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地壳增生和多源性再造与巨量斑岩<bold>-</bold>矽卡岩铜<bold>-</bold>金<bold>/</bold>铁<bold>、</bold>钨<bold>-</bold>钼成矿<bold>: </bold>以长江中下游中段及邻区为例

Crossref DOI link: https://doi.org/10.1360/SSTe-2024-0183

Published Online: 2025-05-19

Published Print: 2025-06-01

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