2014
DOI: 10.1016/j.geothermics.2014.03.003
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Potential for enhanced geothermal systems in low permeability limestones – stimulation strategies for the Western Malm karst (Bavaria)

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Cited by 20 publications
(16 citation statements)
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“…The Molasse basin is a foreland basin north of the Alps that formed due to continental collision. As a target geothermal reservoir formation, the Upper Jurassic Malm underlies the Molasse sediments and is confined by the Mesozoic crystalline basement Mavko et al (2003) and the bulk modulus of titanium dioxid is taken from Carmichael (1984 (Hofmann et al, 2014). The massive facies is mainly dolomitized and has a high permeability, due to recrystallization and karstification.…”
Section: Experimental Procedures 41 Sample Materialsmentioning
confidence: 99%
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“…The Molasse basin is a foreland basin north of the Alps that formed due to continental collision. As a target geothermal reservoir formation, the Upper Jurassic Malm underlies the Molasse sediments and is confined by the Mesozoic crystalline basement Mavko et al (2003) and the bulk modulus of titanium dioxid is taken from Carmichael (1984 (Hofmann et al, 2014). The massive facies is mainly dolomitized and has a high permeability, due to recrystallization and karstification.…”
Section: Experimental Procedures 41 Sample Materialsmentioning
confidence: 99%
“…The quantitative correlation between static and dynamic moduli in combination with sonic logs and seismic data provide the input elastic parameters to populate geomechanical models. Such geomechanical models can be employed to predict the induced stresses and the resulting deformation, caused by production and injection of water from and into geothermal reservoirs, respectively (Cacace et al, 2013;Hofmann et al, 2014).…”
Section: Introductionmentioning
confidence: 99%
“…9). Cacace et al (2013) have investigated the influence of the damage zone on the productivity of the geothermal reservoir, while Hofmann et al (2014) have addressed the potential of a hydraulically induced fracture on the reservoir productivity. The model spans an area of 8730 m times 9760 m and has a maximum vertical extension of 1080 m. It includes a major ENE-WSW striking fossil normal fault surrounded by a damage zone 160 m wide.…”
Section: Virtual Case Study Iii: Fault Dying Out Laterallymentioning
confidence: 99%
“…The model spans an area of 8730 m times 9760 m and has a maximum vertical extension of 1080 m. It includes a major ENE-WSW striking fossil normal fault surrounded by a damage zone 160 m wide. The distance between the assumed fracture and the damage zone is about 98 m at reservoir depth and the fracture has a half-length if 145 m and a total height of 210 m (Hofmann et al 2014). The model domain is constrained by two isohypses along the SW and NE borders and a third fault zone constrains the domain along the NW border.…”
Section: Virtual Case Study Iii: Fault Dying Out Laterallymentioning
confidence: 99%
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