Chronology and Sources of Mesozoic Intrusive Complexes in the Xuzhou-Huainan Region, Central China: Constraints from SHRIMP Zircon U-Pb Dating

SHRIMP zircon U-Pb dating in the Liguo and Jiagou intrusives indicates that they were formed at -130 Ma in the Early Cretaceous. Most inherited zircons in the Liguo intrusive were formed at 2509±43 Ma. Most inherited and detrital zircons in the Jiagou intrusive were formed at -2500 Ma, -2000 Ma and -1800 Ma. The SHRIMP zircon U-Pb dating in two gneiss xenoliths from the Jiagou intrusive yields the ages of 2461±22 Ma and 2508±15 Ma, respectively. The dating results from inherited and detrital zircons in the intrusives and the gneiss xenoliths imply that the magmas could be derived from the partial melting of the basement of the North China Block (NCB). The magmatism is strong and extensive in the periods from 115 to 132 Ma, which is of typical bimodal characteristics. It is suggested that the lithospheric thinning in the eastern North China Block reached its peak in 115-132 Ma.

高温合金单晶铸件中条纹晶的形成机制

对高温合金单晶叶片铸件中条纹晶起源处的微观组织进行了观察分析,提出了这种晶粒缺陷的产生机理。通过微观检测确认了条纹晶的出现是由于铸件表面单个枝晶主干在糊状区内被撕断,但又被残余液体焊合,呈现出明显的起点。导致这种撕裂的主要原因是型壳粘连引起的枝晶收缩严重受阻或是由夹杂切割引起的枝晶强度严重受损,从而形成了条纹晶缺陷产生的2种主要机制。撕裂后的枝晶会发生一定程度的整体偏转,在基体组织上形成一个由小角度晶界封闭而成的狭长晶粒。比较了条纹晶与其它晶粒缺陷的相似和不同之处,并讨论了减少条纹晶缺陷应该采取的工艺措施。