Himalayan zircons resurface in Sumatran arc volcanoes through sediment recycling
Eocene to Oligocene age Himalayan zircons were transported through the Bengal submarine channel, subducted in the Sunda trench, and resurfaced in the arc volcanoes of Sumatra, according to U-Pb-Hf-O isotopes from arc basalts and andesites
Main Authors: | , , , , , , , |
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Format: | Article |
Language: | English |
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Nature Portfolio
2022-11-01
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Series: | Communications Earth & Environment |
Online Access: | https://doi.org/10.1038/s43247-022-00611-6 |
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author | Meng-Hao Gao Ping-Ping Liu Sun-Lin Chung Qiu-Li Li Bin Wang Wei Tian Xian-Hua Li Hao-Yang Lee |
author_facet | Meng-Hao Gao Ping-Ping Liu Sun-Lin Chung Qiu-Li Li Bin Wang Wei Tian Xian-Hua Li Hao-Yang Lee |
author_sort | Meng-Hao Gao |
collection | DOAJ |
description | Eocene to Oligocene age Himalayan zircons were transported through the Bengal submarine channel, subducted in the Sunda trench, and resurfaced in the arc volcanoes of Sumatra, according to U-Pb-Hf-O isotopes from arc basalts and andesites |
first_indexed | 2024-04-12T07:25:47Z |
format | Article |
id | doaj.art-32de944e9fae4b59b406befd1d7ed952 |
institution | Directory Open Access Journal |
issn | 2662-4435 |
language | English |
last_indexed | 2024-04-12T07:25:47Z |
publishDate | 2022-11-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Communications Earth & Environment |
spelling | doaj.art-32de944e9fae4b59b406befd1d7ed9522022-12-22T03:42:12ZengNature PortfolioCommunications Earth & Environment2662-44352022-11-013111110.1038/s43247-022-00611-6Himalayan zircons resurface in Sumatran arc volcanoes through sediment recyclingMeng-Hao Gao0Ping-Ping Liu1Sun-Lin Chung2Qiu-Li Li3Bin Wang4Wei Tian5Xian-Hua Li6Hao-Yang Lee7Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking UniversityKey Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking UniversityInstitute of Earth Sciences, Academia SinicaInstitute of Geology and Geophysics, Chinese Academy of SciencesKey Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking UniversityKey Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking UniversityInstitute of Geology and Geophysics, Chinese Academy of SciencesInstitute of Earth Sciences, Academia SinicaEocene to Oligocene age Himalayan zircons were transported through the Bengal submarine channel, subducted in the Sunda trench, and resurfaced in the arc volcanoes of Sumatra, according to U-Pb-Hf-O isotopes from arc basalts and andesiteshttps://doi.org/10.1038/s43247-022-00611-6 |
spellingShingle | Meng-Hao Gao Ping-Ping Liu Sun-Lin Chung Qiu-Li Li Bin Wang Wei Tian Xian-Hua Li Hao-Yang Lee Himalayan zircons resurface in Sumatran arc volcanoes through sediment recycling Communications Earth & Environment |
title | Himalayan zircons resurface in Sumatran arc volcanoes through sediment recycling |
title_full | Himalayan zircons resurface in Sumatran arc volcanoes through sediment recycling |
title_fullStr | Himalayan zircons resurface in Sumatran arc volcanoes through sediment recycling |
title_full_unstemmed | Himalayan zircons resurface in Sumatran arc volcanoes through sediment recycling |
title_short | Himalayan zircons resurface in Sumatran arc volcanoes through sediment recycling |
title_sort | himalayan zircons resurface in sumatran arc volcanoes through sediment recycling |
url | https://doi.org/10.1038/s43247-022-00611-6 |
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