Structure and Dynamics of the Earth's Interior 1
The silicate mantle and its dynamics have controlled the Earth''s internal cooling for over four billion years. Today, these dynamics are rather slow, but this was not always the case: shortly after the core/mantle separation, this reservoir was significantly melted, with dynamics like those of a magma ocean. Despite advances in analytical and numerical tools and a better understanding of the Eart...
The silicate mantle and its dynamics have controlled the Earth''s internal cooling for over four billion years. Today, these dynamics are rather slow, but this was not always the case: shortly after the core/mantle separation, this reservoir was significantly melted, with dynamics like those of a magma ocean. Despite advances in analytical and numerical tools and a better understanding of the Eart...
