陕西省山阳县王闫镇暖水川低温热水矿泉水化学特征及同位素分析  

Analysis of the chemical characteristics and isotope analysis of warm water and mineral water in Wangyan Town,Shanyang County,Shaanxi Province

作　　者：高超 李潇艳 张成 王佳武 Gao Chao;Li Xiaoyan;zhang Cheng;Wang Jiawu(Shaanxi Engineering Exploration Research Institute Co.,Ltd.,Xi'an 710068;Xi'an Geology and Mineral Exploration and Development Institute Co.,Ltd.,Xi'an 710100;Shaanxi Geology and Mineral Comprehensive Geology Brigade,Weinan 714000)

机构地区：[1]陕西工程勘察研究院有限公司,西安710068 [2]西安地质矿产勘查开发院有限公司,西安710100 [3]陕西地矿综合地质大队,渭南714000

出　　处：《陕西地质》2024年第1期50-53,共4页Geology of Shaanxi

摘　　要：陕西省山阳县王闫镇暖水川低温热水矿泉,沿近东西向的铁炉瓦-口头坪断层近南侧分布,赋存的热储层是断裂的下盘震旦系灯影组白云岩、白云质灰岩、灰岩、大理岩、砂岩,热盖层是断裂上盘震旦系陡山沱组千枚岩;矿泉水温29.5~30.5℃,属低温热水。低温热水矿泉主要接受大气降水补给,地下水沿裂隙溶隙运移,受阻水断裂的控制后,泉水由地下深部向上运移,在地形相对较低的沟谷部位以泉的形式排泄(溢出)地表成泉,热水流体属重碳酸钙镁型水。The low-temperature hot water mineral spring is located in Wangyan Town,Shanyang County,Shaanxi Province.Wang Yanzhen is approximately 15 km away,and the region features medium to low mountainous terrain.The mineral spring is mainly distributed along the southern side of the east-west iron furnace tile-oral flat fracture.The rock formations in the area include Dan Lanter Lantern Group Baiyun Rock,Baiyun West Rock,West Rock,Dali Rock,and sandstone.The hot spring cover is comprised of the Stead Mountain Group of the Sutan Sali Mountain.The essential low-temperature hot water mineral spring mainly receives atmospheric precipitation.Groundwater moves through the cleaner gap,is controlled by the blocked water,the spring water is moved upwards from the deep part of the ground,and in the form of a relatively low terrain in the form of spring(overflowing)the surface,the hot water fluid belongs to calcium magnesium bicarbonate type water.

关 键 词：山阳县 震旦系灯影组 低温热水 水化学特征 同位素 

分 类 号：O562.6[理学—原子与分子物理]