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Reactivated deformation structure induced by Early Cretaceous magmatism in the Sulu Orogen rift basin, eastern China | Synapse
March 3, 2026
Reactivated deformation structure induced by Early Cretaceous magmatism in the Sulu Orogen rift basin, eastern China
JJ
Jianliang Jia
TW
Tao Wang
NP
Nan Peng
Key Points
Reactivated deformation structures signify important geological changes in the Sulu Orogen rift basin.
Key evidence includes the impact of Early Cretaceous magmatism on regional geological formations.
Observational analysis of geological samples from the Sulu Orogen reveals critical insights into historical volcanic activity.
Understanding these geological processes may help predict future tectonic and magmatic activities.
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Jia et al. (Sun,) studied this question.
synapsesocial.com/papers/69a7659dbadf0bb9e87d9bdf
https://doi.org/https://doi.org/10.1016/j.gloplacha.2026.105348