摘要
通过收集新疆雅满苏铁矿多年开采所揭露的地质现象，对其成因否定了以往的各种观点，并从多方面作出了更符合客观事实的重新论证，提出了该矿为一海底火山喷溢熔离型矿床。
Based on exposured geologic phenomenon of Yamansu iron deposit in Xinjiang after being explored for many years, this paper refutes the existing viewpoints on its origin, devises new argumentation from many aspects that accords further with its nature, and raises an idea that the deposit is a volcanic extrusion-overflow melted- separate deposit on seabed.
出处
《长春工程学院学报（自然科学版）》
2001年第4期26-29,共4页
Journal of Changchun Institute of Technology：Natural Sciences Edition
关键词
新疆
火山喷溢
熔离矿床
火山熔岩
Xinjiang
volcanic extrusion-overflow
the melted-separate deposit
volcanic melted rock
