Geochemistry and Geochronology of Early Paleozoic Intrusive Rocks in the Terra Nova Bay Area, Northern Victoria Land, Antarctica
The Terra Nova Intrusive Complex (TNIC) in northern Victoria Land, Antarctica, results from widespread magmatism during the Early Paleozoic Ross Orogeny. According to field relationships, geochemistry, and geochronology data, the northern part of the TNIC comprises the Browning Intrusive Unit (BIU),...
Published in: | Minerals |
---|---|
Main Authors: | , , , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2021
|
Subjects: | |
Online Access: | https://doi.org/10.3390/min11070787 |
id |
ftmdpi:oai:mdpi.com:/2075-163X/11/7/787/ |
---|---|
record_format |
openpolar |
spelling |
ftmdpi:oai:mdpi.com:/2075-163X/11/7/787/ 2023-08-20T04:02:22+02:00 Geochemistry and Geochronology of Early Paleozoic Intrusive Rocks in the Terra Nova Bay Area, Northern Victoria Land, Antarctica Daeyeong Kim Sang-Bong Yi Hyeoncheol Kim Taehwan Kim Taehoon Kim Jong Ik Lee agris 2021-07-20 application/pdf https://doi.org/10.3390/min11070787 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/min11070787 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 11; Issue 7; Pages: 787 Ross Orogeny Terra Nova Intrusive Complex (TNIC) northern Victoria Land (NVL) zircon U-Pb age Sr-Nd isotopes Text 2021 ftmdpi https://doi.org/10.3390/min11070787 2023-08-01T02:13:59Z The Terra Nova Intrusive Complex (TNIC) in northern Victoria Land, Antarctica, results from widespread magmatism during the Early Paleozoic Ross Orogeny. According to field relationships, geochemistry, and geochronology data, the northern part of the TNIC comprises the Browning Intrusive Unit (BIU), which is associated with an arc crustal melting including migmatization of the Wilson Metamorphic Complex, and the later Campbell Intrusive Unit (CIU), which is attributed to the mantle and crustal melting processes. Zircon U-Pb ages suggest Late Neoproterozoic to Early Cambrian protolith with Late Cambrian metamorphism (502 ± 15 Ma) in the WMC, Late Cambrian formation (~500 Ma) of the BIU, and Early Ordovician formation (~480–470 Ma) of the CIU. Sr-Nd isotopic characteristics of the BIU indicate predominant crustal component (εNd(t) = −8.7 to −8.9), whereas those of the CIU reflect both mantle (εNd(t) = 1.8 to 1.6) and crustal (εNd(t) = −4.0 to −7.5) compositions. These results suggest that the northern TNIC magmatism occurring at ~500–470 Ma originated from partial melting of the mantle–mafic crust components and mixing with felsic crust components. By integrating the results with previous studies, the TNIC is considered to be formed by a combination of the mantle and mafic crust melting, crustal assimilation, felsic crust melting, and magma mixing during the Ross Orogeny. Text Antarc* Antarctica Victoria Land MDPI Open Access Publishing Victoria Land Terra Nova Bay Browning ENVELOPE(164.050,164.050,-74.617,-74.617) Minerals 11 7 787 |
institution |
Open Polar |
collection |
MDPI Open Access Publishing |
op_collection_id |
ftmdpi |
language |
English |
topic |
Ross Orogeny Terra Nova Intrusive Complex (TNIC) northern Victoria Land (NVL) zircon U-Pb age Sr-Nd isotopes |
spellingShingle |
Ross Orogeny Terra Nova Intrusive Complex (TNIC) northern Victoria Land (NVL) zircon U-Pb age Sr-Nd isotopes Daeyeong Kim Sang-Bong Yi Hyeoncheol Kim Taehwan Kim Taehoon Kim Jong Ik Lee Geochemistry and Geochronology of Early Paleozoic Intrusive Rocks in the Terra Nova Bay Area, Northern Victoria Land, Antarctica |
topic_facet |
Ross Orogeny Terra Nova Intrusive Complex (TNIC) northern Victoria Land (NVL) zircon U-Pb age Sr-Nd isotopes |
description |
The Terra Nova Intrusive Complex (TNIC) in northern Victoria Land, Antarctica, results from widespread magmatism during the Early Paleozoic Ross Orogeny. According to field relationships, geochemistry, and geochronology data, the northern part of the TNIC comprises the Browning Intrusive Unit (BIU), which is associated with an arc crustal melting including migmatization of the Wilson Metamorphic Complex, and the later Campbell Intrusive Unit (CIU), which is attributed to the mantle and crustal melting processes. Zircon U-Pb ages suggest Late Neoproterozoic to Early Cambrian protolith with Late Cambrian metamorphism (502 ± 15 Ma) in the WMC, Late Cambrian formation (~500 Ma) of the BIU, and Early Ordovician formation (~480–470 Ma) of the CIU. Sr-Nd isotopic characteristics of the BIU indicate predominant crustal component (εNd(t) = −8.7 to −8.9), whereas those of the CIU reflect both mantle (εNd(t) = 1.8 to 1.6) and crustal (εNd(t) = −4.0 to −7.5) compositions. These results suggest that the northern TNIC magmatism occurring at ~500–470 Ma originated from partial melting of the mantle–mafic crust components and mixing with felsic crust components. By integrating the results with previous studies, the TNIC is considered to be formed by a combination of the mantle and mafic crust melting, crustal assimilation, felsic crust melting, and magma mixing during the Ross Orogeny. |
format |
Text |
author |
Daeyeong Kim Sang-Bong Yi Hyeoncheol Kim Taehwan Kim Taehoon Kim Jong Ik Lee |
author_facet |
Daeyeong Kim Sang-Bong Yi Hyeoncheol Kim Taehwan Kim Taehoon Kim Jong Ik Lee |
author_sort |
Daeyeong Kim |
title |
Geochemistry and Geochronology of Early Paleozoic Intrusive Rocks in the Terra Nova Bay Area, Northern Victoria Land, Antarctica |
title_short |
Geochemistry and Geochronology of Early Paleozoic Intrusive Rocks in the Terra Nova Bay Area, Northern Victoria Land, Antarctica |
title_full |
Geochemistry and Geochronology of Early Paleozoic Intrusive Rocks in the Terra Nova Bay Area, Northern Victoria Land, Antarctica |
title_fullStr |
Geochemistry and Geochronology of Early Paleozoic Intrusive Rocks in the Terra Nova Bay Area, Northern Victoria Land, Antarctica |
title_full_unstemmed |
Geochemistry and Geochronology of Early Paleozoic Intrusive Rocks in the Terra Nova Bay Area, Northern Victoria Land, Antarctica |
title_sort |
geochemistry and geochronology of early paleozoic intrusive rocks in the terra nova bay area, northern victoria land, antarctica |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2021 |
url |
https://doi.org/10.3390/min11070787 |
op_coverage |
agris |
long_lat |
ENVELOPE(164.050,164.050,-74.617,-74.617) |
geographic |
Victoria Land Terra Nova Bay Browning |
geographic_facet |
Victoria Land Terra Nova Bay Browning |
genre |
Antarc* Antarctica Victoria Land |
genre_facet |
Antarc* Antarctica Victoria Land |
op_source |
Minerals; Volume 11; Issue 7; Pages: 787 |
op_relation |
https://dx.doi.org/10.3390/min11070787 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/min11070787 |
container_title |
Minerals |
container_volume |
11 |
container_issue |
7 |
container_start_page |
787 |
_version_ |
1774712794179960832 |