摘要
新疆萨吾尔山存在两期不同成因的花岗岩类,其 Rb - Sr 同位素年龄值分别为314 .9 ~320 .3 Ma 和295 ~296 Ma 。结合其侵位的地层及其与火山岩的关系等确定这两种不同类型花岗岩的时代分别为海西中期和晚期。
There exist two periods of genetically different granitoids in Sawuer Mountain of Xinjiang, whose Rb-Sr isotopic ages are 314.9~320.3 Ma and 295~296 Ma respectively. Based on these data in combination with their emplaced strata and their relations with volcanic rocks, it is considered that these two types of granitoids are of Middle and Late Hercynian respectively.
出处
《岩石矿物学杂志》
CAS
CSCD
北大核心
1999年第3期237-242,共6页
Acta Petrologica et Mineralogica
基金
新疆萨吾尔山1:5 万区调项目