P588.122
本文根据全岩Rb-St,锆石U-Pb和角闪石、黑云毒、钾长石K-Ar同位素年龄综合测定结果,再造了安庆-庐江石英正长岩带中黄梅尖岩体的冷却史。矿物对氧同位素地质测温结果证实,扩散作用是控制同位素体系封闭的主导因素。
郑永飞 傅斌.1995.安徽黄梅尖岩体热历史及其与成矿关系:同位素证据[J].地质学报,69(4).Zheng Yongfei, Fu Bin, Gong Bing.1995. THE THERMAL HISTORY OF THE HUANGMEIJIAN INTRUSION IN ANHUI AND ITS RELATION TO MINERALIZATION: ISOTOPIC EVIDENCE[J]. Acta Geologica Sinica,69(4).