A Neoarchean K-rich granitoid belt in the northern North China Craton

Jinghao Fu,Shuwen Liu,Bo Zhang,Rongrong Guo,Maojiang Wang

Precambrian Research（2019）

引用 36|浏览9

暂无评分

摘要

•A ca. 350 km long Neoarchean K-rich granitoid belt in the northern North China Craton.•∼2.90 Ga trondhjemitic gneisses are preserved in the K-rich granitoid belt.•2.55–2.53 Ga sanukitoids and potassic granites stemmed from crust/mantle interactions.•The K-rich granitoid belt was multi-deformed from Neoarchean to Paleoproterozoic period.•Neoarchean southeastward retreating oceanic slab subduction and arc-continent collision.

查看译文

关键词

Neoarchean K-rich granitoid belt,Sanukitoids and potassic granites,Multi-stage deformation,Retreated subductions in the continental margin,Northern North China Craton

AI 理解论文

溯源树

样例

生成溯源树，研究论文发展脉络

Chat Paper

正在生成论文摘要