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Late Mesoproterozoic to Early Neoproterozoic tectono-magmatic evolution of the southwestern margin of the Yangtze Block: Evidence from A-type granitoids in the Yuanmou area
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DOI：10.1016/j.precamres.2026.108131.png)
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Abstract
En 中文
• Two-stages (∼1.06 Ga and ∼ 0.82 Ga) of A-type granitoids are identified in the SW-Yangtze Block; • The two-stage granitoids reveal two distinct tectonic settings; • A tectonic transition from rifting setting to multi-stage subduction settings is proposed.
Keywords:
A-type granitoids
tectonic setting
rifting
subduction
Yangtze Block
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