Tonian crustal melting triggered by subduction along the Rodinia periphery: Evidence from the Liujiaping batholith, NW Yangtze Block, South China
Key Points
Crustal melting in the Tonian period has been linked to subduction processes along the Rodinia margin, enhancing our understanding of ancient tectonics.
Evidence from the Liujiaping batholith indicates that this melting was a significant geological event occurring during the Tonian period, affecting the Yangtze Block.
Geochemical analysis of rock samples shows distinct signatures of subduction-related processes, underlining the complexity of crustal formation in this period.
Insights from this study support the view that crustal evolution is closely tied to subduction dynamics, advocating for further studies in adjacent regions.
Tonian crustal melting triggered by subduction along the Rodinia periphery: Evidence from the Liujiaping batholith, NW Yangtze Block, South China | Synapse
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