内蒙古中部早古生代地体的拼合与增置

内蒙古中部布龙山、温都尔庙一带的蛇绿岩套、蓝门石片岩及其南邻的华北地台两者在空间上以川井－布鲁台庙深大断裂带为界，在时间上具有截然不同的地质演化特点。其内部在构造演化史上也不尽相同，可进一步划分为布龙山－哈拉地层地体和白乃庙－温都尔庙混杂地体。这两个曾分离着的地体，经长时期的运移，于晚志留世之前拼合联为一体，构成早古生代联合地体。直到早二叠世才增置于中朝古板块北缘（或华北地台北缘）。

Early palaeozoic Era of Terrane Pieced together and Accreted in Middle of Inner Mongolia

The ophiolite suite and glaucophane schist assocition are boundary of deep fracture zone of Chuanjing-Bulutaimiao,and joined by North China plateform, Bulongshan,Wenduemiao, in middle of inner Mongolia. They have different from geological and structure evolution of interior,that they can be divided into stratigraphic and chaotic terrane of Bulongshan-Hala and Bainaimiao -Wenduemiao. The both terranes make up early palaeozoic conjunct terrane that severed from each other and movement for long time then they pieced together before Late Devonian. UP to early Permian terranes accreted to northern margin of Sino-Korean palaeo plate.