Articles | Volume 15, issue 9
https://doi.org/10.5194/se-15-1133-2024
https://doi.org/10.5194/se-15-1133-2024
Research article
 | 
16 Sep 2024
Research article |  | 16 Sep 2024

Driven magmatism and crustal thinning of coastal southern China in response to subduction

Jinbao Su, Wenbin Zhu, and Guangwei Li

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1264', Anonymous Referee #1, 15 Jun 2024
    • AC1: 'Reply on RC1', Jinbao Su, 18 Jun 2024
  • RC2: 'Comment on egusphere-2024-1264', Anonymous Referee #2, 04 Jul 2024
    • AC2: 'Reply on RC2', Jinbao Su, 13 Jul 2024
  • RC3: 'Comment on egusphere-2024-1264', Anonymous Referee #3, 04 Jul 2024
    • AC3: 'Reply on RC3', Jinbao Su, 13 Jul 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Jinbao Su on behalf of the Authors (27 Jul 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (02 Aug 2024) by Antonella Longo
ED: Publish as is (02 Aug 2024) by Andrea Di Muro (Executive editor)
AR by Jinbao Su on behalf of the Authors (02 Aug 2024)
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The requested paper has a corresponding corrigendum published. Please read the corrigendum first before downloading the article.

Short summary
The late Mesozoic igneous rocks in the South China Block exhibit flare-ups and lulls, which form in compressional or extensional backgrounds. The ascending of magma forms a mush-like head and decreases crustal thickness. The presence of faults and pre-existing magmas will accelerate emplacement of underplating magma. The magmatism at different times may be formed under similar subduction conditions, and the boundary compression forces will delay magma ascent.
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