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小秦岭大湖金矿成矿流体特征及矿床成因

陈莉, 毛景文, 叶会寿

陈莉, 毛景文, 叶会寿. 小秦岭大湖金矿成矿流体特征及矿床成因[J]. 沉积与特提斯地质, 2010, 30(2): 103-107.
引用本文: 陈莉, 毛景文, 叶会寿. 小秦岭大湖金矿成矿流体特征及矿床成因[J]. 沉积与特提斯地质, 2010, 30(2): 103-107.
CHEN Li, MAO Jing-wen, YE Hui-shou. Ore-forming fluids and ore genesis of the Dahu gold deposit in the Xiaoqinling gold field[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(2): 103-107.
Citation: CHEN Li, MAO Jing-wen, YE Hui-shou. Ore-forming fluids and ore genesis of the Dahu gold deposit in the Xiaoqinling gold field[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(2): 103-107.

小秦岭大湖金矿成矿流体特征及矿床成因

Ore-forming fluids and ore genesis of the Dahu gold deposit in the Xiaoqinling gold field

  • 摘要: 本文运用流体包裹体岩相学、流体包裹体温度测试、流体包裹体成分分析等方法,讨论了大湖金矿床成矿流体的特征和成矿机理。
    Abstract: The Xiaoqinling gold field on the southern margin of the North China platform is one of important gold metallogenic areas in China,where the gold deposits of varying sizes have been explored,including more than one thousand gold-bearing quartz veins and more than forty gold deposits.Exemplified by the Dahu gold deposit in the northern gold belt of the Xiaoqinling gold field,the present paper gives a systematic study of fluid inclusions so as to examine the ore-forming fluids and metallogenic mechanism of the Dahu gold deposit on the basis of petrography,homogenization temperatures and compositions of fluid inclusions.
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出版历程
  • 发布日期:  2010-06-29

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