用地球化学自组织作用思想讨论了鞍山式铁矿床中条带状矿化图案的微观成因机理，认为它们是一种在远离平衡态条件下的耗散结构，建立了成因理论模型。
The idea of geochemical self-organization is employed to explain the microscopical genetic mechanism of banded mineralizing pattern (BMP) developed in Anshan-type iron deposits, China.
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。
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".
前寒武纪条带状含铁建造铁矿床分为阿尔戈马型和苏必利尔湖型两大类。
Precambrian BIF iron ore deposit can be divided into two types, Algoma-type and Lake Superior-type.
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