Titanite fingerprint of SiO2-oversaturated to -undersaturated plutons: Insights into petrogenesis, passive rifting and Neo-Tethys opening on the NE Gondwanan margin
Key Points
Insights into petrogenesis reveal significant geological processes in the NE Gondwanan margin.
Sio2 oversaturation and undersaturation impact the composition and evolution of plutons, influencing rifting.
Analysis of titanite fingerprints provides valuable information about the geological history of the region.
Findings highlight the connection between geological formations and historical continental shifts.
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Titanite fingerprint of SiO2-oversaturated to -undersaturated plutons: Insights into petrogenesis, passive rifting and Neo-Tethys opening on the NE Gondwanan margin | Synapse