综述了近年来在古生物对比、古地磁对比、火山岩岩石建造、岩石地球化学等方面的研究成果。认为早古生代秦岭造山带的历史是岩石圈经历小“开”小“合”的历史.“开”阶段的古地理格局是多岛小海盆,“合”的最终表现是出现加里东运动。 In recent years, the research results on paleontology, paleomagnetic contrast, volcanic rock formation and lithogeochemistry are reviewed. The history of the Qinling orogenic belt in the Early Paleozoic is that the lithosphere experienced a small “open ” small “co ” history. “Open ” stage of the ancient geographical pattern is the multi-island small basin, The performance is Caledonian movement.