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陕西老湾沟金矿地质特征及控矿因素分析
引用本文:白兆华,梅 旭,王 谦,尚金泉,庄红红.陕西老湾沟金矿地质特征及控矿因素分析[J].甘肃地质学报,2013,22(4):63-68.
作者姓名:白兆华  梅 旭  王 谦  尚金泉  庄红红
作者单位:[1]陕西省核工业集团公司二一一大队,陕西西安710024 [2]甘肃省有色金属地质勘查局兰州矿产勘查院,甘肃兰州730046 [3]金川集团有限公司,甘肃金昌737104 [4]陕西省核工业集团公司二一四大队,陕西城固723200
基金项目:中央基金项目,陕西省凤县梁山沟一老湾沟地区金矿普查
摘    要:老湾沟金矿位于秦岭褶皱系礼县-柞水海西褶皱带东段西部,处于唐藏-丹凤-商南大断裂带和礼县-凤镇-山阳大断裂带之间,属凤太多金属成矿带。通过对区域地质特征和老湾沟地区金矿的地层、构造、岩性及围岩蚀变等矿床地质特征研究分析,结合以往在该地区的工作成果及认识,认为该地区矿体受断裂破碎带控制,金矿化在构造带中以浸染状分布于硫化物石英细脉、网脉中,是构造蚀变岩型金矿。在总结矿床地质特征的基础上,进一步对老湾沟金矿进行了控矿因素分析。

关 键 词:老湾沟金矿  地质特征  控矿因素

GEOLOGICAL FEATURES AND ORE-CONTROL FACTORS OF LAOWANGOU GOLD DEPOSIT IN SHANXI PROVINCE
BAI Zhao-hua,MEI xu,WANG qian,SHANG jin-quan,ZHUANG hong-hong.GEOLOGICAL FEATURES AND ORE-CONTROL FACTORS OF LAOWANGOU GOLD DEPOSIT IN SHANXI PROVINCE[J].Acta Geologica Gansu,2013,22(4):63-68.
Authors:BAI Zhao-hua  MEI xu  WANG qian  SHANG jin-quan  ZHUANG hong-hong
Institution:1. 211 Battalion, Shanxi Nuclear Industry Group Company, X i'an 710024, China; 2. Gansu Bureau of Geology and Exploration for Nonferrous Metals, Lanzhou 730046, China; 3. Jinchuan Group CO.,LTD., Jinchang 737104, China; 4. 214 Battalion, Shanxi Nuclear Industry Group Company, Chenggu 723200, China)
Abstract:Laowanggou gold deposit is located in the west of east Hercynian Lixian-Zhashui fold belt, which belongs to Qinling fold system between Tangzang-Danfeng-Shangnan fault and Lixian-Fengzhen-Shanyang fault. According to the analysis on regional geological features and ore deposit geological characteristics of Laowangou, such as the strata, tectonic, lithology, and wall rock alteration and so on, the orebody should be controlled by the fault fracture, the gold mineralization disseminated in sulfide quartz veinlet and nets of arteries of tectonic belt. It is the tectonic altered rock type gold deposit.
Keywords:Laowangou gold deposit  geological features  ore-control factors
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