Moeck, Inga S.

[["dc.bibliographiccitation.journal","Netherlands Journal of Geosciences"],["dc.bibliographiccitation.volume","98"],["dc.contributor.author","Moeck, Inga S."],["dc.contributor.author","Dussel, Michael"],["dc.contributor.author","Weber, Josef"],["dc.contributor.author","Schintgen, Tom"],["dc.contributor.author","Wolfgramm, Markus"],["dc.date.accessioned","2020-12-10T15:22:11Z"],["dc.date.available","2020-12-10T15:22:11Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1017/njg.2019.12"],["dc.identifier.eissn","1573-9708"],["dc.identifier.issn","0016-7746"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/17209"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/73298"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.notes.intern","Merged from goescholar"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Geothermal play typing in Germany, case study Molasse Basin: a modern concept to categorise geothermal resources related to crustal permeability"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","25"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Geothermal Energy"],["dc.bibliographiccitation.volume","9"],["dc.contributor.author","Schintgen, Tom V."],["dc.contributor.author","Moeck, Inga S."],["dc.date.accessioned","2021-11-25T11:24:58Z"],["dc.date.accessioned","2022-08-16T12:46:16Z"],["dc.date.available","2021-11-25T11:24:58Z"],["dc.date.available","2022-08-16T12:46:16Z"],["dc.date.issued","2021-10-28"],["dc.date.updated","2022-07-29T12:18:42Z"],["dc.description.abstract","Abstract\r\n The Molasse Basin in Southern Germany is part of the North Alpine Foreland Basin and hosts the largest accumulation of deep geothermal production fields in Central Europe. Despite the vast development of geothermal energy utilization projects especially in the Munich metropolitan region, the evolution of and control factors on the natural geothermal field, more specifically the time-varying recharge and discharge governing groundwater and heat flow, are still debated. Within the Upper Jurassic (Malm) carbonate aquifer as the main geothermal reservoir in the Molasse Basin, temperature anomalies such as the Wasserburg Trough anomaly to the east of Munich and their underlying fluid and heat transport processes are yet poorly understood. We delineate the two end members of thermal–hydraulic regimes in the Molasse Basin by calculating two contrasting permeability scenarios of the heterogeneously karstified Malm carbonate aquifer along a model section through the Wasserburg Trough anomaly by means of two-dimensional numerical thermal-hydraulic modelling. We test the sensitivity of the thermal-hydraulic regime with regard to paleoclimate by computing the two Malm permeability scenarios both with a constant surface temperature of 9 °C and with the impact of paleo-temperature changes during the last 130 ka including the Würm Glaciation. Accordingly, we consider the hydraulic and thermal effects of periglacial conditions like permafrost formation and the impact of the numerous glacial advances onto the Molasse Basin. Thermal-hydraulic modelling reveals the effect of recurrent glacial periods on the subsurface targets of geothermal interest, which is minor compared to the effect of permeability-related, continuous gravity-driven groundwater flow as a major heat transport mechanism."],["dc.identifier.citation","Geothermal Energy. 2021 Oct 28;9(1):25"],["dc.identifier.doi","10.1186/s40517-021-00207-x"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/93552"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/112744"],["dc.language.iso","en"],["dc.rights","CC BY 4.0"],["dc.rights.holder","The Author(s)"],["dc.subject","Würm Glaciation"],["dc.subject","Permafrost"],["dc.subject","North Alpine Foreland Basin"],["dc.subject","Molasse Basin"],["dc.subject","Upper Jurassic"],["dc.subject","Malm"],["dc.subject","Carbonate aquifer"],["dc.subject","Coupled heat and fluid flow"],["dc.subject","Gravity-driven groundwater flow"],["dc.subject","Permeability"],["dc.title","The interplay of Malm carbonate permeability, gravity-driven groundwater flow, and paleoclimate – implications for the geothermal field and potential in the Molasse Basin (southern Germany), a foreland-basin play"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Geothermal Energy"],["dc.bibliographiccitation.volume","3"],["dc.contributor.author","Deon, Fiorenza"],["dc.contributor.author","Förster, Hans-Jürgen"],["dc.contributor.author","Brehme, Maren"],["dc.contributor.author","Wiegand, Bettina"],["dc.contributor.author","Scheytt, Traugott"],["dc.contributor.author","Moeck, Inga"],["dc.contributor.author","Jaya, Makky S."],["dc.contributor.author","Putriatni, Dewi J."],["dc.date.accessioned","2019-07-09T11:41:55Z"],["dc.date.available","2019-07-09T11:41:55Z"],["dc.date.issued","2015"],["dc.description.abstract","Magmatic settings involving active volcanism are potential locations for economic geothermal systems due to the occurrence of high temperature and steam pressures. Indonesia, located along active plate margins, hosts more than 100 volcanoes and, therefore, belongs to the regions with the greatest geothermal potential worldwide. However, tropical conditions and steep terrain reduce the spectrum of applicable exploration methods, in particular in remote areas. In a case study from the Lamongan volcanic field in East Java, we combine field-based data on the regional structural geology, elemental and isotopic composition of thermal waters, and the mineralogical and geochemical signatures of volcanic rocks in exploring hidden geothermal systems. Results suggest infiltration of groundwater at the volcanoes and faults. After infiltration, water is heated and reacts with rocks before rising to the surface. The existence of a potential heat source is petrologically and geophysically constrained to be an active shallow mafic-magma chamber, but its occurrence is not properly reflected in the composition of the collected warmed spring waters that are predominantly meteoric in origin. In conclusion, spring temperature and hydrochemistry alone may not always correctly reflect the deep geothermal potential of an area."],["dc.identifier.doi","10.1186/s40517-015-0040-6"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/12588"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/58549"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.relation.issn","2195-9706"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Geochemical/hydrochemical evaluation of the geothermal potential of the Lamongan volcanic field (Eastern Java, Indonesia)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]