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阜平岩群下部Sm-Nd同位素年龄及其地质意义
Sm-Nd Isotope Age of the Lower Fuping Group Complex and Its Geological Significance
【摘要】 阜平岩群主要分布在太行山北段,是我国太古宙重要的地层单元,并构成阜平深变质绿岩带的岩石组合。前人认为阜平岩群及其区域变质时代主要为新太古代。本次对阜平岩群下部含辉石斜长角闪岩Sm-Nd同位素年代学的详细研究,获得Sm-Nd等时线年龄3352±50Ma和平均模式年龄3374.5Ma,说明阜平岩群底界年龄接近3400Ma,从而也反映阜平深变质绿岩带形成在古—中太古代,是我国目前最老的绿岩带,也是世界上最古老的绿岩带之一。
【Abstract】 The Fuping Group complex is mainly exposed in the northern part of Taihang Mountain. It is an important Archean stratum in China and consists of a rock association of the Fuping katametamorphic greenstone belt. It was recognized before that the Fuping Group complex and regional metamorphism are mainly of the Neoarchean in age. In this research, pyroxeneferous amphibolites of the lower Fuping Group complex show an Sm-Nd isochronal age of 3352±50 Ma and an average model age of 3374 Ma, which indicates that the isotope age of the bottom boundary of the Fuping Group complex is close to 3400 Ma. This isotope age also indicates that the Fuping Group complex, as well as Fuping katametamorphic greenstone belt, belongs to the Paleo-Mesoarchean. As a result, the Fuping greenstone belt is the oldest greenstone belt in China and one of the oldest greenstone belts in the world.
【Key words】 Fuping Group complex; Sm-Nd isotope age; pyroxeneferous amphibolites; katametamorphic greenstone belt;
- 【文献出处】 地质学报 ,Acta Geologica Sinica , 编辑部邮箱 ,2005年06期
- 【分类号】P597
- 【被引频次】11
- 【下载频次】194