摘要
The internal structure-stratigraphy and geochemical signatures of most forearc suprasubduction zone ophiolites display structural, petrological, geochemical and geochronological evidence, recording different stages of subduction initiation-related magmatism, material flux,
The internal structure-stratigraphy and geochemical signatures of most forearc suprasubduction zone ophiolites display structural, petrological, geochemical and geochronological evidence, recording different stages of subduction initiation-related magmatism, material flux,
