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1)  active hydrothermal area
活动水热区;现代水热区
2)  hydrothermal area
热水活动区
3)  hypothermal water area
低热水区
4)  hydrothermal activity
热水活动
1.
It is suggested that the hydrothermal activity in the Minami—Ensei area shows a “philo continental” property.
冲绳海槽南奄西热水活动区位于奄美大岛西约140km的南奄西海丘西坡(28°23′~255′N,127°375~395′E)。
5)  hydrothermal activity
水热活动
1.
It is indicated from the preliminary analysis that the intensity of the hydrothermal activity progressively decrease from south to north,obviously appearing as the water temperature drop,thespring sedimentdecrease,PH value change from alkaline to neutralit.
本文探讨康定本格措景区热矿水的水热活动变化规律,热储特征和水化学组分的形成及变化。
2.
On the analysis of the relationship among the hydrothermal activity in Zhangzhou geothermal field, its geological structure and comprehensive geophysical fields, such as theseismic sounding, gravity, geomagnetic,geoelectric and seismicity, we come to the conclusion that the Zhangzhou geothermal field is a convective hydrothermal system generated by the extreme heal flow.
本文通过漳州地热田及其周围地区的水热活动、地质构造特征及人工爆破、重力、地磁、电姓结构、地震活动姓等综合地球物理场之间关系分析,得出漳州地热田是高热异常背景下产生的对流型水热系统:深切到上地慢的NE向长乐-南澳断裂、NW向九龙江断裂及E-W向南靖-厦门断裂控制了地下水的深循环,使大气降水得以下渗到>3km深度,被地温加热并富集起来,在静水压力作用下沿通道-断裂带的交汇部位上涌。
6)  active rgion heating
活动区加热
补充资料:地下水水资源评价(见水资源评价)


地下水水资源评价(见水资源评价)


  d ixiashui shuiziyuan Ping】ia地下水水资源评价见水资源评价。
  
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