ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
江汉盆地潜江凹陷王场地区深层卤水水化学特征及成因研究
  
关键词:Qianjiang sag  underground brine  water chemistry  characteristic coefficient  material source
基金项目:国家自然科学基金项目(编号: U20A2092; 42002106);中央级公益性科研院所基本科研业务费专项(编号: KK2005);中国地质调查局地质调查项目(编号: DD20190816; DD20190606)
作者单位E-mail
薛燕 长江大学资源与环境学院 xy15122677013@163.com 
王春连 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室 wangchunlian312@ 163.com 
刘殿鹤 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室
北京大学地球与空间科学学院 
 
王九一 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室  
颜开 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室
冰岛大学地球科学学院 
 
彭琰聪 长江大学资源与环境学院  
高绣纺 长江大学资源与环境学院  
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摘要:
Hydrochemical Characteristics and Genesis of Deep Brines in Wangchang Area, Qianjiang Depression, Jianghan Basin
      There are strategic key mineral resources such as lithium, rubidium and cesium in oilfield brine of sedimentary basin. In this study, 18 underground brine samples from the Wangchang area in Qianjiang depression, Jianghan Basin were collected. Their chemical composition was tested, hydrochemical characteristics, element correlation, and characteristic coefficients were analyzed, and the genesis of deep brine in this area was discussed. The brine in the study area is found in the sandstone of the Paleogene Qianjiang Formation. The average total dissolved solid (TDS) concentration is 260.04 g/L, while the hydrochemistry type is Cl-Na, and the pH value is between 7.03 and 8.01. The TDS of brine in Qianjiang depression decreases yearly, which may be related to water injection. The contents of Na and Cl were positively correlated with TDS, and the contents of Li, K, B, and Br increased with an increase in TDS, while the content of Ca decreased with an increase in TDS, which may clarify the evaporation and concentration processes of the primary sedimentary brine. The high sodium-chloride coefficient (1.09~1.21) and chloro-bromine coefficient (480~1547.60), and the low potassium-chloride coefficient (3.75~14.82) indicate the contributions from the dissolution of stone salt. The fluctuating Ca/Mg coefficient and desulphurization coefficient reflect the uneven sealing and metamorphic degree, and the sealing and metamorphic degree increases from the first subduction to the fourth subduction. The underground brine in the study area is the primary evaporative deposit of the continental salt lake, which is supplemented by the obvious source of stone salt leaching. The overall sealing of the reservoir space is poor and the metamorphism degree is low.
XUE Yan,WANG Chun-lian,LIU Dian-he,WANG Jiu-yi,YAN Kai,PENG Yan-cong,GAO Xiu-fang.2022.Hydrochemical Characteristics and Genesis of Deep Brines in Wangchang Area, Qianjiang Depression, Jianghan Basin[J].Acta Geoscientica Sinica,43(3):347-358.
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