王凯平, 雷崇利, 张培河. 三河尖井田地温异常形成机理[J]. 煤田地质与勘探, 1998, 26(1): 22-25.
引用本文: 王凯平, 雷崇利, 张培河. 三河尖井田地温异常形成机理[J]. 煤田地质与勘探, 1998, 26(1): 22-25.
Wang Kaiping, Lei Chongli, Zhang Peihe. THE FORMATION MECHANISM OF GEOTHERMAL ANOMALY IN SANHEJIAN MINE FIELD[J]. COAL GEOLOGY & EXPLORATION, 1998, 26(1): 22-25.
Citation: Wang Kaiping, Lei Chongli, Zhang Peihe. THE FORMATION MECHANISM OF GEOTHERMAL ANOMALY IN SANHEJIAN MINE FIELD[J]. COAL GEOLOGY & EXPLORATION, 1998, 26(1): 22-25.

三河尖井田地温异常形成机理

THE FORMATION MECHANISM OF GEOTHERMAL ANOMALY IN SANHEJIAN MINE FIELD

  • 摘要: 从热源、成热环境两方面对三河尖井田地温异常形成机理进行研究后认为,井田内煤系基底处于相对抬高的构造位置,使大地热流增大;不同热导率岩层的叠层式组合,使煤系聚集的热量不易散失;地下水运动微弱,所起的降温作用很小等因素是导致井田地温异常的主要原因。

     

    Abstract: The formation mechanism of geothermal anomaly in Sanhejian mine field is studied from both aspects:heat source and teat-forming environment,it is considered that the following factors are the main causes resulting the geothermal anomaly in mine field:the base of coal measures in mine field is located in relatively raised tectonic setting,resulting the increase of geothermal flux;the strata with different thermal conductivity are superimposed,and the heat concentrated in coal measures is not easy to escape,resulting the increase of geotemperature,the movement of groundwater is weak,it has a little influence of the drop in temperature,etc.

     

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