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dc.contributor.authorWeinert, Sebastian
dc.contributor.authorBär, Kristian
dc.contributor.authorScheuvens, Dirk
dc.contributor.authorSass, Ingo
dc.date.accessioned2020-07-20T10:17:02Z
dc.date.available2020-07-20T10:17:02Z
dc.date.issued2020
dc.identifier.urihttps://tudatalib.ulb.tu-darmstadt.de/handle/tudatalib/2420
dc.identifier.urihttps://doi.org/10.25534/tudatalib-260
dc.descriptionThe Gonghe Basin Complex (GBC), is a pull-apart basin located in the Northeastern Qinghai-Tibet plateau (Qinghai, China) displaying various geothermal features such as elevated geothermal gradients and hot springs, whose origin has not been conclusively determined so far. The adjacent mountain ranges and the basement are comprised of granitoidic rock, which, at sufficient depth and temperature, are suitable for deep enhanced geothermal systems. This study aims to investigate if the radiogenic heat production of these plutonic rocks is the heat source for the surface geothermal features. Therefore, 30 newly sampled Triassic, Silurian, Ordovician and Devonian intrusive rocks were extracted from outcrops in the surroundings and within the GBC, of which one sample was retrieved from exploration well DR2 at c. 1800 m. Samples were geochemically discriminated using the results of XRF measurements and radiogenic heat productions were subsequently calculated. Additionally, analysis of 341 intrusive, 105 extrusive, 155 sedimentary and 76 metamorphic rocks of the Qinling-Qilianshan-Kunlunshan were comprised from literature and compared to the data sampled in the GBC. As evidenced in the presented research, the radiogenic heat production measured in the GBC are within the highest calculated for the Qinling-Qilianshan-Kunlunshan. Although, radiogenic heat production rates in the GBC only range from < 1 µW m^-3 in tonalites to > 5 µW m^-3 in two-mica granites and syenogranites. Nonetheless, average heat productions analyzed do not evidence large intrusions of HHP (high heat producing) granitoids as source of the geothermal features in the GBC pull-apart basin.en_US
dc.language.isoenen_US
dc.rightsCreative Commons Attribution 4.0
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectRadiogenic Heat Productionen_US
dc.subjectGonghe Basin Complexen_US
dc.subjectQinling-Qilianshan-Kunlunshanen_US
dc.subjectEnhanced Geothermal Systemsen_US
dc.subjectQinghai-Tibet plateauen_US
dc.subject.classification316-01 Mineralogie, Petrologie und Geochemie
dc.subject.classification315-01 Physik des Erdkörpers
dc.subject.classification314-01 Geologie, Ingenieurgeologie, Paläontologie
dc.subject.ddc550
dc.titleSupplementary information to 'Radiogenic heat production of crystalline rocks in the Gonghe Basin Complex (Northeastern Qinghai-Tibet plateau, China)'en_US
dc.typeDataseten_US
tud.history.classificationVersion=2016-2020;314-01 Geologie, Ingenieurgeologie, Paläontologie;315-01 Physik des Erdkörpers;316-01 Organische und Anorganische Geochemie, Biogeochemie, Mineralogie, Petrologie, Kristallographie, Lagerstättenkunde;


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Creative Commons Attribution 4.0
Except where otherwise noted, this item's license is described as Creative Commons Attribution 4.0