A newly found Paleozoic Japan-type subduction-accretion system

• 来源期刊: 科学通报（英文版）
• 年，卷（期）: 2015,（23）
• 页码范围: 2069-2070
• 页数: 2页
• 语种: 中文
• DOI: 10.1007/s11434-015-0956-z

摘要

Accretionary orogenic belts are complicated collages composed of magmatic arcs, accretionary complexes, ophiolitic mélanges, fore-arc/back-arc basins and microcontinents formed at convergent plate margins, which are key sites of continental growth through earth history [1].