内蒙古自治区乌拉特前旗浅层盐卤水成因分析  

Genesis analysis of shallow brine in the south of Xin'an town,Urad Front Banner,Inner Mongolia Autonomous Region

作　　者：肖长来[1] 刘金锋[1] 邱淑伟[1] 张楠[1] 

机构地区：[1]吉林大学环境与资源学院,吉林长春130026

出　　处：《西安石油大学学报（自然科学版）》2012年第4期13-18,113,共6页Journal of Xi’an Shiyou University（Natural Science Edition）

基　　金：国家"十一五"科技支撑项目(编号:2007BAB28B04-03)

摘　　要：在研究河套地区古地理和古气候的基础上,通过地下水的离子系数特征分析、PHREEQC反向模拟、化学演化过程对比,揭示内蒙古自治区乌拉特前旗的浅层盐卤水是由深层高矿化水沿着断裂向上侵染而成.Based on studying paleo-geography and paleo-climate in Hetao area,it is held that the shallow brine in the studied area was from high mineralized water in deep formation according to the analysis of ion coefficient characteristics,PHREEQC inverse simulation and chemical evolution process contrast of the ground water.The deep high mineralized water moved up along faults to the studied area.

关 键 词：盐卤水 成因 离子系数 PHREEQC 化学演化 

分 类 号：P641.5[天文地球—地质矿产勘探]