摘要
八家子矿区岩石及矿石的稀土元素特征表明,圣宗庙岩体、八家子岩体为同源岩浆侵入体,草沟英交流纹斑岩与上述两岩体在物质来源上具有相关性;炉沟、瓦房沟、碱厂及宽帮岩体亦来自同一岩浆系统。成矿作用主要与炉沟及瓦房沟岩体有关,但成矿物质除岩浆源外,还部分地来源于混合花岗岩及地层。
It is illustrated by REE characteristics of Bajiazi deposit that shengzhong miao and Bajiazi rock bodies are homologous magmatic intrusive bodies and Chaogou dacite Iiparite rock body is related to the same magmatic source.Lugou,Wafanggou, jianchang and kuanbang rock bodies are the same one.Minerogenetic process is correlation with Lugou and Wafanggou rock bodies.The metalloginic material derived from magma source and partly from migmatite and stratum.
出处
《辽宁地质》
1991年第4期322-331,共10页
