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Origin and evolution of silicic magmas in the Okinawa trough: insights from coupled cathodoluminescence, trace element, and oxygen isotope analyses of quartz

Crossref DOI link: https://doi.org/10.1007/s00410-025-02236-2

Published Online: 2025-07-28

Published Print: 2025-09

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Luo, Xinyu https://orcid.org/0009-0004-7501-5677
Zeng, Zhigang

Chen, Zuxing

Zhang, Yuxiang
Funding

Funding for this research was provided by:

National Natural Science Foundation of China (42330409, 42221005, 91958213)

National Basic Research Program of China (2013CB429700)

Taishan Scholars Program (ts201511061)
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Text and Data Mining valid from 2025-07-28

Version of Record valid from 2025-07-28
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Article History

Received: 25 January 2025

Accepted: 25 June 2025

First Online: 28 July 2025

Change Date: 18 August 2025

Change Type: Update

Change Details: The original version of this article was revised due to missing Associate Editor name. Now it has been corrected.

Declarations

:

: The authors declare no competing interests.

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