CAJ | 학술논문

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。
본문대오대련지적사대광수구지일적동초득포철질중탄산염-탄산광수구적지하수구역류동계통、제사기화산활동특점급봉폐반봉폐저수저기구조등사방면진행종합연구。분석료제사기화산지속활동산생적CO2기체축적운일도봉폐반봉폐저수구조대병연구조대진행구역성심순배,경력만장적용려용해작용이형성,우이겁기완만적속도연구조대진행배설,종이형성료중탄산형광수。
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.