摘要
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.
作者
Min Wu
Jiehao Jiang
John S.Tse
Yuanming Pan
吴旻;姜杰浩;John S.Tse;Yuanming Pan(College of Materials Science and Engineering,Zhejiang University of Technology,Hangzhou 310014,China;Shaoxing Research Institute,Zhejiang University of Technology,Shaoxing 312000,China;Department of Physics and Engineering Physics,University of Saskatchewan,Saskatoon,SK S7N 5E2,Canada;Department of Geological Sciences,University of Saskatchewan,Saskatoon,SK S7N 5E2,Canada)
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。
