摘要
争光金矿床是黑龙江省近年来在其西北部地区发现的一个中(大)型的热液-构造蚀变岩型金矿床。文章论述了争光金矿床岩石赋水特征及其地下水补径排条件,认为采用"大井"法计算露采场基岩裂隙水水量是适宜的,其水文地质参数确定合理。
Zhengguang Au deposit is a medium （large） sized hydrothermally altered cataclastic rock type Au deposit discovered in northwest Heilongjiang province.According to occurrence characteristics of water in rocks of Zhengguang Au deposit and supply,run-off and drainage condition of the water it is proper to adopt ＂big well＂ method for calculation of fissure water volume of the bed rock.The hydrogeological parameter is reasonable.
出处
《地质找矿论丛》
CAS
CSCD
2014年第2期299-304,共6页
Contributions to Geology and Mineral Resources Research
关键词
争光金矿床
含水岩组划分
地下水动态
“大井”法计算
参数选择
黑龙江
Zhengguang Au deposit
division of water-bearing rock formations
dynamic state of groundwater
Big well calculation method
choice of parameter
Heilongjiang province
