Before revision: Crust-Mantle and Lithosphere-Asthenosphere Boundaries: Insights from Xenoliths, Orogenic Deep Sections, and Geophysical Studies, pages 1-22, Geological Society of America, 2017, Dynamics The hot mantle material is intruded in the form of a sill (geology) .
After revision: Crust-Mantle and Lithosphere-Asthenosphere Boundaries: Insights from Xenoliths, Orogenic Deep Sections, and Geophysical Studies, pages 1-22, Geological Society of America, 2017, Dynamics The hot mantle material is intruded in the form of a sill .