中国东南华夏板块的武夷山地块与罗霄地块之间存在一个非史密斯的地层带 ,称为雩山结合带。它是早古生代华夏板块与扬子板块拼贴过程中形成造山带的一个部分 ,自早奥陶世开始消减—中晚奥陶世主期挤压—中志留世伸展—晚志留世走滑四个阶段的非史密斯化过程。 There is a non-Smith stratigraphic belt between the Wuyishan massif and the Luoxiao massif in the southeastern China Huaxia plate, which is called the Jieshan belt. It is a part of the orogenic belt formed during the collapsing of the Early Paleozoic Huaxia Plate and Yangtze Plate since the Ordovician began to subside - the middle and late Ordovician subduction - the Middle Zhiyu stretch - late Silurian slippery four The stage of the non-Smith process.