Mid-Neoproterozoic mafic rocks in the western Jiangnan orogen, South China: Intracontinental rifting or subduction?
Widely distributed Meso- to Neoproterozoic igneous rocks record the evolution of the Jiangnan orogen. We present integrated geochemical and geochronological data for basalts from the Gaoqiao area, northwestern Hunan Province. U-Pb dating of zircons indicates that the formation of Gaoqiao basalts occ...
Published in: | Journal of Asian Earth Sciences |
---|---|
Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
2019
|
Subjects: | |
Online Access: | https://doi.org/10.1016/j.jseaes.2019.104039 |
id |
ftcaltechauth:oai:authors.library.caltech.edu:s0svc-5h636 |
---|---|
record_format |
openpolar |
spelling |
ftcaltechauth:oai:authors.library.caltech.edu:s0svc-5h636 2024-10-13T14:01:57+00:00 Mid-Neoproterozoic mafic rocks in the western Jiangnan orogen, South China: Intracontinental rifting or subduction? Wan, Le Zeng, Zuoxun Asimow, Paul D. Zeng, Zhihui Peng, Lianhong Xu, Daliang Wei, Yunxu Liu, Wei Lu, Chengdong Chang, Wenqi 2019-11 https://doi.org/10.1016/j.jseaes.2019.104039 unknown Elsevier https://doi.org/10.1016/j.jseaes.2019.104039 eprintid:98790 info:eu-repo/semantics/closedAccess Other Journal of Asian Earth Sciences, 185, Art. No. 104039, (2019-11) South China Block Mid-Neoproterozoic Mafic rocks Western Jiangnan orogen Subduction-related magmatism Intracontinental rifting info:eu-repo/semantics/article 2019 ftcaltechauth https://doi.org/10.1016/j.jseaes.2019.104039 2024-09-25T18:46:40Z Widely distributed Meso- to Neoproterozoic igneous rocks record the evolution of the Jiangnan orogen. We present integrated geochemical and geochronological data for basalts from the Gaoqiao area, northwestern Hunan Province. U-Pb dating of zircons indicates that the formation of Gaoqiao basalts occurred in the Neoproterozoic, no earlier than 757 ± 16 Ma. Like the contemporaneous mafic rocks in neighboring areas, the Gaoqiao basalts show trace element characteristics suggesting derivation from a source similar to ocean-island basalts (OIBs), including strong enrichment in large-ion lithophile elements (LILEs), high-field strength elements (HFSEs) and TiO_2, and high Ti/Y ratios. Placed in a regional tectonic context, however, the Gaoqiao suite is most consistent with an intracontinental rift model and offers no support to the idea of ongoing subduction in middle-late Mid-Neoproterozoic time in the western Jiangnan orogen. Despite the coincidence between the age of this rift and the separation of East Antarctica-Australia from Laurentia, we argue that the rift recorded in the South China Block (SCB) was an independent and probably unrelated event during the break-up of the Rodinia supercontinent. © 2019 Elsevier Ltd. Received 29 March 2019, Revised 15 September 2019, Accepted 22 September 2019, Available online 23 September 2019. Article in Journal/Newspaper Antarc* Antarctica East Antarctica Ocean Island Caltech Authors (California Institute of Technology) East Antarctica Journal of Asian Earth Sciences 185 104039 |
institution |
Open Polar |
collection |
Caltech Authors (California Institute of Technology) |
op_collection_id |
ftcaltechauth |
language |
unknown |
topic |
South China Block Mid-Neoproterozoic Mafic rocks Western Jiangnan orogen Subduction-related magmatism Intracontinental rifting |
spellingShingle |
South China Block Mid-Neoproterozoic Mafic rocks Western Jiangnan orogen Subduction-related magmatism Intracontinental rifting Wan, Le Zeng, Zuoxun Asimow, Paul D. Zeng, Zhihui Peng, Lianhong Xu, Daliang Wei, Yunxu Liu, Wei Lu, Chengdong Chang, Wenqi Mid-Neoproterozoic mafic rocks in the western Jiangnan orogen, South China: Intracontinental rifting or subduction? |
topic_facet |
South China Block Mid-Neoproterozoic Mafic rocks Western Jiangnan orogen Subduction-related magmatism Intracontinental rifting |
description |
Widely distributed Meso- to Neoproterozoic igneous rocks record the evolution of the Jiangnan orogen. We present integrated geochemical and geochronological data for basalts from the Gaoqiao area, northwestern Hunan Province. U-Pb dating of zircons indicates that the formation of Gaoqiao basalts occurred in the Neoproterozoic, no earlier than 757 ± 16 Ma. Like the contemporaneous mafic rocks in neighboring areas, the Gaoqiao basalts show trace element characteristics suggesting derivation from a source similar to ocean-island basalts (OIBs), including strong enrichment in large-ion lithophile elements (LILEs), high-field strength elements (HFSEs) and TiO_2, and high Ti/Y ratios. Placed in a regional tectonic context, however, the Gaoqiao suite is most consistent with an intracontinental rift model and offers no support to the idea of ongoing subduction in middle-late Mid-Neoproterozoic time in the western Jiangnan orogen. Despite the coincidence between the age of this rift and the separation of East Antarctica-Australia from Laurentia, we argue that the rift recorded in the South China Block (SCB) was an independent and probably unrelated event during the break-up of the Rodinia supercontinent. © 2019 Elsevier Ltd. Received 29 March 2019, Revised 15 September 2019, Accepted 22 September 2019, Available online 23 September 2019. |
format |
Article in Journal/Newspaper |
author |
Wan, Le Zeng, Zuoxun Asimow, Paul D. Zeng, Zhihui Peng, Lianhong Xu, Daliang Wei, Yunxu Liu, Wei Lu, Chengdong Chang, Wenqi |
author_facet |
Wan, Le Zeng, Zuoxun Asimow, Paul D. Zeng, Zhihui Peng, Lianhong Xu, Daliang Wei, Yunxu Liu, Wei Lu, Chengdong Chang, Wenqi |
author_sort |
Wan, Le |
title |
Mid-Neoproterozoic mafic rocks in the western Jiangnan orogen, South China: Intracontinental rifting or subduction? |
title_short |
Mid-Neoproterozoic mafic rocks in the western Jiangnan orogen, South China: Intracontinental rifting or subduction? |
title_full |
Mid-Neoproterozoic mafic rocks in the western Jiangnan orogen, South China: Intracontinental rifting or subduction? |
title_fullStr |
Mid-Neoproterozoic mafic rocks in the western Jiangnan orogen, South China: Intracontinental rifting or subduction? |
title_full_unstemmed |
Mid-Neoproterozoic mafic rocks in the western Jiangnan orogen, South China: Intracontinental rifting or subduction? |
title_sort |
mid-neoproterozoic mafic rocks in the western jiangnan orogen, south china: intracontinental rifting or subduction? |
publisher |
Elsevier |
publishDate |
2019 |
url |
https://doi.org/10.1016/j.jseaes.2019.104039 |
geographic |
East Antarctica |
geographic_facet |
East Antarctica |
genre |
Antarc* Antarctica East Antarctica Ocean Island |
genre_facet |
Antarc* Antarctica East Antarctica Ocean Island |
op_source |
Journal of Asian Earth Sciences, 185, Art. No. 104039, (2019-11) |
op_relation |
https://doi.org/10.1016/j.jseaes.2019.104039 eprintid:98790 |
op_rights |
info:eu-repo/semantics/closedAccess Other |
op_doi |
https://doi.org/10.1016/j.jseaes.2019.104039 |
container_title |
Journal of Asian Earth Sciences |
container_volume |
185 |
container_start_page |
104039 |
_version_ |
1812813879603888128 |