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

Bibliographic Details
Main Authors: Meng-Hao Gao, Ping-Ping Liu, Sun-Lin Chung, Qiu-Li Li, Bin Wang, Wei Tian, Xian-Hua Li, Hao-Yang Lee
Format: Article
Language:English
Published: Nature Portfolio 2022-11-01
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
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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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