Low-δ¹⁸O Felsic Magmatism in the Meghalaya Gneissic Complex #sciencefather #researcher
Low-δ¹⁸O Felsic Magmatism in the Meghalaya Gneissic Complex #sciencefather #researcher
This study documents Mesoproterozoic low-δ¹⁸O felsic magmatism in the Meghalaya Gneissic Complex, India, driven by in situ melting of hydrothermally altered crust, offering key insights into crust–hydrothermal interaction and ancient tectono-magmatic processes.
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