地热异常区

  • 网络geothermal anomalous area
地热异常区地热异常区
  1. 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 .

  2. 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 .

  3. 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 .

  4. 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

  5. 地热异常区的遥感信息识别

    Identification of Remote Sensing Information in Geothermal Abnormal Area

  6. 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 .

  7. 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 ″ .

  8. 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 .

  9. 这些变化所导致的异常就成为了解地下热储、圈定地热异常区、寻找地热田位置的重要标志之一。

    Those abnormities caused by the above variation are one of important symbols to understand underground heat storage , geothermic abnormity area confirmation and geothermic field position search .

  10. 利用水井测温方法确定恒温层温度,以恒温层的温度值作为湖顶地热异常区的下限值,用内插法勾绘温度等值线图,高于该下限值范围的即为地热异常区。

    By using well thermometry method , temperature of constant temperature strata is determined . Regarding temperature in constant temperature strata as the threshold value , geothermal abnormal areas are determined .

  11. 根据已知温泉产出的地质构造条件和地面测温等资料,进行地热异常区综合遥感预测,提出了7处地热异常的有利地段,从而为寻找地热水指出了方向。

    Based on the geological structure conditions of known hot springs and ground thermometric data , the comprehensive remote sensing prediction of geothermal abnormal area was carried out . Seven favorable geothermal abnormal areas were put forward and the direction for hot spring exploration was given .

  12. 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 .

  13. 鄂尔多斯盆地热演化程度异常分布区及形成时期探讨

    Research on region of maturation anomaly and formation time in Ordos basin

  14. 火山区的突发性地热异常特征与火山区的地质构造、火山成因、规模、类型等多种因素有关。

    The characters of the abrupt geothermal anomaly concern many factors such as geological structure , cause of volcanic formation , volcanic scope and type .