低地幔条件下的碳酸盐熔体（英文）

作者：吴旻^*; 姜杰浩; John S.Tse^*; Yuanming Pan^*

来源：Science Bulletin, 2022, 67(13): 1307-1309.

<正>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.