康定杂岩黑云母、角闪石^(39)Ar-^(40)Ar年龄及其意义  

^(39)Ar-^(40)Ar dating of biotites and hornblendes in the Kangding complexes and their significances.

作　　者：李大鹏[1] 陈岳龙[1] 罗照华[1] 

机构地区：[1]中国地质大学,北京100083

出　　处：《岩石学报》2006年第11期2753-2761,共9页Acta Petrologica Sinica

基　　金：国家自然科学基金(资助号40173007);教育部重点科研项目(重点03032)的部分成果。

摘　　要：通过对康定杂岩黑云母、角闪石 Ar-Ar 年龄研究,得出康定杂岩黑云母、角闪石中 Ar 同位素组成明显存在地质离散,有过剩氩;Ar-Ar 年龄并不反映矿物形成后的变质冷却历史。坪的产生可能是由过剩^(40)Ar 存在于非晶粒边缘的缺陷之中,使其与放射性成因^(40)Ar 具有相似活化能,从而使不同种 Ar 组分等比例释气所致。经计算,样品中过剩氩约占氩总量的16%左右。Through the study of Ar-Ar ages of biotites and hornblendes in the Kangding complexes by step-heating release technology, we found the existence of excess argon in these minerals and the irrelevance between the apparent age and the history after metamorphism of the plutonic complexes. Excess argon is trapped in defects which are not connected with the grain boundary, thus it needs the same energy as the radiogenic argon to come out of grain. This feature brings a mixing of different argon components which can explain the plateau ages. And excess argon may take about 16% of total argon.

关 键 词：过剩氩 地质离散 逐级加热 康定杂岩 

分 类 号：P588.347[天文地球—岩石学] P597.3[天文地球—地质学]