Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond
Highlights • Common HIMU end member in adjacent continental and oceanic volcanic provinces. • End member St. Helena HIMU derived from deep upwelling(s)/plume(s). • Plateau collision & plume interaction with Gondwana active margin causes breakup. • Hybrid volcanic-tectonic margins resulted from Z...
Published in: | Earth and Planetary Science Letters |
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Online Access: | https://oceanrep.geomar.de/id/eprint/47962/ https://oceanrep.geomar.de/id/eprint/47962/1/Hoernle%20et.al.pdf https://oceanrep.geomar.de/id/eprint/47962/6/ScienceDirect_files_14Oct2019_07-35-04.575.zip https://oceanrep.geomar.de/id/eprint/47962/8/Hoernle_EPSL_CretNZ_PrePrint.pdf https://doi.org/10.1016/j.epsl.2019.115864 |
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ftoceanrep:oai:oceanrep.geomar.de:47962 2023-05-15T13:37:45+02:00 Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond Hoernle, Kaj Timm, Christian Hauff, Folkmar Tappenden, V. Werner, Reinhard Jolis, Ester Mortimer, N. Weaver, S. Riefstahl, F. Gohl, K. 2020-01-01 text archive https://oceanrep.geomar.de/id/eprint/47962/ https://oceanrep.geomar.de/id/eprint/47962/1/Hoernle%20et.al.pdf https://oceanrep.geomar.de/id/eprint/47962/6/ScienceDirect_files_14Oct2019_07-35-04.575.zip https://oceanrep.geomar.de/id/eprint/47962/8/Hoernle_EPSL_CretNZ_PrePrint.pdf https://doi.org/10.1016/j.epsl.2019.115864 en eng Elsevier https://oceanrep.geomar.de/id/eprint/47962/1/Hoernle%20et.al.pdf https://oceanrep.geomar.de/id/eprint/47962/6/ScienceDirect_files_14Oct2019_07-35-04.575.zip https://oceanrep.geomar.de/id/eprint/47962/8/Hoernle_EPSL_CretNZ_PrePrint.pdf Hoernle, K. , Timm, C. , Hauff, F. , Tappenden, V., Werner, R., Jolis, E., Mortimer, N., Weaver, S., Riefstahl, F. and Gohl, K. (2020) Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond. Open Access Earth and Planetary Science Letters, 529 (Article number 115864). DOI 10.1016/j.epsl.2019.115864 <https://doi.org/10.1016/j.epsl.2019.115864>. doi:10.1016/j.epsl.2019.115864 info:eu-repo/semantics/openAccess Article PeerReviewed info:eu-repo/semantics/article 2020 ftoceanrep https://doi.org/10.1016/j.epsl.2019.115864 2023-04-07T15:47:44Z Highlights • Common HIMU end member in adjacent continental and oceanic volcanic provinces. • End member St. Helena HIMU derived from deep upwelling(s)/plume(s). • Plateau collision & plume interaction with Gondwana active margin causes breakup. • Hybrid volcanic-tectonic margins resulted from Zealandia – Antarctica breakup. Abstract Margins resulting from continental breakup are generally classified as volcanic (related to flood basalt volcanism from a starting plume head) or non-volcanic (caused by tectonic processes), but many margins (breakups) may actually be hybrids caused by a combination of volcanic and tectonic processes. It has been postulated that the collision of the Hikurangi Plateau with the Gondwana margin ∼110 Ma ago caused subduction to cease, followed by large-scale extension and ultimately breakoff of the Zealandia micro-continent from West Antarctica through seafloor spreading which started at ∼85 Ma. Here we report new geochemical (major and trace element and Sr-Nd-Pb-Hf isotope) data for Late Cretaceous (99-69 Ma) volcanism from Zealandia, which include the calc-alkalic, subduction-related Mount Somers (99-96 Ma) and four intraplate igneous provinces: 1) Hikurangi Seamount Province (99-88 Ma), 2) Marlborough Igneous Province (98-94 Ma), 3) Westland Igneous Province (92-69 Ma), and 4) Eastern Chatham Igneous Province (86-79 Ma). Each of the intraplate provinces forms mixing arrays on incompatible-element and isotope ratio plots between HIMU (requiring long-term high U/204Pb) and either a depleted (MORB-source) upper mantle (DM) component or enriched continental (EM) type component (located in the crust and/or upper mantle) or a mixture of both. St. Helena end member HIMU could be the common component in all four provinces. Considering the uniformity in composition of the HIMU end member despite the type of lithosphere (continental, oceanic, oceanic plateau) beneath the igneous provinces, we attribute this component to a sublithospheric source, located beneath all volcanic provinces, and ... Article in Journal/Newspaper Antarc* Antarctica West Antarctica OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) St. Helena ENVELOPE(8.575,8.575,63.621,63.621) West Antarctica Earth and Planetary Science Letters 529 115864 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Highlights • Common HIMU end member in adjacent continental and oceanic volcanic provinces. • End member St. Helena HIMU derived from deep upwelling(s)/plume(s). • Plateau collision & plume interaction with Gondwana active margin causes breakup. • Hybrid volcanic-tectonic margins resulted from Zealandia – Antarctica breakup. Abstract Margins resulting from continental breakup are generally classified as volcanic (related to flood basalt volcanism from a starting plume head) or non-volcanic (caused by tectonic processes), but many margins (breakups) may actually be hybrids caused by a combination of volcanic and tectonic processes. It has been postulated that the collision of the Hikurangi Plateau with the Gondwana margin ∼110 Ma ago caused subduction to cease, followed by large-scale extension and ultimately breakoff of the Zealandia micro-continent from West Antarctica through seafloor spreading which started at ∼85 Ma. Here we report new geochemical (major and trace element and Sr-Nd-Pb-Hf isotope) data for Late Cretaceous (99-69 Ma) volcanism from Zealandia, which include the calc-alkalic, subduction-related Mount Somers (99-96 Ma) and four intraplate igneous provinces: 1) Hikurangi Seamount Province (99-88 Ma), 2) Marlborough Igneous Province (98-94 Ma), 3) Westland Igneous Province (92-69 Ma), and 4) Eastern Chatham Igneous Province (86-79 Ma). Each of the intraplate provinces forms mixing arrays on incompatible-element and isotope ratio plots between HIMU (requiring long-term high U/204Pb) and either a depleted (MORB-source) upper mantle (DM) component or enriched continental (EM) type component (located in the crust and/or upper mantle) or a mixture of both. St. Helena end member HIMU could be the common component in all four provinces. Considering the uniformity in composition of the HIMU end member despite the type of lithosphere (continental, oceanic, oceanic plateau) beneath the igneous provinces, we attribute this component to a sublithospheric source, located beneath all volcanic provinces, and ... |
format |
Article in Journal/Newspaper |
author |
Hoernle, Kaj Timm, Christian Hauff, Folkmar Tappenden, V. Werner, Reinhard Jolis, Ester Mortimer, N. Weaver, S. Riefstahl, F. Gohl, K. |
spellingShingle |
Hoernle, Kaj Timm, Christian Hauff, Folkmar Tappenden, V. Werner, Reinhard Jolis, Ester Mortimer, N. Weaver, S. Riefstahl, F. Gohl, K. Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond |
author_facet |
Hoernle, Kaj Timm, Christian Hauff, Folkmar Tappenden, V. Werner, Reinhard Jolis, Ester Mortimer, N. Weaver, S. Riefstahl, F. Gohl, K. |
author_sort |
Hoernle, Kaj |
title |
Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond |
title_short |
Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond |
title_full |
Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond |
title_fullStr |
Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond |
title_full_unstemmed |
Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond |
title_sort |
late cretaceous (99-69 ma) basaltic intraplate volcanism on and around zealandia: tracing upper mantle geodynamics from hikurangi plateau collision to gondwana breakup and beyond |
publisher |
Elsevier |
publishDate |
2020 |
url |
https://oceanrep.geomar.de/id/eprint/47962/ https://oceanrep.geomar.de/id/eprint/47962/1/Hoernle%20et.al.pdf https://oceanrep.geomar.de/id/eprint/47962/6/ScienceDirect_files_14Oct2019_07-35-04.575.zip https://oceanrep.geomar.de/id/eprint/47962/8/Hoernle_EPSL_CretNZ_PrePrint.pdf https://doi.org/10.1016/j.epsl.2019.115864 |
long_lat |
ENVELOPE(8.575,8.575,63.621,63.621) |
geographic |
St. Helena West Antarctica |
geographic_facet |
St. Helena West Antarctica |
genre |
Antarc* Antarctica West Antarctica |
genre_facet |
Antarc* Antarctica West Antarctica |
op_relation |
https://oceanrep.geomar.de/id/eprint/47962/1/Hoernle%20et.al.pdf https://oceanrep.geomar.de/id/eprint/47962/6/ScienceDirect_files_14Oct2019_07-35-04.575.zip https://oceanrep.geomar.de/id/eprint/47962/8/Hoernle_EPSL_CretNZ_PrePrint.pdf Hoernle, K. , Timm, C. , Hauff, F. , Tappenden, V., Werner, R., Jolis, E., Mortimer, N., Weaver, S., Riefstahl, F. and Gohl, K. (2020) Late Cretaceous (99-69 Ma) basaltic intraplate volcanism on and around Zealandia: Tracing upper mantle geodynamics from Hikurangi Plateau collision to Gondwana breakup and beyond. Open Access Earth and Planetary Science Letters, 529 (Article number 115864). DOI 10.1016/j.epsl.2019.115864 <https://doi.org/10.1016/j.epsl.2019.115864>. doi:10.1016/j.epsl.2019.115864 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1016/j.epsl.2019.115864 |
container_title |
Earth and Planetary Science Letters |
container_volume |
529 |
container_start_page |
115864 |
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1766097360499245056 |