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依兰—伊通断裂温泉带地球化学特征及地震活动性研究

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通过对依兰―伊通断裂上神农温泉、鳖龙温泉、乔屯温泉等8个地下2 000 m左右的温泉点进行研究,分析温泉水水质类型、补给来源、水-岩石平衡状态及循环深度,讨论温泉水深循环对地震活动性的影响.同时,对该断裂附近的温泉水进行化验,分析地下温泉水Na+、HCO3-、SO42-、Cl-等离子的含量及变化,探讨与断裂带附近的地震活动之间的关系.得出初步研究结论:研究区内温泉水化学分析数据差异较大,北东方向的温泉TDS和阴阳离子浓度较高,向南西逐渐递减;近年来,温泉温度呈递减趋势,地震活动较少;研究区内TDS含量、主要离子含量等指标呈现空间分布特征,在空间分布上受活动构造控制较明显.
Research on Geochemical Characteristics and Seismicity of Yilan-Yitong Fault Hot Spring Belt
Based on the research of 8 hot spring spots about 2000 meters underground,such as Shennong Hot Spring,Bielong Hot Spring and Qiaotun Hot Spring on Yilan-Yitong Fault,this article analyzes the water quality type,supply source,water rock equilibrium state and circulation depth of hot spring water,and discusses the impact of hot spring water depth circulation on seismicity.At the same time,laboratory tests are conducted on the hot spring water near the fault to analyze,the contents and changes of Na+,HCO3-,SO42-,Cl-plasma in the under-ground hot spring water,and to explore the relationship between the hot spring water and the seismic activity near the fault zone.A preliminary conclusion is drawn:There are significant differences in the hydrochemical analysis data of hot springs within the research area,,and the concentrations of TDS and anions are higher in the northeast direction,and gradually decrease in the southwest direction;The temperature of hot spring has decreased in recent years,and the seismic activity is less;The contents of TDS and main ions in the research area show spatial distribu-tion characteristics,which are obviously controlled by active structures in spatial distribution.

Yilan-Yitong FaultHot springGeochemistrySeismicity

巴艳芳、马铭志、李雪梅

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吉林地震监测中心站 吉林省吉林市 132108

吉林省地震局 吉林长春 130117

依兰—伊通断裂 温泉 地球化学 地震活动性

2024

科技资讯
北京国际科技服务中心 北京合作创新国际科技服务中心

科技资讯

影响因子:0.51
ISSN:1672-3791
年,卷(期):2024.22(16)