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本文是首次运用构造动力成岩成矿的理论和地质力学分析方法对我国海南石碌铁、铜、钴典型矿床进行研究的重要成果。它以大量实际资料和测试数据为基础,阐述了海南石碌铁、铜、钴矿成矿的构造、地层环境,从多方面论证了流动造构及构造动力分异作用与铁、铜、钴矿富集成矿、富化加厚的内在联系。并对铜、钴矿床中伴生金富集特征及其综合利用前景作了分析与评价,同时对地层的划分、时代的确定,海底火山作用以及岩石、矿石在构造动力作用下所发生的形变相变特征,均作了比较详细的论述。在一定意义上说,它为今后研究矿床形成机制方面开拓了新的研究途径。
This article is the first to use the theory of structural dynamic diagenesis and geomechanical analysis to study the iron, copper and cobalt typical deposits in Shilu, Hainan Province, China. Based on a large amount of actual data and test data, this paper expounds the structure and stratigraphic environment of the iron, copper and cobalt ore deposits in Shilu, Hainan Island. It proves that the flow structure and tectonic differentiation are compatible with iron, copper, cobalt Mineral rich mineralization, enrichment and thickening of the internal relations. The characteristics of associated gold enrichment in copper and cobalt deposits and the prospect of their comprehensive utilization are analyzed and evaluated. At the same time, the stratigraphic division, the determination of the times, the submarine volcanism and the deformation phases of rocks and ores under the action of tectonic force Change characteristics, have made a more detailed discussion. In a certain sense, it opens up a new approach to research on the mechanism of deposit formation in the future.