热田区
- 网络Atsuta
热田区
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结合大地构造和岩石圈深部地球动力学过程,探讨了热田区深部热源成因和地热资源的开发和应用前景。
According to the geotectonics and geodynamic process in the deep lithosphere , the origin of the deep thermal source , the developments and utilizations of the geothermal resources in this geothermal field are discussed in the paper .
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温度场研究表明,热田中心区具有最高温度和最大的地温梯度,此乃漳州盆地的排泄区。
Temperature pattern shows that the highest temperature and geothermal gradient appears in the central part of the Field , which is the discharge area of the Zhangzhou Basin .