Reconnaissance Pb-Pb dating of single mineral phases by the step-leaching method: results from the Caledonides of East Greenland

Reconnaissance Pb-Pb step-leaching analyses have been carried out on garnet and kyanite from the Krummedal supracrustal sequence in East Greenland, yielding respectively Neoproterozoic and Caledonian ages. These data support previous analyses suggesting that the Krummedal supracrustal sequence, wide...

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Published in:Geological Survey of Denmark and Greenland (GEUS) Bulletin
Main Author: Thrane, Kristine
Format: Article in Journal/Newspaper
Language:English
Published: Geological Survey of Denmark and Greenland (GEUS) 2004
Subjects:
Online Access:https://geusbulletin.org/index.php/geusb/article/view/4819
https://doi.org/10.34194/geusb.v6.4819
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spelling ftjgeusbullet:oai:geusjournals.org:article/4819 2023-05-15T16:03:14+02:00 Reconnaissance Pb-Pb dating of single mineral phases by the step-leaching method: results from the Caledonides of East Greenland Thrane, Kristine 2004-12-30 application/pdf https://geusbulletin.org/index.php/geusb/article/view/4819 https://doi.org/10.34194/geusb.v6.4819 eng eng Geological Survey of Denmark and Greenland (GEUS) https://geusbulletin.org/index.php/geusb/article/view/4819/10455 https://geusbulletin.org/index.php/geusb/article/view/4819 doi:10.34194/geusb.v6.4819 GEUS Bulletin; Vol. 6 (2004): East Greenland Caledonides, stratigraphy, structure and geochronology; 67-76 2597-2154 2597-2162 Caledonian East Greenland geochronology Neoproterozoic step-leaching info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article. 2004 ftjgeusbullet https://doi.org/10.34194/geusb.v6.4819 2022-03-15T17:22:15Z Reconnaissance Pb-Pb step-leaching analyses have been carried out on garnet and kyanite from the Krummedal supracrustal sequence in East Greenland, yielding respectively Neoproterozoic and Caledonian ages. These data support previous analyses suggesting that the Krummedal supracrustal sequence, widespread in southern parts of the East Greenland Caledonides, was affected by both an early Neoproterozoic and a Caledonian thermal event. Titanite and apatite fractions from the underlying crystalline basement rocks were analysed in order to obtain metamorphic ages, as a contrast and supplement to the numerous existing protolith ages on orthogneisses. The titanite yielded a date of 486 ± 15 Ma which, if interpreted as a true age, is older than the usual range of Caledonian ages in East Greenland. The significance of this date is uncertain, but one possibility is that it reflects extension and subsidence taking place prior to Caledonian collision. The apatite, in contrast, yielded a very young Caledonian date of 392 ± 24 Ma that may reflect the cooling of the basement gneisses to < 500°C subsequent to collision. Article in Journal/Newspaper East Greenland Greenland GEUS Bulletin (Geological Survey of Denmark and Greenland) Greenland Geological Survey of Denmark and Greenland (GEUS) Bulletin 6 67 76
institution Open Polar
collection GEUS Bulletin (Geological Survey of Denmark and Greenland)
op_collection_id ftjgeusbullet
language English
topic Caledonian
East Greenland
geochronology
Neoproterozoic
step-leaching
spellingShingle Caledonian
East Greenland
geochronology
Neoproterozoic
step-leaching
Thrane, Kristine
Reconnaissance Pb-Pb dating of single mineral phases by the step-leaching method: results from the Caledonides of East Greenland
topic_facet Caledonian
East Greenland
geochronology
Neoproterozoic
step-leaching
description Reconnaissance Pb-Pb step-leaching analyses have been carried out on garnet and kyanite from the Krummedal supracrustal sequence in East Greenland, yielding respectively Neoproterozoic and Caledonian ages. These data support previous analyses suggesting that the Krummedal supracrustal sequence, widespread in southern parts of the East Greenland Caledonides, was affected by both an early Neoproterozoic and a Caledonian thermal event. Titanite and apatite fractions from the underlying crystalline basement rocks were analysed in order to obtain metamorphic ages, as a contrast and supplement to the numerous existing protolith ages on orthogneisses. The titanite yielded a date of 486 ± 15 Ma which, if interpreted as a true age, is older than the usual range of Caledonian ages in East Greenland. The significance of this date is uncertain, but one possibility is that it reflects extension and subsidence taking place prior to Caledonian collision. The apatite, in contrast, yielded a very young Caledonian date of 392 ± 24 Ma that may reflect the cooling of the basement gneisses to < 500°C subsequent to collision.
format Article in Journal/Newspaper
author Thrane, Kristine
author_facet Thrane, Kristine
author_sort Thrane, Kristine
title Reconnaissance Pb-Pb dating of single mineral phases by the step-leaching method: results from the Caledonides of East Greenland
title_short Reconnaissance Pb-Pb dating of single mineral phases by the step-leaching method: results from the Caledonides of East Greenland
title_full Reconnaissance Pb-Pb dating of single mineral phases by the step-leaching method: results from the Caledonides of East Greenland
title_fullStr Reconnaissance Pb-Pb dating of single mineral phases by the step-leaching method: results from the Caledonides of East Greenland
title_full_unstemmed Reconnaissance Pb-Pb dating of single mineral phases by the step-leaching method: results from the Caledonides of East Greenland
title_sort reconnaissance pb-pb dating of single mineral phases by the step-leaching method: results from the caledonides of east greenland
publisher Geological Survey of Denmark and Greenland (GEUS)
publishDate 2004
url https://geusbulletin.org/index.php/geusb/article/view/4819
https://doi.org/10.34194/geusb.v6.4819
geographic Greenland
geographic_facet Greenland
genre East Greenland
Greenland
genre_facet East Greenland
Greenland
op_source GEUS Bulletin; Vol. 6 (2004): East Greenland Caledonides, stratigraphy, structure and geochronology; 67-76
2597-2154
2597-2162
op_relation https://geusbulletin.org/index.php/geusb/article/view/4819/10455
https://geusbulletin.org/index.php/geusb/article/view/4819
doi:10.34194/geusb.v6.4819
op_doi https://doi.org/10.34194/geusb.v6.4819
container_title Geological Survey of Denmark and Greenland (GEUS) Bulletin
container_volume 6
container_start_page 67
op_container_end_page 76
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