苏北盆地老子山地热田成因模式

J4 ›› 2012, Vol. 42 ›› Issue (2): 468-475.

苏北盆地老子山地热田成因模式

杨峰田^1,2, 庞忠和¹, 王彩会³, 段忠丰^1,2, 罗璐^1,2, 李义曼^1,2

1.中国科学院地质与地球物理研究所/工程地质力学重点实验室, 北京100029;
2.中国科学院研究生院, 北京100049;
3.江苏省地质调查研究院, 南京210018

收稿日期:2011-07-06 出版日期:2012-03-26 发布日期:2012-03-26
通讯作者: 庞忠和（1961-），男，研究员，博士生导师，主要从事水循环与水岩相互作用等方面的研究 E-mail:z.pang@mail.iggcas.ac.cn
作者简介:杨峰田(1983-)|男|博士研究生|主要从事水文地球化学与水岩相互作用等方面的研究|E-mail:yangfengtian@yeah.net
基金资助:
国家“863”计划项目（2008AA062303）

Genesis Model of Laozishan Geothermal Field, Subei Basin

Yang Feng-tian^{1, 2}, Pang Zhong-he¹, Wang Cai-hui³, Duan Zhong-feng^{1, 2},Luo Lu^{1, 2}, Li Yi-man^{1, 2}

1.Institute of Geology and Geophysics/Key Laboratory of Engineering Geomechanics, Chinese Academy of Sciences, Beijing100029, China;
2.Graduate University,Chinese Academy of Sciences, Beijing100049, China;
3.Geological Survey of Jiangsu Province, Nanjing210018, China

Received:2011-07-06 Online:2012-03-26 Published:2012-03-26

摘要/Abstract

摘要：

老子山地热田是苏北盆地的典型地热田之一,阐明其成因模式对于该地热田的进一步开发和热水资源的可持续利用具有一定的指导意义。基于大地热流测试和水文地球化学方法对其进行了系统研究。结果表明:该区大地热流背景值为63.9 mW/m²，地热水与浅层地下水和地表水之间在水化学和同位素组成上存在明显差异。经分析，该地热系统属于中低温对流型。其补给区位于距地热田南部约60 km处的盱眙－张八岭一带的丘陵地区，热储温度为73~120 ℃，循环深度为2 350~4 200 m，循环周期约为7 800 a，热水在区内NNE－SSW向与NW－SE向断裂的交汇处上涌，形成地热田。

关键词: 苏北盆地, 老子山, 地热田, 成因模式, 中低温对流型地热系统

Abstract:

Laozishan is a typical geothermal field in Subei Basin. We conducted a systematic study to explore into the genesis mechanism through heat flow measurement and hydrogeochemical investigation, for the purpose of further exploration and sustainable use of the geothermal resources. Results show that the background heat flow is 63.9 mW/m², and the hydrochemical and isotopic compositions of the thermal water are different from those of the shallow groundwater and surface water. Based on these data, the genesis model of the geothermal field has been postulated to be a low-medium temperature geothermal system of convective type. The recharge area is located in the Zhangbaling to the Xuyi mountain chain with a distance of about 60 km to the south of the geothermal field. The reservoir temperature of the geothermal field has been estimated to be 73-120 ℃, with a water circulation depth of 2 350-4 200 m. The water age is about 7 800 a.The thermal water flows upward in Laozishan area in the intersection zones of the faults striking NNE-SSW and NW-SE.

Key words: Subei basin, Laozishan, geothermal fields, genesis model, low-medium temperature geothermal system of convective type

中图分类号:

P641.3

杨峰田, 庞忠和, 王彩会, 段忠丰, 罗璐, 李义曼. 苏北盆地老子山地热田成因模式[J]. J4, 2012, 42(2): 468-475.

YANG Feng-tian, PANG Zhong-he, WANG Cai-hui, DUAN Zhong-feng, LUO Lu, LI Yi-man. Genesis Model of Laozishan Geothermal Field, Subei Basin[J]. J4, 2012, 42(2): 468-475.

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