geothermal heat flow meaning in Chinese
地热流
Examples
- Based on analysis of geologic foundation record about pingzhuang basin , a lot of sino - foreign geothermal geology record and investigation of field geology , measuring of ground temperature in person and geo - chemical analysis of ascension spring , gushing water of fault , the fact that the anomaly of geothermal gradient of pingzhuang basin , which is in region of low geothermal gradient , is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out . after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys , the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed . the sound condition of transmissibility fault and feeding water source , which are imperative in formation of the low - medium temperature geothermal system of convective type , is possessed in pingzhuang basin
通过对平庄盆地基础地质资料、国内外大量地热地质资料的分析和野外地质调查、矿井实测地温以及上升泉、断层涌水的地球化学分析等工作基础上，指出地处低地温梯度背景区的平庄盆地地温梯度异常是由于盆地基底隆起和坳陷引起传导型大地热流再分配所致；运用州sys数值模拟了大地热流向地表传导背景下的盆地地温场，从而揭示了盆地基底(义县组)顶界面地温分布特征；阐明了盆地具有形成中低温对流型地热系统所必需的导水断裂、补给水源等的良好条件，中低温对流型地热系统是地热勘查的主要对象；圈定了平庄盆地北部朝阳沟?骆驼营子地热勘查远景区。