsible for the range of ages. While the older ages are consistent with the expected magnetic anomaly age and the fossil evidence, the presence of the alteration makes these ages unreliable for defining the age of the basaltic crust. Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-45.262000,-45.262000,53.331300,53.331300) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
105-647A Age dated dated standard deviation Argon-40 DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg105 North Atlantic Ocean Ocean Drilling Program ODP Potassium standard deviation Sample code/label Sample code/label 2 |
spellingShingle |
105-647A Age dated dated standard deviation Argon-40 DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg105 North Atlantic Ocean Ocean Drilling Program ODP Potassium standard deviation Sample code/label Sample code/label 2 Roddick, J C K-Ar data for whole-rock basalts at ODP Hole 105-647A (Table 1) |
topic_facet |
105-647A Age dated dated standard deviation Argon-40 DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg105 North Atlantic Ocean Ocean Drilling Program ODP Potassium standard deviation Sample code/label Sample code/label 2 |
description |
Alteration of basalt samples in the basement rocks of Site 647 produced a range of K-Ar ages from 35 to 71 Ma. Microprobe data indicate that an alteration phase contributes nearly 50% of the potassium in the samples. Thus, a component with uncertain argon-retention characteristics is considered responsible for the range of ages. While the older ages are consistent with the expected magnetic anomaly age and the fossil evidence, the presence of the alteration makes these ages unreliable for defining the age of the basaltic crust. |
format |
Dataset |
author |
Roddick, J C |
author_facet |
Roddick, J C |
author_sort |
Roddick, J C |
title |
K-Ar data for whole-rock basalts at ODP Hole 105-647A (Table 1) |
title_short |
K-Ar data for whole-rock basalts at ODP Hole 105-647A (Table 1) |
title_full |
K-Ar data for whole-rock basalts at ODP Hole 105-647A (Table 1) |
title_fullStr |
K-Ar data for whole-rock basalts at ODP Hole 105-647A (Table 1) |
title_full_unstemmed |
K-Ar data for whole-rock basalts at ODP Hole 105-647A (Table 1) |
title_sort |
k-ar data for whole-rock basalts at odp hole 105-647a (table 1) |
publisher |
PANGAEA |
publishDate |
1989 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.745269 https://doi.org/10.1594/PANGAEA.745269 |
op_coverage |
LATITUDE: 53.331300 * LONGITUDE: -45.262000 * DATE/TIME START: 1985-10-15T04:10:00 * DATE/TIME END: 1985-10-23T18:15:00 * MINIMUM DEPTH, sediment/rock: 704 m * MAXIMUM DEPTH, sediment/rock: 736 m |
long_lat |
ENVELOPE(-45.262000,-45.262000,53.331300,53.331300) |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Supplement to: Roddick, J C (1989): K-Ar dating of basalts from Site 647, Ocean Drilling Program Leg 105. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 885-887, https://doi.org/10.2973/odp.proc.sr.105.176.1989 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.745269 https://doi.org/10.1594/PANGAEA.745269 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.74526910.2973/odp.proc.sr.105.176.1989 |
_version_ |
1810463441495785472 |