江西修水县辉煌地热地质特征及成因分析  

GEOLOGICAL FEATURES AND CAUSES OF THE HUIHUANG GEOTHERM IN XIUSHUI,JIANGXI

作　　者：梅惠呈[1] 李忠社[1] 蔡亮[1] 

机构地区：[1]江西省地质矿产勘查开发局九一五地质大队,南昌330002

出　　处：《地质灾害与环境保护》2013年第2期49-53,共5页Journal of Geological Hazards and Environment Preservation

摘　　要：辉煌地下热水属低温地热资源中的温热水。埋藏浅,热储形态简单,平面分布为一个由构造破碎带组成的椭圆状。辉煌温泉的异常地热主要来源于九岭花岗闪长岩体深部余热与北东向活动性断裂带的深循环热有关。The Huihuang underground hot water, belonging to low-temperature geothermal resources and buried in shallow geothermal reservoirs, is distributed in a flat oval-shape composed of structural fracture zones. The study shows that the Huihuang geotherm takes source from the afterheat in deep Jiuling granodiorite and the circulating heat in the deep active North-East fault zone.

关 键 词：地热 地质特征 成因 辉煌 

分 类 号：P641.11[天文地球—地质矿产勘探]