Earth’s deep interior consists of two layers, the rocky mantle and the metallic core. The detailed composition of the lower mantle and the core (particularly, the light elements in the core), the physical and chemical state of silicate minerals and metallic phases in the core-mantle boundary region, and the nature of material transport between core and mantle through time and space remains understudied. Core Mantle Coevolution: A Multidisciplinary approach solves major unsolved problems focusing on the core mantle interaction and coevolution and presents new directions in research filling the void in literature from the past two decades. Volume highlights include: State-of-the-art science on core-mantle interactions and their influences on evolution of deep planetary systems Depicts present-day Earth’s interior, its formational processes and evolutionary mechanisms Aims for a deeper understanding of the thermal-chemical-mechanical-electromagnetic interaction in the core-mantle boundary through theoretical investigations on thermal-chemical evolution of Earths mantle and core Offers insights on the fusion of different research fields such as "high pressure mineral physics", "high-precision geochemical analysis", "high resolution geophysical observations, latest realms of geoneutrino field", and "theoretical computations" Presents latest results on multimegabar high pressure and temperature experiments with high precision analytical results on element and isotope partitioning experiments, as well as theoretical computations of material properties under high pressure and temperature Reviews large-scale seismological and geomagnetic observations and its data analysis to image the heterogeneous and anisotropy structure in the deep Earth Core Mantle Coevolution: A Multidisciplinary approach is a valuable resource for researchers, professionals, and graduate students from a wide variety of fields including mineralogy, geochemistry, petrology, tectonics, geomagnetism, seismology, and geophysics.

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