Carbonate melts at high pressure and temperature conditions are crucial to the deep carbon cycle and play critical roles in the dynamics and evolution of Earth’s mantle.Melting of carbon-bearing rocks,which generates...Carbonate melts at high pressure and temperature conditions are crucial to the deep carbon cycle and play critical roles in the dynamics and evolution of Earth’s mantle.Melting of carbon-bearing rocks,which generates carbonatitic and carbonated silicate melts in the mantle,has been suggested as the primary agents for the outgassing of carbon from Earth’s interior dictating the deep carbon cycle.展开更多
基金supported by the National Natural Science Foundation of China(51701180,51871201,and U1802254)supported by the Canada Research Chair program and a grant from Natural Sciences and Engineering Research Council of Canada。
文摘Carbonate melts at high pressure and temperature conditions are crucial to the deep carbon cycle and play critical roles in the dynamics and evolution of Earth’s mantle.Melting of carbon-bearing rocks,which generates carbonatitic and carbonated silicate melts in the mantle,has been suggested as the primary agents for the outgassing of carbon from Earth’s interior dictating the deep carbon cycle.
