Coexisting Carbonatite and Silicate Melt Inclusions in the Cretaceous Volcanic Rock from the Central Great Xing'an Range,Northeast China:Evidence for Recycled Carbonate from Subducted Paleo-Pacific Plate  

作　　者：Chao Zhang Hongxu Pu Jianqiang Liu Xiaojun Wang Wenqiang Yang Zhenbing She Shitou Wu Gang Zeng Lihui Chen Francois Holtz 

机构地区：[1]State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,China [2]State Key Laboratory of Biogeology and Environmental Geology,School of Earth Sciences,China University of Geosciences,Wuhan 430078,China [3]State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China [4]State Key Laboratory for Mineral Deposits Research,School of Earth Sciences and Engineering,Nanjing University,Nanjing 210023,China [5]Institute of Mineralogy,Leibniz University Hannover,Hannover 30167,Germany

出　　处：《Journal of Earth Science》2025年第1期364-372,共9页地球科学学刊(英文版)

基　　金：supported by the National Natural Science Foundation of China(Nos.42130310 and 41972055)。

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.

关 键 词：NORTHEAST Paleo Earth 

分 类 号：P534.53[天文地球—古生物学与地层学] P588.245[天文地球—地质学] P542