地热异常

  • 网络geothermal anomaly
地热异常地热异常
  1. 利用浅层测温确定了地热异常带。

    Using shallow temperature probe , geothermal anomaly belts are determined .

  2. 扬子准地台区是本省地热异常的主要分布区。

    Yangtze paraplatform is a major distribution region for geothermal anomaly .

  3. 2003年甘肃山丹&民乐MS6.0地震前平凉地热异常特征

    Anomalous features of geotherm in Pingliang before the 2003 Shandan-Minle M_S 6.0 earthquake , Gansu province

  4. 西安及其周围地区是地热异常区。

    Xi'an City and its ambient area are geothermal anomaly regions .

  5. 中亚的地热异常与强震前兆

    Terrestrial heat anomalies and strong earthquake precursors in Central Asia

  6. 地热异常与地震活动关系的综合分析

    Study of the relationship between geothermal anomalies and seismic activity

  7. 漳州盆地地热异常与重磁异常的相关性研究

    Correlative research between geothermal and gravity-magnetic anomalies in Zhangzhou Basin

  8. 结果,发现地球水化学与地温场存在密切关系,并依此确定了地热异常区和深部断裂构造。

    Geothermal anomaly area and deep seated faults are determined .

  9. 河北怀来ML4.4地震前的地热异常

    Geothermal Anomaly before Huailai , Hebei , Earthquake of M_L4.4

  10. 地面红外辐射土壤测温法在地热异常区的应用

    Survey temperature of the infrared radiation in the surface soil

  11. 大同&阳高地震地热异常与机理初探

    A study on the geothermal anomaly and of the datong & yanggao earthquake

  12. 地热异常区的遥感信息识别

    Identification of Remote Sensing Information in Geothermal Abnormal Area

  13. 雷州半岛局部地热异常及其形成机制

    Local geothermal anomalies and their formation mechanisms on Leizhou peninsula , South China

  14. 江苏地温水温场特征及地热异常分布规律与控制条件探讨

    Geotemperature Field Feature and Distribution Law of Geothermal Anomaly and Their Control Conditions

  15. 地热异常的水槽模型实验

    Model experiment of geothermal anomaly with water tank

  16. 鸡东盆地地热异常与地下热水分布规律研究

    Research on Geothermal Abnormalism and Distributive Law of Underground Hot Water in Jidong Basin

  17. 导热断裂与低热导率岩层组合容易形成地热异常,形成层状热储和带状热储。

    Combination of heat conducting faults and low conductive stratas easily form geothermal anomaly region .

  18. 火山区突发性地热异常热红外传输机理研究

    Research on Transmission Mechanism of Thermal Infrared Remote Sensing for Abrupt Geothermal Anomaly in Volcanic Region

  19. 河北省煤矿区地热异常与地热资源开发前景浅议

    A Discussion on Geothermal Resource and Prospects of Its Development in Coal Mines of Hebei Province

  20. 地下热水的评价因子为地热异常程度及热流体质量。

    Geothermal water resource can be assessed by the abnormity degree of geothermal and thermal flow quality .

  21. 西安地区活动构造与地热异常分布关系及地热开发利用

    The Relationship between Active Structure and Geothermal Anomaly Distribution and Exploitation for the Geothermal Resources in the Xi'an Area

  22. 腾冲不但是现代火山活动区,也是地热异常区,这里温泉、热泉及喷气孔到处可见。

    Tengchong is a famous active area of the modern volcano , where the hydrothermal activity is very violent .

  23. 实验研究证实,在火山喷发前兆期,火山区有明显的突发性地热异常现象。

    A lot of experiments have proved that there is an obvious abrupt geothermal anomaly in volcanic region before volcanic eruption .

  24. 榆中盆地地热异常区,处于区域性地热背景之上,具有深源热机制。

    The geothermal anomalous area of Yuzhong Basin is on the regional geothermal background and related to deep source geothermal mechanism .

  25. 邯邢东部平原区温增温率3℃/100m,被任为是不宜开采利用的非地热异常区。

    The geothermal gradient in eastern Hanxing plain is 3oC / 100m and it was regarded as unexploitable ″ non-geothermal anomalous area ″ .

  26. 从古地热异常形成机制出发,提出热液变质作用模式以及古地热-变质系统的概念。

    Based on the mechanism of palaeogeothermal field formation , a hydrothermal metamorphic mode and the concept of palaeogeothermal metamorphic system are presented .

  27. 地热异常分布主要受区域构造因素控制,断裂导热是本区地热异常的主要特点。

    The anomalies are controlled by tectonic factors ; fault heat conduction is the major feature of the geothermal anomaly in the area .

  28. 地热异常及地热田的热源主要来自地下深处经自然增温而形成的热量。

    The heat sources of geotemperature anomaly and geothermal fields originate from quantity of heat which is formed by natural temperature increment in depth .

  29. 本文以水文地球化学观点和方法,对冀中拗陷地热异常区深井网多井孔热水化学观测资料进行了计算处理。

    In this paper , data of hydro-chemical observation obtained from deep wells in the geothermal anomaly area of Central Hebei Depression are analysed .

  30. 河北省部分煤矿区存在地热异常现象,地温梯度最高可达6℃/100m,形成矿井热害。

    Abnormal geotemperatures exist in part of coal mines in Hebei Province . The highest gradient of rock temperature is 6 ℃ / 100m .