Diorite Vein in Quenched Basalt and Its Implication for the Origin of Late-Granitoid Intrusives in Naga Hills Ophiolite, Northeast India

Ghose, N. C., & Chatterjee, N. (2011). Diorite Vein in Quenched Basalt and Its Implication for the Origin of Late-Granitoid Intrusives in Naga Hills Ophiolite, Northeast India. In Dyke Swarms:Keys for Geodynamic Interpretation (pp. 315–330). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-12496-9_19