黑龙江省老柞山金矿床东矿带东部水文地质特征  

Heilongjiang Province Laozuoshan Gold Ore Deposit East Ore Belt East Hydrology Geologycal Feature

作　　者：刘喜友 刘洪军[2] 代文玉 

机构地区：[1]黑龙江省有色金属地质勘查七0一队,黑龙江桦南县154400 [2]黑龙江省有色金属地质勘查七0二队,牡丹江157021 [3]黑龙江省有色金属地质矿产勘查研究总院,哈尔滨150046

出　　处：《黄金科学技术》2007年第2期9-14,共6页Gold Science and Technology

摘　　要：在《老柞山金矿区东西矿带勘探报告》基础上,结合作者多年的矿区水文地质工作经验,对东矿带东部构造裂隙含水层提出了新的认识,确认了F12断层下盘构造裂隙含水带的存在。This article is on the foundation of ＂Laozuoshan gold ore area east weast ore belt exploration rports＂, unifies the author many year ore area hydrology geology work experience, the streture crevasse water -beating stratum proposed to the east ore belt east ,confirmed F12 fault sole structure crevasse water- beating zone existence.

关 键 词：东矿带东部 构造裂隙含水带 F12断层 

分 类 号：P618.51[天文地球—矿床学]