喀拉通克铜镍硫化物矿床地质特征、成因探讨及新的找矿方向

喀拉通克铜镍硫化物矿床,发现于上世纪80年代,但在最近的十多年中,找矿工作一直没有取得重大突破。因此,反思找矿思路,已经显得非常重要。本文简单介绍了该矿床的地质情况,探讨了矿床成因,并在此基础上提出了新的找矿方向:寻找岩浆通道型块状硫化物矿床。

The Kalatongke Ni-Cu sulfide deposit discovered in the 80s of the last century, but the recent 10 years, the prospecting work has failed to achieve any major breakthrough. Therefore, reflecting prosI^ecting ideas, have become very important. This paper introduces the geology of the deposit, discusses the genesis, and on the basis of these to find a new direction for prospecting ： Magma massive sulfide deposit.