首页> 外文会议>Asia Current Research on Fluid Inclusion Meeting >ORE-FORMING FLUID CHARACTERISTICS OF THE JIJIAWA GOLD DEPOSIT IN HENAN PROVINCE
【24h】

ORE-FORMING FLUID CHARACTERISTICS OF THE JIJIAWA GOLD DEPOSIT IN HENAN PROVINCE

机译:河南省吉济瓦金矿床的矿石形成流体特征

获取原文

摘要

The Jijiawa gold deposit, Henan Province, is located in the western part of the Xiong?er moun- tain gold polymetallic ore concentration area. The mining stratas are consisted of the Taihua Group of Neoarchean, which mainly are biotite plagioclase gneiss, long oblique angle gneiss and shallow parti- cle rock, and the Mesoproterozoic Xiong?er Group, which mainly are amygdaloidal andesite, porphyri- es andesite and dacite. And the intrusive rocks are mainly diabasic dike in the Mesoproterozoic Xiong?er Group. SN and NE trend fault segments are very well developed in the deposit area, and they are the main ore-controlling structure.
机译:河南省琼江金矿床位于熊的西部,雄厚的金多金属矿石浓度面积。矿业斯特拉塔斯由太监群体的新化,主要是Biotite Plagioclase环球菌,长倾斜角球和浅层岩石,以及Mesoproterozoice Xiong?ER组,主要是杏仁晶体,卟啉骨,卟啉和粘土。并且侵入式岩石主要是中间蛋白巨蜥的糖尿病堤防彼得·彼得群。 SN和NE趋势故障段在沉积物区内非常开发,它们是主要的矿石控制结构。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号