试论五大连池东焦得布矿水成控机理  

Forming mechanism of Dongjiaodebu mineral water in Wudalianchi,Heilongjiang Province

作　　者：张峰龙[1,2] 姜吉生[1,2] 王益良[1,2] 董学良 

机构地区：[1]黑龙江省九○四水文地质工程地质勘察院,黑龙江哈尔滨150027 [2]吉林大学环境与资源学院,吉林长春130026

出　　处：《吉林地质》2012年第2期113-116,共4页Jilin Geology

摘　　要：本文对五大连池的四大矿水区之一的东焦得布铁质重碳酸盐-碳酸矿水区的地下水区域流动系统、第四纪火山活动特点及封闭半封闭贮水贮气构造等四方面进行综合研究。分析了第四纪火山持续活动产生的CO2气体蓄积运逸到封闭半封闭贮水构造带并沿构造带进行区域性深循环,经历漫长的溶滤溶解作用而形成,又以极其缓慢的速度沿构造带进行排泄,从而形成了重碳酸型矿水。Through researched one of the four mineral water regions-Dongjiaodebu iron hydrocarbonate-carbonate mineral water area,focus on four aspects including groundwater flow system,Quaternary volcanic activity features and closed-semi-closed the water gas storage structure.Analyzed CO2 gas,produced by the Quaternary volcano continued activities,accumulated and transported into the closed-semi closed water storage tectonic belt,and along the tectonic belts cycled regional deeply,underwent the long dissolve function to form,and along the tectonic belt discharged with extremely slow speed,thus forming a bicarbonate type mineral water.

关 键 词：东焦得布 矿水 成控机理 

分 类 号：TK521[动力工程及工程热物理—热能工程]