Induced subduction initiation near an ultra-slow spreading ridge: A case study from the Beila ophiolite in the north-central Tibetan Plateau-Reference-Cited by-同舟云学术

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Induced subduction initiation near an ultra-slow spreading ridge: A case study from the Beila ophiolite in the north-central Tibetan Plateau

Published:2024-11 Issue: Volume:135 Page:1-16
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Zhai Qingguo,Tang Yue,Hu Peiyuan,Liu Yiming,Wang Wei

Funder

Jiangsu Provincial Key Laboratory for the Research and Utilization of Plant Resources, Chinese Academy of Sciences

China Geological Survey, Ministry of Natural Resources

National Natural Science Foundation of China

Tianjin Postdoctoral Science Foundation

National Aerospace Science Foundation of China

Publisher

Elsevier BV

Reference88 articles.

1. A record of spontaneous subduction initiation in the Izu-Bonin-Mariana arc;Arculus;Nat. Geosci.,2015

2. The application of SHRIMP to Phanerozoic geochronology: a critical appraisal of four zircon standards;Black;Chem. Geol.,2003

3. Improved Pb-206/U-258 microprobe geochronology by the monitoring of a trace-element-related matrix effect; SHRIMP, ID-TIMS, ELA-ICP-MS and oxygen isotope documentation for a series of zircon standards;Black;Chem. Geol.,2004

4. Rapid forearc spreading between 130 and 120Ma: Evidence from geochronology and geochemistry of the Xigaze ophiolite, southern Tibet;Dai;Lithos,2013

5. Forearc magmatic evolution during subduction initiation: insights from an early Cretaceous Tibetan ophiolite and comparison with the Izu-Bonin-Mariana forearc;Dai;Geol. Soc. Am. Bull.,2021

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