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J4 ›› 2007, Vol. 15 ›› Issue (2): 1-8.
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LIANG Dong, DAI Jian-Bin
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Abstract:
Daxin gold deposit in Hunan province are hosted by the Sinian gravel - bearing sand-stone slate, and are closely controlled by the faults. The mineralizing stage of these deposits can be divided into two periods: i.e. period of hydrothermal mineralizing and period of epigenic mineralizing, and the former one is the primary mineralizing period. These gold deposits should belong to the type of magmatic hydrothermal gold deposits that were mainly occurred in the fractured altered rocks. Strata, structure/tectonic and magmatism are the three important factors that controlled the formation of Daxin gold deposits.
Key words: gold deposit, controlled - deposit factor, geological features, Daxin, Hunan province
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LIANG Dong, DAI Jian-Bin. The Geological Features and Controlled - Deposit factors on Daxin Gold Deposit in Hunan[J].J4, 2007, 15(2): 1-8.
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[1] 王高道.(湖南高家坳微细浸染型金矿床成矿地质特征.见:刘东生.)中国卡林型金矿[M].南京:南京大学出版社.1994.356-373. [2] 饶家荣,王纪恒,曹一中.湖南深部构造.湖南地质增刊7[J].1993.49-53. [3] 李已华,吴继承,周遗军.湘中白马山一龙山金矿带穹隆控矿规律分析[J].黄金地质,2004.10(4):32-36. [4] 饶家荣,骆检兰,易志军.锡矿山锑矿田幔一壳构造成矿模型及找矿预测[J].物探与化探,1999,23(4):241-249.
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