摘要
0 INTRODUCTION Subduction of oceanic plate is vital for carbon redistribution and recycling between Earth's surface and mantle,which plays a critical role in shaping carbon budgets and terrestrial habitability through geological time(e.g.,Plank and Manning,2019;Sverjensky et al.,2014;Dasgupta and Hirschmann,2010).The long-term subduction of Pacific/Paleo-Pacific Plate from Late Mesozoic to Cenozoic beneath Northeast China makes this area an ideal candidate for exploring ancient carbon recycling and its impact on Earth's surface environment.
基金
supported by the National Natural Science Foundation of China(Nos.42130310 and 41972055)。
