This paper is a stage result of special research for "marble" in contact of Daye iron deposit and "banded pyroxene-garnet marble" distributed in the "marble".

本文是对大冶铁矿床接触带“大理岩”及其中分布的“条带状辉石-石榴石大理岩”进行专门研究的阶段性结果。

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This paper systematically expounds rock characteristics, ore-forming process, natrium origin and natrium alteration mechanism in contacting zones of Daye iron deposit.

对于大冶铁矿内接触带钠化蚀变的岩石特征、钠质来源、动力机制、形成机理等作了比较系统的阐述。

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Suitable for the interactive inversion and interpretation in exploitation stage, this method is finally applied in dealing with geomagnetic data of the Daye iron deposit with satisfactory results.

该方法适合于开采阶段的交互反演解释，将该方法运用于大冶铁矿，取得了很好的地质效果。

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