Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica
Previous mapping of granitoid rocks in the Dry Valleys area of southern Victoria Land, Antarctica, identified the calc‐alkaline (DV1a), adakitic (DV1b), and monzonitic (DV2) suites. A fourth older suite comprising alkaline gabbro, syenite, and A‐type granite occurs in the Mt Dromedary area c. 80 km...
Published in: | New Zealand Journal of Geology and Geophysics |
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Taylor & Francis
2000
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Online Access: | https://researchonline.jcu.edu.au/12972/1/12972_Cox_2000.pdf |
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ftjamescook:oai:researchonline.jcu.edu.au:12972 2024-02-11T09:56:18+01:00 Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica Cox, Simon C. Parkinson, David L. Allibone, Andrew H. Cooper, Alan F. 2000 application/pdf https://researchonline.jcu.edu.au/12972/1/12972_Cox_2000.pdf unknown Taylor & Francis http://dx.doi.org/10.1080/00288306.2000.9514906 https://researchonline.jcu.edu.au/12972/ https://researchonline.jcu.edu.au/12972/1/12972_Cox_2000.pdf Cox, Simon C., Parkinson, David L., Allibone, Andrew H., and Cooper, Alan F. (2000) Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, 43 (4). pp. 501-520. restricted Article PeerReviewed 2000 ftjamescook https://doi.org/10.1080/00288306.2000.9514906 2024-01-15T23:26:53Z Previous mapping of granitoid rocks in the Dry Valleys area of southern Victoria Land, Antarctica, identified the calc‐alkaline (DV1a), adakitic (DV1b), and monzonitic (DV2) suites. A fourth older suite comprising alkaline gabbro, syenite, and A‐type granite occurs in the Mt Dromedary area c. 80 km to the south. U‐Pb zircon dating of Bonney Pluton, the largest calc‐alkaline DV1a intrusion, indicates emplacement of this regional‐scale body at 505 ± 2 Ma. Pb‐loss and inherited zircon were common to Bonney Pluton analyses of this study. U‐Pb dating of monazite from Valhalla Pluton, a principal DV1b suite adakitic intrusion, indicates emplacement at 488 ± 2 Ma. The Bonney Pluton age constrains the peak of calc‐alkaline plutonism at 505 Ma and the Valhalla Pluton age records the major pulse of adakitic plutonism that is inferred to mark the final stages of subduction c. 490 Ma along this section of the East Antarctic margin. Nd and Sr isotope data for the calc‐alkaline DV1a suite and adakitic DV1b suite define distinct ranges for each suite, supporting their subdivision on the basis of field relationships, petrography, and whole‐rock geochemistry. Calc‐alkaline DV1a suite granite magmas have ϵNd(T) = ‐4–2 to ‐6.1 and Srᵢ = 0.7071–0.7079, whereas the adakitic DV1b suite rocks have a wider range of ϵNd(T) = ‐1.9 to ‐7.2 and Srᵢ = 0.7065–0.7097. The isotopic data suggest a significant mantle component and subordinate crustal component in the source region of both suites. Time‐dependent variations in the isotopic ratios of DV1a and DV1b suites imply a progressive increase in the proportion of more radiogenic material in the source region of the granitoid rocks, either mantle‐ or crust‐derived material. Larger adakitic DV1b plutons are more “evolved” than equivalent, smaller plutons of the same DV1b suite. Vanda Dikes and monzonitic DV2 suite intrusions are characterised by particularly low Srᵢ = 0.7044–0.7067 and near‐constant ϵNd(T) = ‐4.8 to ‐5.3, which indicate a petrogenesis for these younger intrusions distinct from ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Victoria Land James Cook University, Australia: ResearchOnline@JCU Antarctic Bonney ENVELOPE(162.417,162.417,-77.717,-77.717) Dromedary ENVELOPE(163.033,163.033,-78.317,-78.317) Valhalla ENVELOPE(161.933,161.933,-77.583,-77.583) Vanda ENVELOPE(161.550,161.550,-77.533,-77.533) Victoria Land New Zealand Journal of Geology and Geophysics 43 4 501 520 |
institution |
Open Polar |
collection |
James Cook University, Australia: ResearchOnline@JCU |
op_collection_id |
ftjamescook |
language |
unknown |
description |
Previous mapping of granitoid rocks in the Dry Valleys area of southern Victoria Land, Antarctica, identified the calc‐alkaline (DV1a), adakitic (DV1b), and monzonitic (DV2) suites. A fourth older suite comprising alkaline gabbro, syenite, and A‐type granite occurs in the Mt Dromedary area c. 80 km to the south. U‐Pb zircon dating of Bonney Pluton, the largest calc‐alkaline DV1a intrusion, indicates emplacement of this regional‐scale body at 505 ± 2 Ma. Pb‐loss and inherited zircon were common to Bonney Pluton analyses of this study. U‐Pb dating of monazite from Valhalla Pluton, a principal DV1b suite adakitic intrusion, indicates emplacement at 488 ± 2 Ma. The Bonney Pluton age constrains the peak of calc‐alkaline plutonism at 505 Ma and the Valhalla Pluton age records the major pulse of adakitic plutonism that is inferred to mark the final stages of subduction c. 490 Ma along this section of the East Antarctic margin. Nd and Sr isotope data for the calc‐alkaline DV1a suite and adakitic DV1b suite define distinct ranges for each suite, supporting their subdivision on the basis of field relationships, petrography, and whole‐rock geochemistry. Calc‐alkaline DV1a suite granite magmas have ϵNd(T) = ‐4–2 to ‐6.1 and Srᵢ = 0.7071–0.7079, whereas the adakitic DV1b suite rocks have a wider range of ϵNd(T) = ‐1.9 to ‐7.2 and Srᵢ = 0.7065–0.7097. The isotopic data suggest a significant mantle component and subordinate crustal component in the source region of both suites. Time‐dependent variations in the isotopic ratios of DV1a and DV1b suites imply a progressive increase in the proportion of more radiogenic material in the source region of the granitoid rocks, either mantle‐ or crust‐derived material. Larger adakitic DV1b plutons are more “evolved” than equivalent, smaller plutons of the same DV1b suite. Vanda Dikes and monzonitic DV2 suite intrusions are characterised by particularly low Srᵢ = 0.7044–0.7067 and near‐constant ϵNd(T) = ‐4.8 to ‐5.3, which indicate a petrogenesis for these younger intrusions distinct from ... |
format |
Article in Journal/Newspaper |
author |
Cox, Simon C. Parkinson, David L. Allibone, Andrew H. Cooper, Alan F. |
spellingShingle |
Cox, Simon C. Parkinson, David L. Allibone, Andrew H. Cooper, Alan F. Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica |
author_facet |
Cox, Simon C. Parkinson, David L. Allibone, Andrew H. Cooper, Alan F. |
author_sort |
Cox, Simon C. |
title |
Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica |
title_short |
Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica |
title_full |
Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica |
title_fullStr |
Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica |
title_full_unstemmed |
Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica |
title_sort |
isotopic character of cambro-ordovician plutonism, southern victoria land, antarctica |
publisher |
Taylor & Francis |
publishDate |
2000 |
url |
https://researchonline.jcu.edu.au/12972/1/12972_Cox_2000.pdf |
long_lat |
ENVELOPE(162.417,162.417,-77.717,-77.717) ENVELOPE(163.033,163.033,-78.317,-78.317) ENVELOPE(161.933,161.933,-77.583,-77.583) ENVELOPE(161.550,161.550,-77.533,-77.533) |
geographic |
Antarctic Bonney Dromedary Valhalla Vanda Victoria Land |
geographic_facet |
Antarctic Bonney Dromedary Valhalla Vanda Victoria Land |
genre |
Antarc* Antarctic Antarctica Victoria Land |
genre_facet |
Antarc* Antarctic Antarctica Victoria Land |
op_relation |
http://dx.doi.org/10.1080/00288306.2000.9514906 https://researchonline.jcu.edu.au/12972/ https://researchonline.jcu.edu.au/12972/1/12972_Cox_2000.pdf Cox, Simon C., Parkinson, David L., Allibone, Andrew H., and Cooper, Alan F. (2000) Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, 43 (4). pp. 501-520. |
op_rights |
restricted |
op_doi |
https://doi.org/10.1080/00288306.2000.9514906 |
container_title |
New Zealand Journal of Geology and Geophysics |
container_volume |
43 |
container_issue |
4 |
container_start_page |
501 |
op_container_end_page |
520 |
_version_ |
1790602070216146944 |