Climate Change Data Portal
DOI | 10.1016/j.tecto.2021.228927 |
Integrated 3D geological modelling of the northern Upper Rhine Graben by joint inversion of gravimetry and magnetic data | |
Frey M.; Weinert S.; Bär K.; van der Vaart J.; Dezayes C.; Calcagno P.; Sass I. | |
发表日期 | 2021 |
ISSN | 00401951 |
卷号 | 813 |
英文摘要 | The crystalline basement of the Upper Rhine Graben is a major target for deep geothermal exploration due to the generally high reservoir temperatures and the increased radiogenic heat production. The geothermal potential is strongly dependent on the lithology because mainly the thermal but also the hydraulic properties are affected by the rock type. For this reason, the so far most detailed 3D model of the basement in the northern Upper Rhine Graben was developed based on existing structural models, in particular the Hesse 3D 2.0 and GeORG models. Since only a few boreholes fully penetrate the thick sediment cover, additional magnetic and gravity data provided valuable information on the geometry of the deep horizons. To interpret the Bouguer anomalies reasonably with respect to the crystalline basement, the regional gravity field and sedimentary effect were subtracted from the observed data. In comparison to the commonly applied deterministic modelling approaches, a stochastic joint inversion of the gravity and magnetic anomalies was performed that utilizes the principles of a Monte-Carlo-Markov-Chain simulation. For an appropriate attribution of the model units, existing petrophysical databases of the region have been used and in addition, the magnetic susceptibility of more than 430 rock samples was measured. High-resolution voxel models of the density and susceptibility distribution were generated as a result of the inversion, which allow conclusions about the crustal composition under the sedimentary formations. An interpretative map of the basement geology, derived from the inversion results, is presented. © 2021 Elsevier B.V. |
关键词 | 3D modellingGravityJoint inversionMagneticsPetrophysicsUpper Rhine Graben |
英文关键词 | Buildings; Geothermal energy; Geothermal prospecting; Lithology; Magnetic susceptibility; Magnetism; Markov chains; Monte Carlo methods; Sedimentology; Stochastic systems; 3D geological modelling; Deterministic modelling; Geothermal exploration; Gravity and magnetic anomalies; Magnetic and gravity datum; Monte Carlo Markov chain; Radiogenic heat production; Reservoir temperatures; 3D modeling; geothermal system; gravity anomaly; magnetic anomaly; magnetic field; Markov chain; Monte Carlo analysis; petrology; three-dimensional modeling; Germany; Rhine Valley; Upper Rhine Valley |
语种 | 英语 |
来源期刊 | Tectonophysics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/207974 |
作者单位 | Technical University of Darmstadt, Institute of Applied Geosciences, Department of Geothermal Science and Technology, Schnittspahnstraße 9, Darmstadt, 64287, Germany; Darmstadt Graduate School of Excellence Energy Science and Engineering, Otto-Berndt-Straße 3, Darmstadt, 64287, Germany; BRGM, 3, avenue Claude Guillemin, BP36009, Orléans cedex, 45060, France |
推荐引用方式 GB/T 7714 | Frey M.,Weinert S.,Bär K.,et al. Integrated 3D geological modelling of the northern Upper Rhine Graben by joint inversion of gravimetry and magnetic data[J],2021,813. |
APA | Frey M..,Weinert S..,Bär K..,van der Vaart J..,Dezayes C..,...&Sass I..(2021).Integrated 3D geological modelling of the northern Upper Rhine Graben by joint inversion of gravimetry and magnetic data.Tectonophysics,813. |
MLA | Frey M.,et al."Integrated 3D geological modelling of the northern Upper Rhine Graben by joint inversion of gravimetry and magnetic data".Tectonophysics 813(2021). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Frey M.]的文章 |
[Weinert S.]的文章 |
[Bär K.]的文章 |
百度学术 |
百度学术中相似的文章 |
[Frey M.]的文章 |
[Weinert S.]的文章 |
[Bär K.]的文章 |
必应学术 |
必应学术中相似的文章 |
[Frey M.]的文章 |
[Weinert S.]的文章 |
[Bär K.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。