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作 者:ZHANGHongfei NigelHarris RandyParrish ZHANGLi ZHAOZidan
机构地区:[1]FacultyofEarthSciences,ChinaUniversityofGeosciences,Wuhan430074.China [2]DepartmentofEarthSciences,TheOpenUniversity,MiltonKeynes,MK76AA,UK [3]NERCIsotopeGeosciencesLaboratory,BritishGeologicalSurvey,Nottingham,NG125GG,UK [4]SchoolotEarthScienceandLandResources.ChinaUniversityofGeosciences,Beijing100083,China
出 处:《Chinese Science Bulletin》2004年第19期2087-2092,共6页
摘 要:U-Pb ages of zircon,monazite and xenotime from the Kude and the Sajia leucogranites in the Sajia dome of the North Hima- layan tectonic unit are measured using TIMS method. The results show that the magma emplacement ages for the Kude and the Sajia leu- cogranite are 27.5±0.5 and 14.4±0.2 Ma,respectively. Combined with published U-Pb data from the North Himalayan leu- cogranites,the time-span for the formation of the North Himalayan leucogranites is updated from 27.5 to 10 Ma,instead of previous 15 to 10 Ma.According to the U-Pb ages,the petrogenesis for the North Himalayan leucogranites can be constrained.It is suggested that the North Himalayan leu- cogranites have variety in their petrogenesis.U-Pb ages of zircon,monazite and xenotime from the Kude and the Sajia leucogranites in the Sajia dome of the North Hima- layan tectonic unit are measured using TIMS method. The results show that the magma emplacement ages for the Kude and the Sajia leu- cogranite are 27.5±0.5 and 14.4±0.2 Ma,respectively. Combined with published U-Pb data from the North Himalayan leu- cogranites,the time-span for the formation of the North Himalayan leucogranites is updated from 27.5 to 10 Ma,instead of previous 15 to 10 Ma.According to the U-Pb ages,the petrogenesis for the North Himalayan leucogranites can be constrained.It is suggested that the North Himalayan leu- cogranites have variety in their petrogenesis.
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