List of criteria for the geothermal survey of deep-reaching faults in Germany

被引:12
作者
Agemar, Thorsten [1 ]
Hese, Fabian [2 ]
Moeck, Inga [1 ]
Stober, Ingrid [3 ]
机构
[1] Leibniz Inst Angew Geophys, Stilleweg 2, Hannover, Germany
[2] Landesamt Landwirtschaft Umwelt & Landliche Raume, Hamburger Chaussee 25, D-24220 Flintbek, Germany
[3] KIT, Inst Angew Geowissensch, Kaiserstr 12, D-76131 Karlsruhe, Germany
来源
ZEITSCHRIFT DER DEUTSCHEN GESELLSCHAFT FUR GEOWISSENSCHAFTEN | 2017年 / 168卷 / 02期
关键词
fault; geothermal potential; deep groundwater; hot spring; stress field; reservoir; fracture systems; Germany; RHINE GRABEN; BLACK-FOREST; FLUID-FLOW; PERMEABILITY; ZONES; DEFORMATION; EVOLUTION; BASIN; WATER; ROCK;
D O I
10.1127/zdgg/2017/0084
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Disruptive deformations create deep subsurface faults, which may result in the formation of hydrothermal fluid pathways. Deep-reaching faults are promising targets for geothermal exploration. In Germany, the hydraulic properties of faults are usually not known when geothermal wells are planned. However, there are documented and plausible criteria to assess the geothermal potential of faults in advance. Experience gained from geologic exploration of faults confirms an empirical correlation between fault geometry and the distribution of geothermal resources. Geothermal surveys indicate that damage zones at fault terminations and interfering faults (e.g. relay ramps, crossing faults etc.) could represent favourable settings for exploration in critically stressed areas. Besides fault geometry and stress regime, additional criteria are outlined for the assessment of the geothermal potential of faults.
引用
收藏
页码:285 / 300
页数:16
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