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作 者:Emilio Saccani Vinod Samuel M.Santosh
机构地区:[1]Department of Physics and Earth Sciences,Ferrara University,44122,Ferrara,Italy [2]Department of Earth System Sciences,Yonsei University,Seoul,South Korea [3]China University of Geosciences(Beijing),Beijing 100083,China
出 处:《Geoscience Frontiers》2020年第1期1-2,共2页地学前缘(英文版)
摘 要:Ophiolite studies over the decades have played a crucial role in better understanding of mid-ocean ridge and subduction zone processes,mantle dynamics and heterogeneity,fluid-rock interactions in both sub-oceanic and sub-arc upper mantle,and the mechanisms of continental growth in accretionary and collisional belts.The continued interest in ophiolites as a topic of multi-disciplinary research in Earth Sciences has resulted in a wealth of new data,syntheses,and ideas from ophiolites around the world.
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