The relation between geological structure and heat-generating in western area of Guilin
The relation between geological structure and heat-generating in western area of Guilin
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发表时间：
2001
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通讯作者：
Miao Zhong-ling
中科院分区：
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作者：
Miao Zhong-ling
通过对桂西地区遥感、地质构造和水地质的大量研究，发现地热主要与裂缝有关。泉水沿裂缝分布，发热受龙神—永福断裂带控制，龙神—永福断裂带是主要的导热蓄热构造。两江-渡头多重向斜的二级褶皱和层间破碎带也是重要的储热构造。大多数储热库都是断层裂缝型储热库。最有利的产热位置是龙神—永福断裂带，该断裂带拉力作用，并向东北、西北、东西向相互作用。
By an enormous study of remote sensing, geological structure and watergeology in west Guilin, it is found that geoheat is mainly relative to fractures. Springs distribute along fractures.Heat-generating is controlled by Longshen-Yongfu fault zone.Longshen-Yongfu fault zone is the main heat-conducting and heat-storage structure. The second -order fold and fracture zone between layers in Liangjiang-Dutou multiple syncline are also important heat-storage structure. The majority of heat-storage reservoirs are fault-fractures. The most advantageous position where heat generates is Longshen-Yongfu fault which acts tensile and interacts northeastwards, northwestwards and east-westwards.