摘要
赞坎铁矿Ⅲ号矿带形成的“岛状”地面高磁异常特征，是由多层矿体近地表波状变形引起，这与该区目前发现的地面高磁异常特征以带状为主明显不同。利用已有勘查成果对该磁异常特征进行分析，确定矿带与异常的关系，以期对该区找矿提供新的思路。
The island high ground magnetic anomaly formed by the orebody in Zankan iron deposit is caused by the surface wavy deformation of multilayer ore bodies,which is obviously different from the discovered stripled magnetic anomaly in this area so far.Using the known prospecting achievement to analyze,this magnetic anomaly can help us con- finn the relationship between the ore belt and the anomaly and then provide new ideas for the gelolgical prospection in this area.
出处
《新疆地质》
CAS
CSCD
北大核心
2013年第F12期27-30,共4页
Xinjiang Geology
基金
2010-2012年中国地质调查局矿产调查评价类项目-新疆塔什库尔干县赞坎铁调查评价项目资助
