Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica
The Takaka Terrane of New Zealand’s South Island contains a Middle to early Late Cambrian intraoceanic island arc assemblage that consists of the terrigeneous to volcanogenic Haupiri Group sediments and the predominantly mafic Devil River Volcanics. Pb, Nd, and Sr isotopes, and major and trace eleme...
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ftoceanrep:oai:oceanrep.geomar.de:5838 2023-05-15T13:43:56+02:00 Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica Wombacher, Frank Münker, C. 2000 text https://oceanrep.geomar.de/id/eprint/5838/ https://oceanrep.geomar.de/id/eprint/5838/1/Wombacher.pdf en eng University of Chicago Press https://oceanrep.geomar.de/id/eprint/5838/1/Wombacher.pdf Wombacher, F. and Münker, C. (2000) Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica. Journal of Geology, 108 (6). pp. 663-686. info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2000 ftoceanrep 2023-04-07T14:51:46Z The Takaka Terrane of New Zealand’s South Island contains a Middle to early Late Cambrian intraoceanic island arc assemblage that consists of the terrigeneous to volcanogenic Haupiri Group sediments and the predominantly mafic Devil River Volcanics. Pb, Nd, and Sr isotopes, and major and trace element data are presented here for the Haupiri Group sediments. These data have implications for (1) the stratigraphy of the Takaka Terrane, (2) the reconstruction of the Cambrian Gondwana margin along Australia/Antarctica, and (3) geochemical and isotope provenance studies in general. Nd isotopes, Th/Sc, and rare earth elements (REE) show that the volcaniclastic components in the Haupiri Group sediments reflect the concomitant island arc and back‐arc volcanism. These sediments can probably be linked with the Early Cambrian Kanmantoo Group and Ordovician Lachlan Fold Belt sediments in SE Australia. To explain the Nd isotope compositions, published detrital zircon populations, and paleocurrent data, an Antarctic source with Grenvillian and Ross‐Delamerian age granitoids, as well as a significant portion of reprocessed Paleoproterozoic and/or Archean crust, is required. We adopt a bipolar subduction model for the Cambrian Gondwana margin along Australia/Antarctica and support the previous suggestion that the Cambrian arc assemblages of the Takaka Terrane of New Zealand and the Antarctic Bowers Terrane belong to the same arc system with a paleogeographical position offshore the Antarctic continent. Article in Journal/Newspaper Antarc* Antarctic Antarctica Antarctica Journal OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Antarctic Bowers ENVELOPE(164.083,164.083,-85.000,-85.000) New Zealand The Antarctic |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
The Takaka Terrane of New Zealand’s South Island contains a Middle to early Late Cambrian intraoceanic island arc assemblage that consists of the terrigeneous to volcanogenic Haupiri Group sediments and the predominantly mafic Devil River Volcanics. Pb, Nd, and Sr isotopes, and major and trace element data are presented here for the Haupiri Group sediments. These data have implications for (1) the stratigraphy of the Takaka Terrane, (2) the reconstruction of the Cambrian Gondwana margin along Australia/Antarctica, and (3) geochemical and isotope provenance studies in general. Nd isotopes, Th/Sc, and rare earth elements (REE) show that the volcaniclastic components in the Haupiri Group sediments reflect the concomitant island arc and back‐arc volcanism. These sediments can probably be linked with the Early Cambrian Kanmantoo Group and Ordovician Lachlan Fold Belt sediments in SE Australia. To explain the Nd isotope compositions, published detrital zircon populations, and paleocurrent data, an Antarctic source with Grenvillian and Ross‐Delamerian age granitoids, as well as a significant portion of reprocessed Paleoproterozoic and/or Archean crust, is required. We adopt a bipolar subduction model for the Cambrian Gondwana margin along Australia/Antarctica and support the previous suggestion that the Cambrian arc assemblages of the Takaka Terrane of New Zealand and the Antarctic Bowers Terrane belong to the same arc system with a paleogeographical position offshore the Antarctic continent. |
format |
Article in Journal/Newspaper |
author |
Wombacher, Frank Münker, C. |
spellingShingle |
Wombacher, Frank Münker, C. Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica |
author_facet |
Wombacher, Frank Münker, C. |
author_sort |
Wombacher, Frank |
title |
Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica |
title_short |
Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica |
title_full |
Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica |
title_fullStr |
Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica |
title_full_unstemmed |
Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica |
title_sort |
pb, nd and sr isotope and ree systematics of cambrian sediments from new zealand: implications for the reconstruction of the early paleozoic gondwana margin along australia and antarctica |
publisher |
University of Chicago Press |
publishDate |
2000 |
url |
https://oceanrep.geomar.de/id/eprint/5838/ https://oceanrep.geomar.de/id/eprint/5838/1/Wombacher.pdf |
long_lat |
ENVELOPE(164.083,164.083,-85.000,-85.000) |
geographic |
Antarctic Bowers New Zealand The Antarctic |
geographic_facet |
Antarctic Bowers New Zealand The Antarctic |
genre |
Antarc* Antarctic Antarctica Antarctica Journal |
genre_facet |
Antarc* Antarctic Antarctica Antarctica Journal |
op_relation |
https://oceanrep.geomar.de/id/eprint/5838/1/Wombacher.pdf Wombacher, F. and Münker, C. (2000) Pb, Nd and Sr isotope and REE systematics of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Paleozoic Gondwana margin along Australia and Antarctica. Journal of Geology, 108 (6). pp. 663-686. |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1766195212031361024 |