|本期目录/Table of Contents|

[1]欧阳澍培,周晓成,何 苗,等.云南宁洱—通关火山区温泉水文地球化学与地震短临前兆异常特征研究[J].地震研究,2023,46(01):37-48.[doi:10.20015/j.cnki.ISSN1000-0666.2023.0005 ]
 OUYANG Shupei,ZHOU Xiaocheng,HE Miao,et al.The Characteristics of the Hydrogeochemical Seismic Anomaly of Hot Springs in the Ning'er-Tongguan Volcanic Area[J].Journal of Seismological Research,2023,46(01):37-48.[doi:10.20015/j.cnki.ISSN1000-0666.2023.0005 ]
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云南宁洱—通关火山区温泉水文地球化学与地震短临前兆异常特征研究(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
46
期数:
2023年01期
页码:
37-48
栏目:
地震地下流体监测预报理论及技术应用专栏
出版日期:
2023-01-01

文章信息/Info

Title:
The Characteristics of the Hydrogeochemical Seismic Anomaly of Hot Springs in the Ning'er-Tongguan Volcanic Area
作者:
欧阳澍培1周晓成1何 苗1天 娇1李静超1董金元1李 营1颜玉聪1刘峰立1姚炳宇1王昱文1曾召君1陈曲菲2罗志鑫1吉庚凤1
(1.中国地震局地震预测研究所 高压物理与地震科技联合实验室,北京 100036; 2.新疆维吾尔自治区消防救援总队 乌鲁木齐市消防救援支队经济技术开发区大队,新疆 乌鲁木齐 830009)
Author(s):
OUYANG Shupei1ZHOU Xiaocheng1HE Miao1TIAN Jiao1LI Jingchao1DONG Jinyuan1LI Ying1YAN Yucong1LIU Fengli1YAO Bingyu1WANG Yuwen1ZENG Zhaojun1CHEN Qufei2LUO Zhixin1JI Gengfeng1
(1.United Laboratory of High Pressure Physics and Earthquake Science,Institute of Earthquake Forecasting,China Earthquake Administration,Beijing 100036,China)(2.Economic and Technological Development Zone Brigade,Fire and Rescue Detachment of Urumqi,Fire and Rescue department of Xinjiang Uygur Autonomous Region,Urumqi 830009,Xinjiang,China)
关键词:
温泉 水文地球化学 前兆异常 宁洱—通关火山区
Keywords:
hot-spring fluids hydrogeochemistry earthquake precursors the Ning'er-Tongguan volcanic area
分类号:
P315.724
DOI:
10.20015/j.cnki.ISSN1000-0666.2023.0005
摘要:
温泉水文地球化学监测可以提供很好的地震短临前兆异常信息。通过采集云南宁洱—通关火山区8个温泉出露点的水样进行水化分析,研究了温泉水文地球化学变化与地震的关系。结果表明:①通关火山温泉有6种水化类型,分别是Na?Ca-HCO3、Na?Cl-HCO3、Na-HCO3、Ca-HCO3、Na?Ca-SO4?HCO3和Na?Ca-Cl?SO4型。② δ18O和δD值分别为12.69%~-10.80‰和-89.2%~-81.5‰,表明研究区温泉水主要补给来源是大气降水,补给高程为2.0~2.7 km。③温泉的热储温度在81.7℃~86.3℃,热循环深度为1.1~1.3 km,其热源主要是地热增温及岩浆热。④ 2020年云南绿春ML4.4地震前,清平热水塘和西萨温泉的Na+、Cl-、SO2-4浓度均出现不同幅度的升高; 2021年双柏MS5.2地震前,清平、西萨、厄里3个连续监测点的Na+、Cl-、SO2-4短临前兆异常响应较为明显,表现为震前5~10 d离子浓度异常升高,震后离子浓度降低至平均值上下波动。⑤短临前兆异常主要原因是震前区域构造应力场发生了变化,断裂带裂隙通透性改变,岩层渗透率增加,断裂带内的水循环发生变化,原有的水-岩反应平衡状态改变,温泉水各组分含量相应发生了变化。 关键词:温泉; 水文地球化学; 前兆异常; 宁洱—通关火山区
Abstract:
The hydrogeochemial characteristics reflect information of seismic activities.In this study,eight hot spring sites in Ning'er-Tongguan volcanic area of Yunnan Province are selected for sampling and analysis.The results are as follows:① Volcanic hot springs in Tongguan belong to six hydrogeochemical types:Na?Ca-HCO3,Na?Cl-HCO3,Na-HCO3,Ca-HCO3,Na?Ca-SO4?HCO3 and Na?Ca-Cl?SO4.②The oxygen and hydrogen isotopes(δ18O and δD)range from 12.69‰ to-10.80‰ and-89.2‰ to-81.5‰ respectively.This indicates that the main source of the recharge for the hot springs is precipitation,and the recharge elevation ranges from 2.0 km to 2.7 km.③ The geothermal reservoir temperature of the hot springs,calculated by the hydrogeochemical temperature scale,ranges from 52.5 ℃ to 56.4 ℃.The circulation depth of hot springs was estimated from 1.1 km to 1.3 km.The main source of heat is from geothermal gradient and magma heat.④Before the 2020 Luchun Earthquake,The concentration of Na+,Cl-,SO2-4in Qingping Hot Spring and Xisa Hot Spring rose synchronously.The Na+,Cl-,SO2-4ions on three monitoring sites responded to the 2021 Shuangbai Earthquake.These ions had risen 5-10 days before the Shuangbai Earthquake,then fell to the average level after the earthquake.The seismic anomaly was related to the epicentral distance and earthquake magnitude.⑤The variation of tectonic stress field increased the permeability of the stratum,and then the water in the lower aquifer mixed up with that in the upper aquifer,therefore changed the compositions of the hot-spring water.And the short-term and impending seismic precursors appeared.

参考文献/References:

车用太,鱼金子.2014.地壳流体对地震活动的影响与控制作用[J].国际地震动态,(8):1-9.
方维萱,胡瑞忠,谢桂青,等.2002.云南哀牢山地区构造岩石地层单元及其构造演化[J].大地构造与成矿学,(1):28-36.
郭清海.2020.岩浆热源型地热系统及其水文地球化学判据[J].地质学报,94(12):3544-3554.
[HJ1.9mm]李学伦,孙效功,王永红.1997.山东半岛温泉的分布规律与成因[J].青岛海洋大学学报,27(3):389-396.
牟保磊.1999.元素地球化学[M].北京:北京大学出版社.
潘明,吕勇,郝彦珍,等.2015.云南昌宁玉地里温泉水文地球化学特征及形成模式[J].地球与环境,43(1):98-103.
庞忠和.1987.地下水运动对地温场的影响——研究进展综述[J].水文地质工程地质,(3):30-34.
田雷,余怀忠,周志华.2018.基于水化学分析的滇17井流体异常识别及应用[J].地震研究,41(4):551-558.
汪集旸,熊亮萍,庞忠和.1993.中低温对流型地热系统[M].北京:科学出版社.
王皓,柴蕊.2009.地热温标在地热系统中的应用研究[J].河北工程大学学报(自然科学版),26(3):54-58.
王恒纯.1991.同位素水文地质概论[M].北京:地质出版社.
王晓翠.2016.云南沘江沿岸温泉水化学特征和水文地球化学模拟研究[D].北京:中国地质大学(北京).
王云,赵慈平,李其林,等.2018.滇东南楔形构造区典型地热流体地球化学特征研究[J].地震研究,41(4):534-543.
吴坤罡.2016.云南思茅地块活动构造体系及成因机制研究[D].北京:中国地质大学(北京).
许佩瑶,丁志农.1997.含锶饮用天然矿泉水的形成[J].勘察科学技术,(5):36-38.
颜玉聪,周晓成,朱成英,等.2022.2020年新疆伽师MS6.4地震前后伽师地区温泉水文地球化学特征[J].地震研究,45(2):229-240.
张贵玲,角媛梅,何礼平,等.2015.中国西南地区降水氢氧同位素研究进展与展望[J].冰川冻土,37(4):1094-1103.
张洪平,刘恩凯,王东升,等.1991.中国大气降水稳定同位素组成及影响因素[C]//中国地质科学院水文地质工程地质研究所文集,(7):106-115.
张柯,马浩明.2002.华南沿海温泉成因探讨[J].中山大学学报(自然科学版),41(1):82-86.
张彧齐.2020.云南思茅盆地泉水水文地球化学特征及成因研究[D].北京:中国地质大学(北京).
赵慈平,陈有丽,王云,等.2014.云南宁洱—通关火山区最上地壳地热场:构造和岩浆活动意义[J].岩石学报,30(12):3645-3656.
赵慈平,王云,周挚,等.2017.宁洱火山区壳内岩浆囊现今温度:来自CO2-CH4碳同位素地质温度计的估计[J].岩石学报,33(1):231-249.
Andrén M,Stockmann G,Skelton A, et al.2016.Coupling between mineral reactions,chemical changes in groundwater,and earthquakes in Iceland[J].Journal of Geophysical Research Solid Earth,121:2315-2337.
Clark M K,Royden L H.2000.Topographic ooze:Building the eastern margin of Tibet by lower crustal flow[J].Geology,28(8):703-706.
Craig H.1961.Isotopic variations in meteoric waters[J].Science,133(3465):1702-1703.
Du J,Cheng W,Zhang Y,et al.2006.Helium and carbon isotopic compositions of thermal springs in the earthquake zone of Sichuan,Southwestern China[J].Journal of Asian Earth Sciences,26(5):533-539.
Fournier R O.1977.Chemicalgeothermometers and mixing models for geothermal systems[J].Pergamon,5(1-4):41-50.
Giggenbach W F.1988.Geothermal solute equilibria.Derivation of Na-K-Mg-Ca geoindicators[J].Geochimica Et Cosmochimica Acta,52(12):2749-2765.
Li C,Zhou X C,Yan Y, et al.2021.Hydrogeochemical characteristics of hot springs and their short-term seismic precursor anomalies along the Xiaojiang Fault Zone,Southeast Tibet Plateau[J].Water,13(19):2638.
Liu L,Du J G,Zhou X C, et al.2012.Continuously observation of fault fluid geiochemistry after Yushu MS7.1 earthquake[J].Progress in Geophysics,27(3):888-893.
Pang Z,Kong Y,Li J, et al.2017.An isotopic geoindicator in the hydrological cycle[J].Procedia Earth and Planetary Science,17:534-537.
Shi Z,Shi Z,Yin G, et al.2014.Travertine deposits,deep thermal metamorphism and tectonic activity in the Longmenshan tectonic region,southwestern China[J].Tectonophysics,633(1):156-163.
Shi Z,Zhang H,Wang G.2020.Groundwater trace elements change induced by MS5.0 earthquake in Yunnan[J].Hydrology,581:124424.
Skelton A,Claesson L L,Wästeby N, et al.2019.Hydro-chemical changes before and after earthquakes based on long term measurements of multipleparameters at 2 sites in northern Iceland-A review[J].Journal of Geophysical Research Solid Earth,124:2702-2720.
Soto-Jiménez M F,Páez-Osuna F.2001.Distribution and normalization of heavy metal concentrations in mangrove and lagoonal sediments from Mazatlán harbor(SE gulf of California).Estuar Coast Shelf Sci,53:259-274.
Tian J,Pang Z,Liao D, et al.2021.Fluid geochemistry and its implications on the role of deep faults in the genesis of high temperature systems in the eastern edge of the Qinghai Tibet Plateau[J].Applied Geochemistry.
Wang B,Liu Y,Sun X, et al.2018.Hydrogeological and geochemical observations for earthquake prediction research in China:A brief overview[J].Geophysics,175(7):2541-2555.
Yu J,Zhang H,Yu F,et al.1984.Oxygen and hydrogen isotopic compositions of Meteoric Waters in the Eastern Part of Xizang[J].Geochemistry,3(2):93-101.
Zhang M,Xu S,Zhou X C,et al.2021.Deciphering a mantle degassing transect related with India-Asia continental convergence from the perspectiveof volatile origin and outgassing[J].Geochimica et Cosmochimica Acta,310: 61-78.
Zhang Y F,Tan H B,Zhang W J, et al.2015.A new geochemical Perspective on hydrochemical evolution of the Tibetan Geothermal System[J].Geochemistry International,53:1090-1106.
Zhou X C,Liu L,Chen Z, et al.2017.Gas geochemistry of the hot spring in the Litang Fault Zone,Southeast Tibetan Plateau[J].Applied Geochemistry,79:17-26.

备注/Memo

备注/Memo:
收稿日期:2022-03-30.
基金项目:国家重点研发计划(2017YFC1500501-05,2019YFC1509203)、国家自然科学基金面上项目(41673106,42073063,4193000170)和中国地震局地震预测研究所基本科研业务费(2021IEF0101,2021IEF1201)联合资助.
第一作者简介:欧阳澍培(1997-),硕士研究生在读,主要从事地震流体地球化学研究.E-mail:ouyangshupei888@163.com.
通讯作者简介:周晓成(1978-),研究员,主要从事构造地球化学、流体地球化学研究.E-mail:zhouxiaocheng188@163.com.
更新日期/Last Update: 2023-01-01