摘要
大龙潭金矿是云南在新近系砂砾岩中找金新突破。区内矿体分布于NW向断层F4、F6所夹持的大龙潭向斜近核部层间挤压滑动破碎带中,含矿地层为上新统三营组,属微细浸染型。
The discovery of Dalongtan Au deposit is a new breakthrough of Au prospecting in Neogene Sandstone-Conglomerate of Yunnan. The ore bodies in this area are mainly distributed in the interbed pressed sliding zone nearing the core of Dalongtan syncline between NW-wards fault F_4, F_6.
出处
《云南地质》
2004年第3期328-336,共9页
Yunnan Geology
