Magma-Rock and Magma-Mush Interactions as Fundamental Processes of Magmatic Differentiation
Author: Anastassia Borisova
Publisher: Frontiers Media SA
Published: 2024-08-08
Total Pages: 208
ISBN-13: 2832552994
DOWNLOAD EBOOKDuring transport, a percolating melt or magma may contact rock or a magmatic mush, resulting in inevitable interactions that may be described as magma/melt-rock or magma/melt-mush interactions. Examples of these types of interactions include mantle metasomatism, mineral-melt reaction in the mantle, mineral dissolution in magma, crustal wallrock partial melting, and thermal remobilization of preexisting mushy magma (rejuvenation of mush) by intruding high specific enthalpy magma. This spectrum of processes plays a major role in the composition, thickness, and age of the mantle lithosphere and its associated crust. These interactions also impact the asthenosphere because melts that form in the deepest parts of the mantle may ascend and interact with shallower mantle during transport.