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Structural Origin of the Red-Ribbon Style Iron Ores in the Xinyu Iron Deposit,Central Jiangxi Province
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作者 CHEN Zhengle ZHANG Qing +3 位作者 CHEN Bailin WANG Xueping SHEN Tao WU Junjie 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2015年第2期691-692,共2页
The Xinyu iron deposit, located in central Jiangxi Province, is one of the most important BIF-type deposits in China. It is hosted in the Late Proterozoic volcanic- sedimentary rocks, which are composed of sericite- c... The Xinyu iron deposit, located in central Jiangxi Province, is one of the most important BIF-type deposits in China. It is hosted in the Late Proterozoic volcanic- sedimentary rocks, which are composed of sericite- chlorite pyhllite, magnetite-bearing chlorite phyllite or schist, magnetite quartzite, and schist (Yu et al., 1989; Zeng et al., 2011). 展开更多
关键词 Structural Origin of the Red-Ribbon style Iron Ores in the Xinyu Iron Deposit Central Jiangxi Province
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